Articles | Volume 10, issue 5
Solid Earth, 10, 1621–1634, 2019
https://doi.org/10.5194/se-10-1621-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Special issue: Advances in seismic imaging across the scales
Solid Earth, 10, 1621–1634, 2019
https://doi.org/10.5194/se-10-1621-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article 02 Oct 2019
Research article | 02 Oct 2019
Improving the quality of empirical Green's functions, obtained by cross-correlation of high-frequency ambient seismic noise
Nikita Afonin et al.
Related authors
Nikita Afonin, Elena Kozlovskaya, Suvi Heinonen, and Stefan Buske
Solid Earth Discuss., https://doi.org/10.5194/se-2020-160, https://doi.org/10.5194/se-2020-160, 2020
Revised manuscript under review for SE
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
Nikita Afonin, Elena Kozlovskaya, Suvi Heinonen, and Stefan Buske
Solid Earth Discuss., https://doi.org/10.5194/se-2020-160, https://doi.org/10.5194/se-2020-160, 2020
Revised manuscript under review for SE
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, M. Majdanski, P. H. Voss, E. Kozlovskaya, and PASSEQ Working Group
Solid Earth, 6, 73–91, https://doi.org/10.5194/se-6-73-2015, https://doi.org/10.5194/se-6-73-2015, 2015
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
Related subject area
Subject area: Crustal structure and composition | Editorial team: Seismics, seismology, geoelectrics, and electromagnetics | Discipline: Geophysics
What can seismic noise tell us about the Alpine reactivation of the Iberian Massif? An example in the Iberian Central System
In situ hydromechanical responses during well drilling recorded by fiber-optic distributed strain sensing
Coherent diffraction imaging for enhanced fault and fracture network characterization
Vertical seismic profiling with distributed acoustic sensing images the Rotliegend geothermal reservoir in the North German Basin down to 4.2 km depth
Sparse 3D reflection seismic survey for deep-targeting iron-oxide deposits and their host rocks, Ludvika Mines-Sweden
Fault sealing and caprock integrity for CO2 storage: an in-situ injection experiment
Seismic evidence for failed rifting in the Ligurian Basin, Western Alpine domain
Azimuth-, angle- and frequency-dependent seismic velocities of cracked rocks due to squirt flow
Characteristics of a fracture network surrounding a hydrothermally altered shear zone from geophysical borehole logs
Bayesian full-waveform inversion of tube waves to estimate fracture aperture and compliance
Correlation of core and downhole seismic velocities in high-pressure metamorphic rocks: a case study for the COSC-1 borehole, Sweden
Prediction of seismic P-wave velocity using machine learning
Large-scale electrical resistivity tomography in the Cheb Basin (Eger Rift) at an International Continental Drilling Program (ICDP) monitoring site to image fluid-related structures
Anisotropic P-wave travel-time tomography implementing Thomsen's weak approximation in TOMO3D
Full-waveform inversion of short-offset, band-limited seismic data in the Alboran Basin (SE Iberia)
Fault interpretation in seismic reflection data: an experiment analysing the impact of conceptual model anchoring and vertical exaggeration
Quantifying the impact of the structural uncertainty on the gross rock volume in the Lubina and Montanazo oil fields (Western Mediterranean)
What happens to fracture energy in brittle fracture? Revisiting the Griffith assumption
Constraining the geotherm beneath the British Isles from Bayesian inversion of Curie depth: integrated modelling of magnetic, geothermal, and seismic data
Crustal-scale depth imaging via joint full-waveform inversion of ocean-bottom seismometer data and pre-stack depth migration of multichannel seismic data: a case study from the eastern Nankai Trough
Imaging the East European Craton margin in northern Poland using extended correlation processing of regional seismic reflection profiles
Ionian Abyssal Plain: a window into the Tethys oceanic lithosphere
Granite microporosity changes due to fracturing and alteration: secondary mineral phases as proxies for porosity and permeability estimation
3-D seismic travel-time tomography validation of a detailed subsurface model: a case study of the Záncara river basin (Cuenca, Spain)
The effect of rock composition on muon tomography measurements
Seismic imaging of dyke swarms within the Sorgenfrei–Tornquist Zone (Sweden) and implications for thermal energy storage
Juvenal Andrés, Puy Ayarza, Martin Schimmel, Imma Palomeras, Mario Ruiz, and Ramon Carbonell
Solid Earth, 11, 2499–2513, https://doi.org/10.5194/se-11-2499-2020, https://doi.org/10.5194/se-11-2499-2020, 2020
Yi Zhang, Xinglin Lei, Tsutomu Hashimoto, and Ziqiu Xue
Solid Earth, 11, 2487–2497, https://doi.org/10.5194/se-11-2487-2020, https://doi.org/10.5194/se-11-2487-2020, 2020
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Spatially continuous strain responses in two monitoring wells induced by a well-drilling process were monitored using high-resolution fiber-optic distributed strain sensing (DSS). The modeling results suggest that the strain polarities and magnitudes along the wellbores may be indicative of the layered-permeability structure or heterogeneous formation damage. The performance and value of DSS as a novel hydrogeophysical tool for in situ subsurface monitoring are emphasized.
Benjamin Schwarz and Charlotte M. Krawczyk
Solid Earth, 11, 1891–1907, https://doi.org/10.5194/se-11-1891-2020, https://doi.org/10.5194/se-11-1891-2020, 2020
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Intricate fault and fracture networks cut through the upper crust, and their detailed delineation and characterization play an important role in the Earth sciences. While conventional geophysical sounding techniques only provide indirect means of detection, we present scale-spanning field data examples, in which coherent diffraction imaging – a framework inspired by optics and visual perception – enables the direct imaging of these crustal features at an unprecedented spatial resolution.
Jan Henninges, Evgeniia Martuganova, Manfred Stiller, Ben Norden, and Charlotte M. Krawczyk
Solid Earth Discuss., https://doi.org/10.5194/se-2020-169, https://doi.org/10.5194/se-2020-169, 2020
Revised manuscript accepted for SE
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We performed a seismic survey in two 4.3 km deep geothermal research wells using the novel method of distributed acoustic sensing and wireline cables. The characteristics of the acquired data, methods for data processing and quality improvement, and interpretations on the geometry and structure of the sedimentary and volcanic reservoir rocks are presented. The method enables measurements at high temperatures and reduced cost compared to conventional sensors.
Alireza Malehmir, Magdalena Markovic, Paul Marsden, Alba Gil, Stefan Buske, Lukasz Sito, Emma Bäckström, Martiya Sadeghi, and Stefan Luth
Solid Earth Discuss., https://doi.org/10.5194/se-2020-141, https://doi.org/10.5194/se-2020-141, 2020
Revised manuscript accepted for SE
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A smooth transition toward decarbonization demands access to more minerals of critical importance. Europe has a good geology for many of these mineral deposits but at depth requiring sensitive, environmentally-friendly and cost-effective methods for their exploration. In this context, we present a sparