Articles | Volume 6, issue 1
https://doi.org/10.5194/se-6-73-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Special issue:
https://doi.org/10.5194/se-6-73-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
16 Jan 2015
Research article |
| 16 Jan 2015
Upper mantle structure around the Trans-European Suture Zone obtained by teleseismic tomography
I. Janutyte
CORRESPONDING AUTHOR
NORSAR, Kjeller, Norway
Vilnius University, Vilnius, Lithuania
Lithuanian Geological Survey, Vilnius, Lithuania
M. Majdanski
Institute of Geophysics Polish Academy of Sciences, Warsaw, Poland
P. H. Voss
Geological Survey of Denmark and Greenland – GEUS, Copenhagen, Denmark
E. Kozlovskaya
Sodankylä Geophysical Observatory/Oulu Unit, University of Oulu, Oulu, Finland
PASSEQ Working Group
indicated in Acknowledgements
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Nikita Afonin, Elena Kozlovskaya, Kari Moisio, Emma-Riikka Kokko, and Jarkko Okkonen
The Cryosphere, 18, 2223–2238, https://doi.org/10.5194/tc-18-2223-2024, https://doi.org/10.5194/tc-18-2223-2024, 2024
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Our study shows that seismic events in the wetlands in Arctic and sub-Arctic areas are capable of producing ground motions strong enough to damage the infrastructures like roads and basements of buildings located at distances of several hundreds of metres from the wetlands. That is why this phenomenon deserves further studies.
Nikita Afonin, Elena Kozlovskaya, Suvi Heinonen, and Stefan Buske
Solid Earth, 12, 1563–1579, https://doi.org/10.5194/se-12-1563-2021, https://doi.org/10.5194/se-12-1563-2021, 2021
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In our study, we show the results of a passive seismic interferometry application for mapping the uppermost crust in the area of active mineral exploration in northern Finland. The obtained velocity models agree well with geological data and complement the results of reflection seismic data interpretation.
Kristian Svennevig, Trine Dahl-Jensen, Marie Keiding, John Peter Merryman Boncori, Tine B. Larsen, Sara Salehi, Anne Munck Solgaard, and Peter H. Voss
Earth Surf. Dynam., 8, 1021–1038, https://doi.org/10.5194/esurf-8-1021-2020, https://doi.org/10.5194/esurf-8-1021-2020, 2020
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The 17 June 2017 Karrat landslide in Greenland caused a tsunami that killed four people. We apply a multidisciplinary workflow to reconstruct a timeline of events and find that three historic landslides occurred in 2009, 2016, and 2017. We also find evidence of much older periods of landslide activity. Three newly discovered active slopes might pose a future hazard. We speculate that the trigger for the recent events is melting permafrost due to a warming climate.
Nikita Afonin, Elena Kozlovskaya, Jouni Nevalainen, and Janne Narkilahti
Solid Earth, 10, 1621–1634, https://doi.org/10.5194/se-10-1621-2019, https://doi.org/10.5194/se-10-1621-2019, 2019
Nikita Afonin, Elena Kozlovskaya, Ilmo Kukkonen, and DAFNE/FINLAND Working Group
Solid Earth, 8, 531–544, https://doi.org/10.5194/se-8-531-2017, https://doi.org/10.5194/se-8-531-2017, 2017
Elena Kozlovskaya, Janne Narkilahti, Jouni Nevalainen, Riitta Hurskainen, and Hanna Silvennoinen
Geosci. Instrum. Method. Data Syst., 5, 365–382, https://doi.org/10.5194/gi-5-365-2016, https://doi.org/10.5194/gi-5-365-2016, 2016
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The paper describes the history and the present state of instrumental seismic observations at the University of Oulu and Sodankylä Geophysical Observatory in northern Finland that started in 1950s. This includes both seismic observations at permanent seismic stations and temporary seismic experiments by portable seismic equipment. We describe the instrumentation and major research topics of seismic group at the SGO and discuss the plans for their future development.
Olga Usoltseva and Elena Kozlovskaya
Solid Earth, 7, 1095–1108, https://doi.org/10.5194/se-7-1095-2016, https://doi.org/10.5194/se-7-1095-2016, 2016
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We address the problem of seismicity in the intraplate area of northern Fennoscandia using the information on local events recorded by the POLENET/LAPNET seismic array. We relocate the seismic events, calculate a 3-D tomographic P wave velocity model of the uppermost crust and investigate a focal mechanism of the event. Our results demonstrate that the Baltic-Bothnia Megashear is an important large-scale, reactivated tectonic structure that has to be taken into account when estimating seismic hazard.
Hanna Silvennoinen, Elena Kozlovskaya, and Eduard Kissling
Solid Earth, 7, 425–439, https://doi.org/10.5194/se-7-425-2016, https://doi.org/10.5194/se-7-425-2016, 2016
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POLENET/LAPNET broadband seismic network was deployed in northern Fennoscandia 2007–2009. In our study we estimate the 3D architecture of the upper mantle beneath the network using high-resolution teleseismic P-wave tomography. Our study reveals a highly heterogeneous lithospheric mantle. The most significant feature seen in the obtained velocity model is a large elongated low-velocity anomaly beneath the crust, separating the three cratonic units that formed the region in the early Proterozoic.
I. Janutyte, E. Kozlovskaya, M. Majdanski, P. H. Voss, M. Budraitis, and PASSEQWorking Group
Solid Earth, 5, 821–836, https://doi.org/10.5194/se-5-821-2014, https://doi.org/10.5194/se-5-821-2014, 2014
S. Gregersen and P. H. Voss
Solid Earth, 5, 109–118, https://doi.org/10.5194/se-5-109-2014, https://doi.org/10.5194/se-5-109-2014, 2014
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Wind turbines that are located close to a seismometer produce ground tremors that can increase the noise level at the seismic station. Using numerical models, we analyse the effectivity of borehole installations to reduce this impact. We study effects of geophysical parameters on the borehole effectivity and validate our modelling approach with data from real boreholes. Boreholes are effective in reducing the impact of wind turbines; however, this depends on the wavelength of the seismic wave.
Sebastian Hellmann, Melchior Grab, Cedric Patzer, Andreas Bauder, and Hansruedi Maurer
Solid Earth, 14, 805–821, https://doi.org/10.5194/se-14-805-2023, https://doi.org/10.5194/se-14-805-2023, 2023
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Acoustic waves are suitable to analyse the physical properties of the subsurface. For this purpose, boreholes are quite useful to deploy a source and receivers in the target area to get a comprehensive high-resolution dataset. However, when conducting such experiments in a subsurface such as glaciers that continuously move, the boreholes get deformed. In our study, we therefore developed a method that allows an analysis of the ice while considering deformations.
Laura A. Ermert, Enrique Cabral-Cano, Estelle Chaussard, Darío Solano-Rojas, Luis Quintanar, Diana Morales Padilla, Enrique A. Fernández-Torres, and Marine A. Denolle
Solid Earth, 14, 529–549, https://doi.org/10.5194/se-14-529-2023, https://doi.org/10.5194/se-14-529-2023, 2023
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Mexico City is built on a unique ground containing the clay-rich sediments of the ancient lake Texcoco. Continuous imperceptible shaking of these deposits by city traffic and other sources allows us to monitor changes in the subsurface seismic wave speed. Wave speed varies seasonally, likely due to temperature and rain effects; it temporarily drops after large earthquakes then starts to recover. Throughout the studied period, it increased on average, which may be related to soil compaction.
Laura Anna Ermert, Maria Koroni, and Naiara Korta Martiartu
Solid Earth, 14, 485–498, https://doi.org/10.5194/se-14-485-2023, https://doi.org/10.5194/se-14-485-2023, 2023
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We investigate women's representation in seismology to raise awareness of existing gender disparities.
By analysing the authorship of peer-reviewed articles, we identify lower representation of women among single authors, high-impact authors, and highly productive authors. Seismology continues to be a male-dominated field, and trends suggest that parity is decades away. These gaps are an obstacle to women’s career advancement and, if neglected, may perpetuate the leaky-pipeline problem.
Jordi Díaz, Sergi Ventosa, Martin Schimmel, Mario Ruiz, Albert Macau, Anna Gabàs, David Martí, Özgenç Akin, and Jaume Vergés
Solid Earth, 14, 499–514, https://doi.org/10.5194/se-14-499-2023, https://doi.org/10.5194/se-14-499-2023, 2023
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We assess the capability of multiple methods based on the interpretation of seismic noise to map the basement of the Cerdanya Basin, located in the eastern Pyrenees. Basement depth estimations retrieved from the different approaches are consistent, with maximum depths reaching 700 m close to the Têt fault bounding the basin to the east. Our results prove that seismic noise analysis using high-density networks is an excellent tool to improve the geological characterization of sedimentary basins.
Zahra Zali, Theresa Rein, Frank Krüger, Matthias Ohrnberger, and Frank Scherbaum
Solid Earth, 14, 181–195, https://doi.org/10.5194/se-14-181-2023, https://doi.org/10.5194/se-14-181-2023, 2023
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Investigation of the global Earth's structure benefits from the analysis of ocean bottom seismometer (OBS) data that allow an improved seismic illumination of dark spots of crustal and mantle structures in the oceanic regions of the Earth. However, recordings from the ocean bottom are often highly contaminated by noise. We developed an OBS noise reduction algorithm, which removes much of the oceanic noise while preserving the earthquake signal and does not introduce waveform distortion.
Jerome Azzola, Katja Thiemann, and Emmanuel Gaucher
EGUsphere, https://doi.org/10.5194/egusphere-2022-1417, https://doi.org/10.5194/egusphere-2022-1417, 2022
Preprint archived
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Distributed Acoustic Sensing is applied to the micro-seismic monitoring of a geothermal plant. In this domain, the feasibility of managing the large flow of generated data and their suitability to monitor locally induced seismicity was yet to be assessed. The proposed monitoring system efficiently managed the acquisition, processing and saving of the data over a 6-month period. This testing period proved that the monitoring concept advantageously complements more classical monitoring networks.
Heather Kennedy, Katrin Löer, and Amy Gilligan
Solid Earth, 13, 1843–1858, https://doi.org/10.5194/se-13-1843-2022, https://doi.org/10.5194/se-13-1843-2022, 2022
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The energy transition is an important topic for benefiting the future; thus renewable energy is required to reach net-zero carbon emission goals. Geothermal energy, heat from the ground, can be used in this transition. Therefore, geothermal fields need to be characterized as much as possible to allow for increased productivity within these fields. This study involves and looks at potential fractures within a geothermal field at depth to help increase the overall understanding of this field.
Roberto Cabieces, Mariano S. Arnaiz-Rodríguez, Antonio Villaseñor, Elizabeth Berg, Andrés Olivar-Castaño, Sergi Ventosa, and Ana M. G. Ferreira
Solid Earth, 13, 1781–1801, https://doi.org/10.5194/se-13-1781-2022, https://doi.org/10.5194/se-13-1781-2022, 2022
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This paper presents a new 3D shear-wave velocity model of the lithosphere of northeastern Venezuela, including new Moho and Vp / Vs maps. Data were retrieved from land and broadband ocean bottom seismometers from the BOLIVAR experiment.
Megha Chakraborty, Wei Li, Johannes Faber, Georg Rümpker, Horst Stoecker, and Nishtha Srivastava
Solid Earth, 13, 1721–1729, https://doi.org/10.5194/se-13-1721-2022, https://doi.org/10.5194/se-13-1721-2022, 2022
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Earthquake magnitude is a crucial parameter in defining its damage potential, and hence its speedy determination is essential to issue an early warning in regions close to the epicentre. This study summarises our findings in an attempt to apply deep-learning-based classifiers to earthquake waveforms, particularly with respect to finding an optimum length of input data. We conclude that the input length has no significant effect on the model accuracy, which varies between 90 %–94 %.
Carola Leva, Georg Rümpker, and Ingo Wölbern
Solid Earth, 13, 1243–1258, https://doi.org/10.5194/se-13-1243-2022, https://doi.org/10.5194/se-13-1243-2022, 2022
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The seismicity of Fogo and Brava, Cape Verde, is dominated by volcano-tectonic earthquakes in the area of Brava and volcanic seismic signals, such as hybrid events, on Fogo. We locate these events using a multi-array analysis, which allows the localization of seismic events occurring outside the network and of volcanic signals lacking clear phases. We observe exceptionally high apparent velocities for the hybrid events located on Fogo. These velocities are likely caused by a complex ray path.
Michal Chamarczuk, Michal Malinowski, Deyan Draganov, Emilia Koivisto, Suvi Heinonen, and Sanna Rötsä
Solid Earth, 13, 705–723, https://doi.org/10.5194/se-13-705-2022, https://doi.org/10.5194/se-13-705-2022, 2022
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In passive seismic measurement, all noise sources from the environment, such as traffic, vibrations caused by distant excavation, and explosive work from underground mines, are utilized. In the Kylylahti experiment, receivers recorded ambient noise sources for 30 d. These recordings were subjected to data analysis and processing using novel methodology developed in our study and used for imaging the subsurface geology of the Kylylahti mine area.
Jorge Acevedo, Gabriela Fernández-Viejo, Sergio Llana-Fúnez, Carlos López-Fernández, Javier Olona, and Diego Pérez-Millán
Solid Earth, 13, 659–679, https://doi.org/10.5194/se-13-659-2022, https://doi.org/10.5194/se-13-659-2022, 2022
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The NW Iberian Peninsula provides one of the most complete Variscan sections in Europe, showing the transition between a sedimentary domain with folds and thrust and a metamorphic domain with igneous intrusions. By processing the seismic ambient noise recorded by several seismograph networks in this area, new 3-D S-wave velocity and radial anisotropy models were created. These models reveal the limit between the two domains, delineating the core of the large western European Variscan Belt.
Thierry Camelbeeck, Koen Van Noten, Thomas Lecocq, and Marc Hendrickx
Solid Earth, 13, 469–495, https://doi.org/10.5194/se-13-469-2022, https://doi.org/10.5194/se-13-469-2022, 2022
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Over the 20th century, shallow damaging seismicity occurred in and near the Hainaut coal mining area in Belgium. We provide an overview of earthquake parameters and impacts, combining felt and damage testimonies and instrumental measurements. Shallower earthquakes have a depth and timing compatible with mining activity. The most damaging events occurred deeper than the mines but could still have been triggered by mining-caused crustal changes. Our modelling can be applied to other regions.
Nicola Piana Agostinetti, Alberto Villa, and Gilberto Saccorotti
Solid Earth, 13, 449–468, https://doi.org/10.5194/se-13-449-2022, https://doi.org/10.5194/se-13-449-2022, 2022
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Sensing the Earth is a fundamental operation for the future where georesources, like geothermal energy and CO2 underground storage, will become important tools for addressing societal challenges. The development of networks of optical fibre cables gives the possibility of a sensing grid with an unprecedented spatial coverage. Here, we investigate the potential of using portions of a optical fibre cable as a standard seismometer for exploring the subsurface and monitoring georesources.
Carolin M. Boese, Grzegorz Kwiatek, Thomas Fischer, Katrin Plenkers, Juliane Starke, Felix Blümle, Christoph Janssen, and Georg Dresen
Solid Earth, 13, 323–346, https://doi.org/10.5194/se-13-323-2022, https://doi.org/10.5194/se-13-323-2022, 2022
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Hydraulic stimulation experiments in underground facilities allow for placing monitoring equipment close to and surrounding the stimulated rock under realistic and complex conditions at depth. We evaluate how accurately the direction-dependent velocity must be known for high-resolution seismic monitoring during stimulation. Induced transient deformation in rocks only 2.5–5 m apart may differ significantly in magnitude and style, and monitoring requires sensitive sensors adapted to the frequency.
Jaroslava Plomerová, Helena Žlebčíková, György Hetényi, Luděk Vecsey, Vladislav Babuška, and AlpArray-EASI and AlpArray working
groups
Solid Earth, 13, 251–270, https://doi.org/10.5194/se-13-251-2022, https://doi.org/10.5194/se-13-251-2022, 2022
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We present high-resolution tomography images of upper mantle structure beneath the E Alps and the adjacent Bohemian Massif. The northward-dipping lithosphere, imaged down to ∼200 km beneath the E Alps without signs of delamination, is probably formed by a mixture of a fragment of detached European plate and the Adriatic plate subductions. A detached high-velocity anomaly, sub-parallel to and distinct from the E Alps heterogeneity, is imaged at ∼100–200 km beneath the southern part of the BM.
Gregor Rajh, Josip Stipčević, Mladen Živčić, Marijan Herak, Andrej Gosar, and the AlpArray Working Group
Solid Earth, 13, 177–203, https://doi.org/10.5194/se-13-177-2022, https://doi.org/10.5194/se-13-177-2022, 2022
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We investigated the 1-D velocity structure of the Earth's crust in the NW Dinarides with inversion of arrival times from earthquakes. The obtained velocity models give a better insight into the crustal structure and show velocity variations among different parts of the study area. In addition to general structural implications and a potential for improving further work, the results of our study can also be used for routine earthquake location and for detecting errors in seismological bulletins.
Guido Maria Adinolfi, Raffaella De Matteis, Rita de Nardis, and Aldo Zollo
Solid Earth, 13, 65–83, https://doi.org/10.5194/se-13-65-2022, https://doi.org/10.5194/se-13-65-2022, 2022
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We propose a methodology useful to evaluate (1) the reliability of a focal mechanism solution inferred by the inversion of seismological data and (2) the performance of a seismic network, operated to monitor natural or induced seismicity, to assess focal mechanism solutions. As a test case, we studied the focal mechanism reliability by using synthetic data computed for ISNet, a local seismic network monitoring the Irpinia fault system (southern Italy).
Nicola Piana Agostinetti and Giulia Sgattoni
Solid Earth, 12, 2717–2733, https://doi.org/10.5194/se-12-2717-2021, https://doi.org/10.5194/se-12-2717-2021, 2021
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One of the present-day challenges for geoscientists is tackling the big data revolution. An ever-growing amount of data needs to be processed and data are subjectively handled before using them to make inferences on the Earth’s interior. But imposing subjective decisions on the data might have strong influences on the final outputs. Here we present a totally novel and automatic application for screening the data and for defining data volumes that are consistent with physical hypotheses.
Marcel Paffrath, Wolfgang Friederich, Stefan M. Schmid, Mark R. Handy, and the AlpArray and AlpArray-Swath D Working Group
Solid Earth, 12, 2671–2702, https://doi.org/10.5194/se-12-2671-2021, https://doi.org/10.5194/se-12-2671-2021, 2021
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The Alpine mountain belt was formed by the collision of the Eurasian and African plates in the geological past, during which parts of the colliding plates sank into the earth's mantle. Using seismological data from distant earthquakes recorded by the AlpArray Seismic Network, we have derived an image of the current location of these subducted parts in the earth's mantle. Their quantity and spatial distribution is key information needed to understand how the Alpine orogen was formed.
Felix N. Wolf, Dietrich Lange, Anke Dannowski, Martin Thorwart, Wayne Crawford, Lars Wiesenberg, Ingo Grevemeyer, Heidrun Kopp, and the AlpArray Working Group
Solid Earth, 12, 2597–2613, https://doi.org/10.5194/se-12-2597-2021, https://doi.org/10.5194/se-12-2597-2021, 2021
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The Ligurian Sea opened ~30–15 Ma during SE migration of the Calabrian subduction zone. Using ambient seismic noise from stations on land and at the ocean bottom, we calculated a 3D shear-velocity model of the Ligurian Basin. In keeping with existing 2D studies, we find a shallow crust–mantle transition at the SW basin centre that deepens towards the northeast, Corsica, and the Liguro-Provençal coast. We observe a separation of SW and NE basins. We do not observe high crustal vP/vS ratios.
Martin Thorwart, Anke Dannowski, Ingo Grevemeyer, Dietrich Lange, Heidrun Kopp, Florian Petersen, Wayne C. Crawford, Anne Paul, and the AlpArray Working Group
Solid Earth, 12, 2553–2571, https://doi.org/10.5194/se-12-2553-2021, https://doi.org/10.5194/se-12-2553-2021, 2021
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We analyse broadband ocean bottom seismometer data of the AlpArray OBS network in the Ligurian Basin. Two earthquake clusters with thrust faulting focal mechanisms indicate compression of the rift basin. The locations of seismicity suggest reactivation of pre-existing rift structures and strengthening of crust and uppermost mantle during rifting-related extension. Slightly different striking directions of faults may mimic the anti-clockwise rotation of the Corsica–Sardinia block.
Rainer Kind, Stefan M. Schmid, Xiaohui Yuan, Benjamin Heit, Thomas Meier, and the AlpArray and AlpArray-SWATH-D Working Groups
Solid Earth, 12, 2503–2521, https://doi.org/10.5194/se-12-2503-2021, https://doi.org/10.5194/se-12-2503-2021, 2021
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A large amount of new seismic data from the greater Alpine area have been obtained within the AlpArray and SWATH-D projects. S-to-P converted seismic phases from the Moho and from the mantle lithosphere have been processed with a newly developed method. Examples of new observations are a rapid change in Moho depth at 13° E below the Tauern Window from 60 km in the west to 40 km in the east and a second Moho trough along the boundary of the Bohemian Massif towards the Western Carpathians.
Bogdan Grecu, Felix Borleanu, Alexandru Tiganescu, Natalia Poiata, Raluca Dinescu, and Dragos Tataru
Solid Earth, 12, 2351–2368, https://doi.org/10.5194/se-12-2351-2021, https://doi.org/10.5194/se-12-2351-2021, 2021
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The lockdown imposed in Romania to prevent the spread of COVID-19 has significantly impacted human activity across the country. By analyzing the ground vibrations recorded at seismic stations, we were able to monitor the changes in human activity before and during the lockdown.
The reduced human activity during the lockdown has also provided a good opportunity for stations sited in noisy urban areas to record earthquake signals that would not have been recorded under normal conditions.
Ruth Keppler, Roman Vasin, Michael Stipp, Tomás Lokajícek, Matej Petruzálek, and Nikolaus Froitzheim
Solid Earth, 12, 2303–2326, https://doi.org/10.5194/se-12-2303-2021, https://doi.org/10.5194/se-12-2303-2021, 2021
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Rocks in mountain belts have been deformed during continental collision causing a certain alignment of the minerals referred to as crystallographic preferred orientation (CPO). Minerals have anisotropic properties: the velocity of seismic waves travelling through them is direction dependent. This leads to anisotropy of the rocks. We measured the CPO of common rocks within the Alps. With this data and known anisotropic properties of the minerals we calculated the seismic anisotropy of the rocks.
Mario Arroyo-Solórzano, Diego Castro-Rojas, Frédérick Massin, Lepolt Linkimer, Ivonne Arroyo, and Robin Yani
Solid Earth, 12, 2127–2144, https://doi.org/10.5194/se-12-2127-2021, https://doi.org/10.5194/se-12-2127-2021, 2021
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We present the first seismic noise variation levels during COVID-19 in Central America using 10 seismometers. We study the impact of the seismic noise reduction on the detectability of earthquakes and on the felt reports. Our results show maximum values (~50 % decrease) at seismic stations near airports and densely inhabited cities. The decrease in seismic noise improved earthquake locations and reports. Seismic noise could also be useful to verify compliance with lockdown measures.
Laura Peruzza, Alessandra Schibuola, Maria Adelaide Romano, Marco Garbin, Mariangela Guidarelli, Denis Sandron, and Enrico Priolo
Solid Earth, 12, 2021–2039, https://doi.org/10.5194/se-12-2021-2021, https://doi.org/10.5194/se-12-2021-2021, 2021
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In weakly seismic or poorly monitored areas, the uncritical use of earthquake catalogues can be misleading. This is the case for a central sector in the Po Valley, where the Northern Apennines and Southern Alps collide. We collect and reprocess the available instrumental data of about 300 earthquakes from 1951 to 2019. The seismicity is weak, deeper than expected, and far from some existing human activities carried out underground. The potential tectonic causative sources are still unknown.
Fabian Limberger, Michael Lindenfeld, Hagen Deckert, and Georg Rümpker
Solid Earth, 12, 1851–1864, https://doi.org/10.5194/se-12-1851-2021, https://doi.org/10.5194/se-12-1851-2021, 2021
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Frequency-dependent amplitude decays of seismic signals induced by wind turbines are determined from (up to) 6 months of continuous recordings measured along an 8 km profile located at a wind farm in Bavaria, Germany. The radiation pattern and amplitude decay of the induced signals are accounted for by an analytical approach that includes path and source effects. This approach is generalized to predict the characteristic seismic radiation patterns of arbitrary wind farm configurations.
Alessio Spurio Mancini, Davide Piras, Ana Margarida Godinho Ferreira, Michael Paul Hobson, and Benjamin Joachimi
Solid Earth, 12, 1683–1705, https://doi.org/10.5194/se-12-1683-2021, https://doi.org/10.5194/se-12-1683-2021, 2021
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The localization of an earthquake is affected by many uncertainties. To correctly propagate these uncertainties into an estimate of the earthquake coordinates and their associated errors, many simulations of seismic waves are needed. This operation is computationally very intensive, hindering the feasibility of this approach. In this paper, we present a series of deep-learning methods to produce accurate seismic traces in a fraction of the time needed with standard methods.
Marguerite Mathey, Christian Sue, Colin Pagani, Stéphane Baize, Andrea Walpersdorf, Thomas Bodin, Laurent Husson, Estelle Hannouz, and Bertrand Potin
Solid Earth, 12, 1661–1681, https://doi.org/10.5194/se-12-1661-2021, https://doi.org/10.5194/se-12-1661-2021, 2021
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This work features the highest-resolution seismic stress and strain fields available at the present time for the analysis of the active crustal deformation of the Western Alps. In this paper, we address a large dataset of newly computed focal mechanisms from a statistical standpoint, which allows us to suggest a joint control from far-field forces and from buoyancy forces on the present-day deformation of the Western Alps.
Marcel Paffrath, Wolfgang Friederich, and the AlpArray and AlpArray-SWATH D Working Groups
Solid Earth, 12, 1635–1660, https://doi.org/10.5194/se-12-1635-2021, https://doi.org/10.5194/se-12-1635-2021, 2021
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Using the AlpArray seismic network, we have determined highly accurate travel times of P waves from over 370 major global earthquakes between 2015 and 2019, which shall be used for a tomography of the mantle beneath the greater Alpine region.
Comparing with theoretical travel times of a standard reference earth model, we receive very stable patterns of travel-time differences across the network which provide evidence of varying subduction behaviour along the strike of the Alpine orogen.
Itzhak Lior, Anthony Sladen, Diego Mercerat, Jean-Paul Ampuero, Diane Rivet, and Serge Sambolian
Solid Earth, 12, 1421–1442, https://doi.org/10.5194/se-12-1421-2021, https://doi.org/10.5194/se-12-1421-2021, 2021
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The increasing use of distributed acoustic sensing (DAS) inhibits the transformation of optical fibers into dense arrays of seismo-acoustic sensors. Here, DAS strain records are converted to ground motions using the waves' apparent velocity. An algorithm for velocity determination is presented, accounting for velocity variations between different seismic waves. The conversion allows for robust determination of fundamental source parameters, earthquake magnitude and stress drop.
Sarah Mader, Joachim R. R. Ritter, Klaus Reicherter, and the AlpArray Working Group
Solid Earth, 12, 1389–1409, https://doi.org/10.5194/se-12-1389-2021, https://doi.org/10.5194/se-12-1389-2021, 2021
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The Albstadt Shear Zone, SW Germany, is an active rupture zone with sometimes damaging earthquakes but no visible surface structure. To identify its segmentations, geometry, faulting pattern and extension, we analyze the continuous earthquake activity in 2011–2018. We find a segmented N–S-oriented fault zone with mainly horizontal and minor vertical movement along mostly NNE- and some NNW-oriented rupture planes. The main horizontal stress is oriented NW and due to Alpine-related loading.
Gesa Maria Petersen, Simone Cesca, Sebastian Heimann, Peter Niemz, Torsten Dahm, Daniela Kühn, Jörn Kummerow, Thomas Plenefisch, and the AlpArray and AlpArray-Swath-D working groups
Solid Earth, 12, 1233–1257, https://doi.org/10.5194/se-12-1233-2021, https://doi.org/10.5194/se-12-1233-2021, 2021
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The Alpine mountains are known for a complex tectonic history. We shed light onto ongoing tectonic processes by studying rupture mechanisms of small to moderate earthquakes between 2016 and 2019 observed by the temporary AlpArray seismic network. The rupture processes of 75 earthquakes were analyzed, along with past earthquakes and deformation data. Our observations point at variations in the underlying tectonic processes and stress regimes across the Alps.
Azam Jozi Najafabadi, Christian Haberland, Trond Ryberg, Vincent F. Verwater, Eline Le Breton, Mark R. Handy, Michael Weber, and the AlpArray and AlpArray SWATH-D working groups
Solid Earth, 12, 1087–1109, https://doi.org/10.5194/se-12-1087-2021, https://doi.org/10.5194/se-12-1087-2021, 2021
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This study achieved high-precision hypocenters of 335 earthquakes (1–4.2 ML) and 1D velocity models of the Southern and Eastern Alps. The general pattern of seismicity reflects head-on convergence of the Adriatic Indenter with the Alpine orogenic crust. The relatively deeper seismicity in the eastern Southern Alps and Giudicarie Belt indicates southward propagation of the Southern Alpine deformation front. The derived hypocenters form excellent data for further seismological studies, e.g., LET.
Javier Ojeda and Sergio Ruiz
Solid Earth, 12, 1075–1085, https://doi.org/10.5194/se-12-1075-2021, https://doi.org/10.5194/se-12-1075-2021, 2021
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In Santiago, Chile, the lockdown imposed due to COVID-19 was recorded by seismological instruments. This analysis shows temporal changes in the surface vibrations controlled by lockdown phases, mobility, and epidemiological factors. Our findings suggest that
dynamic lockdownand the early deconfinement in April 2020 caused an increase in mobility and therefore virus transmission. We propose that seismic networks could be used to monitor urban mobility as a new proxy in public policies.
Jiří Kvapil, Jaroslava Plomerová, Hana Kampfová Exnerová, Vladislav Babuška, György Hetényi, and AlpArray Working Group
Solid Earth, 12, 1051–1074, https://doi.org/10.5194/se-12-1051-2021, https://doi.org/10.5194/se-12-1051-2021, 2021
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This paper presents a high-resolution 3-D shear wave velocity (vS) model of the Bohemian Massif crust imaged from high-density data and enhanced depth sensitivity of tomographic inversion. The dominant features of the model are relatively higher vS in the upper crust than in its surrounding, a distinct intra-crustal interface, and a velocity decrease in the lower part of the crust. The low vS in the lower part of the crust is explained by the anisotropic fabric of the lower crust.
Martijn P. A. van den Ende and Jean-Paul Ampuero
Solid Earth, 12, 915–934, https://doi.org/10.5194/se-12-915-2021, https://doi.org/10.5194/se-12-915-2021, 2021
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Distributed acoustic sensing (DAS) is an emerging technology that measures stretching of an optical-fibre cable. This technology can be used to record the ground shaking of earthquakes, which offers a cost-efficient alternative to conventional seismometers. Since DAS is relatively new, we need to verify that existing seismological methods can be applied to this new data type. In this study, we reveal several issues by comparing DAS with conventional seismometer data for earthquake localisation.
Cited articles
Aki, K., A. Christoffersson, and Husebye, E. S.: Determination of the three-dimensional seismic structure of the lithosphere, J. Geophys. Res., 82, 277–296, 1977.
Arlitt, R.: Teleseismic body wave tomography across the Trans-European Suture Zone between Sweden and Denmark, PhD theses, ETH, Swiss Federal Institute of Technology Zürich, Swiss, 1999.
Artemieva, I. M.: Global 1° × 1° thermal model TC1 for the continental lithosphere: implications for lithosphere secular evolution, Tectonophysics, 416, 245–277, 2006.
Artemieva, I. M.: Dynamic topography of the East European craton: Shedding light upon lithospheric structure, composition and mantle dynamics, Global and Planetary Change, 58, 411–434, 2007.
Artemieva, I. M., Thybo, H., and Kaban, M. K.: Deep Europe today: Geophysical synthesis of the upper mantle structure and lithospheric processes over 3.5 Ga, in: European Lithosphere Dynamics, edited by: Gee, D. and Stephenson, R., Geological Society London, Special Publication, 32, 11–41, 2006.
Babuška V. and Plomerova J.: Subcrustal Lithosphere Around the Saxothuringian-Moldanubian Suture Zone – a model derived from anisotropy of seismic wave velocities, Tectonophysics, 332, 185–199, 2001.
Babuška, V., Plomerova, J., and Fischer, T.: Intraplate Seismicity in the Western Bohemian Massif (Central Europe): A possible correlation with a paleoplate junction, J. Geophysics, 44, 149–159, 2007.
Banka, D., Pharao, T. C., Williamson, J. P., and the TESZ Project Potential Field Core Group: Potential field imaging of Paleozoic orogenic structure in northern and central Europe, Tectonophysics, 360, 23–45, 2002.
Belka, Z., Ahrendt, H., Franke, and W., and Wemmer, K.: The Baltica-Gondwana suture in central Europe: evidence from K–Ar ages of detrital muscovites and biogeographical data, in: Orogenic Processes: Quantification and Modelling of the Variscan Belt, edited by: Franke, W., Haak, V., Oncken, O., and Taner, D., Geological Society, London, 87–102, 2000.
Beller, S., Kozlovskaya, E., Achauer, U., and Tiberi, Ch.: Joint inversion of teleseismic and gravity data beneath the Fennoscandian Shield, EGU General Assembly 2013, Geophys. Res. Abstracts, 15, EGU 2013-4771-2, 2013.
Blundel, D., Freeman, R., and Mueller, S. (Eds.): A Continent Revealed – The European Geotraverse. European Science Foundation, Cambridge University Press, Cambridge, 287 pp., 1992.
Bogdanova, S. V., Gorbatschev, R., Stephenson, R. A., and Guterch A. (Eds.): EUROBRIDGE: Palaeoproterozoic accretion of Fennoscandia and Sarmatia, Tectonophysics, 339, 1–2, 2001.
Bogdanova, S., Gorbatschev, R., Grad, M., Janik, T., Guterch, A., Kozlovskaya, E., Motuza, G., Skridlaite, G., Starostenko, V., Taran, L., and the EUROBRIDGE and POLONAISE Working Groups: EUROBRIDGE: new insight into the geodynamic evolution of the East European Craton, in: European Lithospheric Dynamics. Memoirs Number 32, edited by: Gee, D. G. and Stephenson, R. A., Geological Society, London, 599–625, 2006.
Bogdanova, S. V., Bingen, B., Gorbatschev, R., Kheraskova, T. N, Kozlov, V. I., Puchkov, V. N., and Volozh, Yu. A.: The East European Craton (Baltica) before and during the assembly of Rodinia, Precam. Res., 160, 23–45, 2008.
Bruneton, M., Pedersen, H. A., Farra, V., Arndt, N. T., Vacher, P., Achauer, U., Alinaghi, A., Ansorge, J., Bock, G., Friederich,W., Grad, M., Guterch, A., Heikkinen, P., Hjelt, S.-E., Hyvönen, T. L., Ikonen, J.-P., Kissling, E., Komminaho, K., Korja, A., Kozlovskaya, E., Nevsky, M. V., Paulssen, H., Pavlenkova, N. I., Plomerová, J., Raita, T., Riznichenko, O. Y., Roberts, R. G., Sandoval, S., Sanina, I. A., Sharov, N. V., Shomali, Z. H., Tiikkainen, J., Wielandt, E., Wilegalla, K., Yliniemi, J., and Yurov, Y. G.: Complex lithospheric structure under the central Baltic Shield from surface wave tomography, J. Geophys. Res., 109, B10303, https://doi.org/10.1029/2003JB002947, 2004.
Cotte, N., Pedersen, H. A., and TOR Working Group: Sharp contrast in lithospheric structure across the Sorgenfrei–Tornquist zone as inferred by Rayleigh wave analysis of TOR1 project data, Tectonophysics, 360, 75–88, 2002.
Czuba, W., Grad, M., Luosto, U., Motuza, G., Nasedkin, V., and POLONAISE P5 Working Group: Crustal structure of the East European craton along the POLONAISE'97 P5 profile, Acta Geoph. Pol., 49, 145–168, 2001.
Dadlez, R., Grad, M., and Guterch, A.: Crustal structure below the Polish Basin: Is it composed of proximal terranes derived from Baltica?, Tectonophysics, 411, 111–128, 2005.
Dörr W., Belka Z., Marheine D., Schastok J., Valverde Vaquero P., and Wiszniewska J.: U–Pb and Ar–Ar geochronology of anorogenic granite magmatism of the Mazury complex NE Poland, in: Precambrian Research, edited by: Rämo, T., Special issue, 119, 101–102, 2002.
Eaton, D. W., Darbyshire, F., Evans, R. L., Grütter, H., Jones, A. G., and Yuan, X.: The elusive lithosphere–asthenosphere boundary (LAB) beneath cratons, Lithos, 109, 1–22, 2009.
EUROBRIDGE SeismicWorking Group: Seismic velocity structure across the Fennoscandia-Sarmatia suture of the East European Craton beneath the EUROBRIDGE profile through Lithuania and Belarus, Tectonophysics, 314, 193–217, 1999.
EUROBRIDGE Working Group, and EUROBRIDGE'95: Deep seismic profiling within the East European Craton, Tectonophysics, 339, 153–175, 2001.
Franke, W. and Zelazniewicz, A.: The Eastern Termination of the Variscides: Terrane Correlation and Kinematic Evolution in Orogenic processes: quantification and modelling in the Variscan Belt, Special Publications, edited by: Franke W., Haak W., Oncken O., and Tanner, D., Geol. Soc., London, 179, 63–85, 2000.
Garetskii, R. G., Boborykin, A. M., Bogino, V. A., German, V. A., Veres, S. A., Klushin, S. V., and Shafaruk, V. G.: Deep seismic sounding on the territory of Belorussia, Geophys. J. Internat., 8, 439–448, 1990.
Gee, D. G. and Stephenson, R. A.: The European lithosphere: an introduction, in: European Lithophere Dynamics, edited by: Gee, D. G. and Stephenson, R. A., Geol. Soc. Lond. Mem., 32, 1–9, 2006.
Geissler, W. H., Sodoudi, F., and Kind, R.: Thickness of the central and eastern European lithosphere as seen by S receiver functions, Geophys. J. Int., 181, 604–634, 2010.
Grad, M. and Tripolsky, A.: Crustal structure from P and S seismic waves and petrological model of the Ukrainian shield, Tectonophysics, 250, 89–112, 1995.
Grad, M., Keller, G. R., Thybo, H., Guterch, A., and POLONAISE Working Group: Lower lithospheric structure beneath the Trans-European Suture Zone from POLONAISE'97 seismic profiles, Tectonophysics, 360, 153–168, 2002.
Grad, M., Janik, T., Guterch, A., Sroda, P., Czuba, W., and EUROBRIDGE'94–97, POLONAISE'97 and CELEBRATION 2000 Seismic Working Groups: Lithospheric structure of the western part of the East European Craton investigated by deep seismic profiles, Geol. Quart., 50, 9–22, 2006.
Gregersen, S., Pedersen, L. B., Roberts, R. G., Shomali, H., Berthelsen, A., Thybo, H., Mosegaard, K., Pedersen, T., Voss, P., Kind, R., Bock, G., Gossler, J., Wylegala, K., Rabbel, W., Woelbern, I., Budweg, M., Busche, H., Korn, M., Hock, S., Guterch, A., Grad, M., Wilde-Piorko, M., Zuchniak, M., Plomerova, J., Ansorge, J., Kissling, E., Arlitt, R., Waldhauser, F., Ziegler, P., Achauer, U., Pedersen, H., Cotte, N., Paulssen, H., and Engdahl, E. R.: Important findings expected from Europe's largest seismic array. Eos, Trans. Am. Geophys. Union, 80, 1–6, 1999.
Gregersen, S., Voss, P., Nielsen, L. V., Achauer, U., Busche, H., Rabbel, W., and Shomali, Z. H.: Uniqueness of modeling results from teleseismic P wave tomography in Project TOR, Tectonophysics, 481, 99–107, 2010.
Griffin, W. L., O'Reilly, S. Y., Abe, N., Aulbach, S., Davies, R. M., Pearson N. J., Doyle, B. J., and Kivi, K.: The origin and evolution of Archean lithospheric mantle, Precam. Res., 127, 19–41, 2003.
Guterch, A. and Grad, M.: Seismic structure of the Earth's crust between Precambrian and Variscan Europe in Poland, Publs. Inst. Geophys. Pot. Acad. Sc., M-18, 67–73, 1996.
Guterch, A. and Grad, M.: Lithospheric structure of the TESZ in Poland based on modern seismic experiments, Geol. Quart., 50, 23–32, 2006.
Guterch, A., Grad, M., Thybo, H., Keller, G. R., and the POLONAISE Working Group: POLONAISE'97 – an international seismic experiment between Precambrian and Variscan Europe in Poland, Tectonophysics 314, 101–121, 1999.
Guterch, A., Grad, M., Keller, G. R., and POLONAISE'97, CELEBRATION 2000, ALP 2002, SUDETES 2003 Working Groups: Huge contrasts of the lithospheric structure revealed by new generation seismic experiments in Central Europe, Przegld Geologiczny, 52, 2004.
Hansen, T. M. and Balling, N.: Upper-mantle reflectors: modeling of seismic wavefield characteristics and tectonic implications, Geophys. J. Int, 157, 664–682, 2004.
Johnston, A. C., Coppersmith, K. J., Kanter, L. R., and Cornell, C. A.: The earthquakes of stable continental regions. Elektric Power Institute, Report in Vol. 1: Assessment of Large Earthquake Potential, no. TR-102261-V1, 1994.
Jones, A. G., Plomerova, J., Korja, T., Sodoudi, F., and Spakman, W.: Europe from the bottom up: A statistical examination of the central and northern European lithosphere-asthenosphere boundary from comparing seismological and electromagnetic observations, Lithos, 120, 14–29, 2010.
Karousova, H., Plomerova, J., and Babuska, V.: Upper-mantle structure beneath the southern Bohemian Massif and its surroundings imaged by high-resolution tomography, Geophys. J. Int., 194, 1203–1215, https://doi.org/10.1093/gji/ggt159, 2013.
Knapmeyer-Endrun, B., Krüger, F., Legendre, C. P., Geissler, W. H., and PASSEQ Working Group: Tracing the influence of the Trans-European Suture Zone into the mantle transition zone, Earth Planet. Sci. Lett., 363, 73–87, 2013a.
Knapmeyer-Endrun, B., Krüger, and PASSEQ Working Group: Imaging the lithosphere-asthenosphere boundary across the transition from Phanerozoic Europe to the East-European Craton with S-receiver functions, Geophys. Res. Abstr., 15, EGU2013-6972, 2013b.
Korja, T.: How is the European Lithosphere Imaged by Magnetotellurics?, Surv. Geophys., 28, 239–272, .2007.
Kostyuchenko, S. L., Egorkin, A. V., and Solodilov, L. N.: Structure and genetic mechanisms of the Precambrian rifts of the East European Platform in Russia by integrated study of seismic, gravity, and magnetic data, Tectonophysics, 313, 9–28, 1999.
Koulakov, I., Kaban, M. K., Tesauro M., and Cloetingh S.: P- and S-velocity anomalies in the upper mantle beneath Europe from tomographic inversion of ISC data, Geophys. J. Int., 179, 345–366, 2009.
Legendre, C. P., Meier, T., Lebedev, S., Friederich, W., and Viereck-Götte, L.: A shear wave velocity model of the European upper mantle from automated inversion of seismic shear and surface waveforms, Geophys. J. Int., 191, 282–304, 2012.
Majda\'nski, M.: The structure of the crust in TESZ area by kriging interpolation, Acta Geophys., 60, 59–75, 2012.
Majorowicz, J. A., Čermak, V., Šafanda, J., Krzywiec, P., Wróblewska, M., Guterch, A., and Grad, M.: Heat flow models across the Trans-European Suture Zone in the area of the POLONAISE'97 seismic experiment, Phys. Chem. Earth, 28, 375–391, 2003.
Malinowski, M., Grad, M., Guterch, A., and CELEBRATION 2000 Working Group: Three-dimensional seismic modelling of the crustal structure between East European Craton and the Carpathians in SE Poland based on CELEBRATION 2000 data, Geophys. J. Int., 173, 546–565, 2008.
Matzel, E. and Grand, S. P.: The anisotropic structure of the East European platform, J. Geophys. Res., 109, B01302, https://doi.org/10.1029/2001JB000623, 2004.
McKenzie, D. P.: Some remarks on the heat flow and gravity anomalies, J. Geophys. Res., 72, 6261–6273, 1967.
Menke, W.: Geophysical data analysis: Discrete inverse theory, Academic Press, Inc., Orlando, Fl., 260 pp., 1984.
Motuza, G.: Žem\.e}s plutos bei kristalinio pamato sandaros ir sud\.eties raida, in: Lietuvos žem\.es gelmi\k{u raida ir ištekliai, edited by: Baltrūnas, V., UAB Petro ofsetas, Vilnius, 11–40, 2004.
Motuza, G.: Structure and formation of the crystalline crust in Lithuania, Mineralogical Society of Poland, Special Papers, 26, 67–79, 2005.
Motuza, G. and Staškus, V.: Seniausios Lietuvos uolienos, Geologijos akiračiai, ISSN 1392-0006, 3/4, 41–47, 2009.
Nolet, G. and Zielhuis, A.: Low S velocities under the Tornquist–Teisseyre zone: evidence from water injection into the transition zone by subduction, J. Geophys. Res., 99, 15813–15820, 1994.
Pharaoh, T. C.: Paleozoic terranes and their lithospheric boundaries within the Trans-European Suture Zone (TESZ): a review, Tectonophysics, 314, 17–41, 1999.
Pharaoh, T. C. and TESZ Project Core Group: EUROPROBE Trans-European Suture Zone project. British Geological Survey, EUROPROBE News 12, June 2000, 2000.
Pharaoh, T. C., England, R. W., Verniers, J., and Zelainiewicz, A.: Introduction: geological and geophysical studies in the Tram-European Suture Zone, Geol. Mug., 134, 585–590, 1997.
Plomerova, J. and Babuska, V.: Seismic anisotropy of the lithosphere around the Trans-European suture zone (TESZ) based on teleseismic body-wave data of the TOR experiment, Tectonophysics, 360, 89–114, 2002.
Plomerova, J. and Babuska, V.: Long memory of mantle lithosphere fabric – European LAB constrained from seismic anisotropy, Lithos, 120, 131–143, 2010.
Plomerova J., Babuška V., Sileny J., and Horalek, J.: Seismic anisotropy and velocity variations in the mantle beneath the Saxothuringicum-Moldanubicum con- tact in central Europe, in: Geodynamics of Lithosphère and Earh's Mantle: Seismic Anisotropy as a Recird of the Past and Present Dynamic Processes, edited by: Plomerova, J., Liebermann, R. C., and Babuška, V., Pure and Appi. Geoph., Special issue, 151 pp., 1998.
Plomerova, J., Kouba, D., and Babuska, V.: Mapping the lithosphere-asthenosphere boundary (LAB) through changes in surface-wave anisotropy, Tectonophysics, 358, 175–185, 2002.
Plomerova, J., Achauer, U., Babuska, V., Vecsey, L., and BOHEMA Working Group: Upper mantle beneath the Eger Rift (Central Europe): plume or asthenosphere upwelling?, Geophys. J. Int., 169, 675–682, 2007.
Plomerova, J., Babuska, V., Kozlovskaya, E., Vecsey, L., and Hyvonen, L. T.: Seismic anisotropy – a key to resolve fabrics of mantle lithosphere of Fennoscandia, Tectonophysics, 462, 125–136, 2008.
Praus, O., Pěčová, J., Petr, V., Babuska, V., and Plomerova, J.: Magnetotelluric and seismological determination of the lithosphere–asthenosphere transition in Central Europe, Phys. Earth Planet Int., 60, 212–228, 1990.
Rämö, O. T., Huhma, H., and Kirs, J.: Radiogenic Isotopes of the Estonian and Latvian Rapakivi Granite Suite: New Data from the Concealed Precambrian of the East European Craton, Precam. Res., 79, 209–226, 1996.
Sandoval, S., Kissling, E., Ansorge, J., and the SVEKALAPKO STWG: High- Resolution body wave tomography beneath the SVEKALAPKO array: I. A-priori 3-D crustal model and associated traveltime effects on teleseismic wavefronts, Geoph. J. Int., 153, 75–87, 2003.
Sandoval Castano, S.: The Lithosphere-Asthenosphere System beneath Fennoscandia (Baltic Shield) by Body-wave Tomography, A dissertation submitted to the Swiss Federal Institute of Technology Zurich, 2002.
Shomali, Z. H., Roberts, R. G., Pedersen, L. B., and the TOR Working Group: Lithospheric structure of the Tornquist Zone resolved by nonlinear P and S teleseismic tomography along the TOR array, Tectonophysics, 416, 133–149, 2006.
Skridlaite, G. and Motuza, G.: Precambrian domains in Lithuania: evidence of terrane tectonics, Tectonophysics, 339, 113–133, 2001.
Sroda, P. and the POLCRUST and PASSEQ Working Groups: Seismic anisotropy and deformations of the TESZ lithosphere near the East European Craton margin in SE Poland at various scales and depths, EGU General Assembly 2014, Geophys. Res. Abstracts, Vol. 16, EGU2014-6463-1, 2014.
Steck, L. K. and Prothero, W. A. J.: A 3-D raytracer for teleseismic body-wave arrival times, Bull. Seism. Soc. Am., 81, 1332–1339, 1991.
Tesauro, M., Kaban, M. K., and Cloetingh, S. A. P. L.: EuCRUST-07: A new reference model for the European crust, Geophys. Res. Lett., 35, L05313, https://doi.org/10.1029/2007GL32244, 2008.
Thybo, H.: Crustal structure and tectonic evolution of the Tornquist Fan region as revealed by geophysical methods, Bull. Geol. Soc. Den., 46, 145–160, 2000.
Thybo, H., Janik, T., Omelchenko, V. D., Grad, M., Garetsky, R. G., Belinsky, A. A., Karatayev, G. I., Zlotski, G., Knudsen, M. E., Sand, R., Yliniemi, J., Tiira, T., Luosto, U., Komminaho, K., Giese, R., Guterch, A., Lund, C.-E., Kharitonov, O. M., Ilchenko, T., Lysynchuk, D. V., Skobelev, V. M., and Doody, J. J.: Upper lithospheric seismic velocity structure across the Pripyat Trough and the Ukrainian Shield along the EUROBRIDGE'97 profile, Tectonophysics, 371, 41–79, 2003.
Vecsey, L., Plomerova, J., Babuska, V., and PASSEQ Working Group: Structure of the mantle lithosphere around the TESZ – from the East European Craton to the Variscan Belt. EGU General Assembly 2013, Geophys. Res. Abstracts, Vol. 15, EGU2013-3133, 2013.
Vinnik, L. P. and Ryaboy, V. Z.: Deep structure of the East European platform according to seismic data, Phys. Earth Planet. Inter., 25, 27–37, 1981.
Wagner, G. A., Gögen, K., Jonckheere, R., Wagner, I., and Woda, C.: Dating the Quarternary volcanoes Komorní Hurka (Kammerbühl) and Železná Hurka (Eisenbühl), Czech Republic, by TL, ESR, alpha-recoil and fission track chronometry, Z. Geol. Wiss., 30, 191–200, 2002.
Weiland, C. M., Steck, L. K., Dawson, P. B., and Korneev, V. A.: Nonlinear teleseismic tomography at Long Valley caldera, using three-dimensional minimum travel time ray tracing, J. Geophys. Res., 100, 20379–20390, 1995.
Wessel, P. and Smith, W.: Free software helps map and display data, EOS, Trans. Am. Union 72, 441 pp., 1991.
Wilde-Piorko, M., Grad, M., and TOR Working Group: Crustal structure variation from the Precambrian to Palaeozoic platforms in Europe imaged by the inversion of teleseismic receiver functions – project TOR, Geophys. J. Internat., 150, 261–270, 2002.
Wilde-Piórko, M., Geissler, W.H., Plomerová, J., Grad, M., Babuška, V., Brückl, E., Čyžien\.e, J., Czuba, W., Eengland, R., Gaczy\'nski, E., Gazdova, R., Gregersen, S., Guterch, A., Hanka, W., Heged\Hus, E., Heuer, B., Jedlička, P., Lazauskien\.e, J., Randy Keller, G., Kind, R., Klinge, K., Kolinsky, P., Komminaho, K., Kozlovskaya, E., Kr\Huger, F., Larsen, T., Majda\'nski, M., Málek, J., Motuza, G., Novotný, O., Pietrasiak, R., Plenefish, Th., Rŭžek, B., Šliaupa, S., \'Sroda, P., \'Swieczak, M., Tiira, T., Voss, P., and Wiejacz, P.: PASSEQ 2006–2008: PASsive Seismic Experiment in Trans-European Suture Zone, Stud. Geophys. Geod., 52, 439–448, 2008.
Wilde-Piórko, M., \'Swieczak, M., Grad, M., and Majda\'nski, M.: Integrated seismic model of the crust and upper mantle of the Trans-European Suture zone between the Precambrian craton and Phanerozoic terranes in Central Europe, Tectonophysics, 481, 108–115, 2010.
Winchester, J. A. and the PACE TMR Network Team: Paleozoic amalgamation of Central Europe: new results from recent geological and geophysical investigations, Tectonophysics, 360, 5–21, 2002.
Wüstefeld, A., Bokelmann, G., and Barruol, G.: Evidence for ancient lithospheric deformation in the East European Craton based on mantle seismic anisotropy and crustal magnetics, Tectonophysics, 481, 16–28, 2010.
Yliniemi, J., Kozlovskaya, E., Hjelt, S. E., Komminaho, K., and Ushakov, A.: Structure of the crust and uppermost mantle beneath southern Finland revealed by analysis of local events registered by the SVEKALAPKO seismic array, Tectonophysics, 394, 41–67, 2004.
Zhu, H., Bozdağ, E., Peter, D., and Tromp, J.: Structure of the European upper mantle revealed by adjoint tomography, Nat. Geosci., 5, 493–498, 2012.
Zielhuis, A. and Nolet, G.: Deep seismic expression of the ancient plate boundary in Europe, Science, New Series, 265, 79–81, 1994.
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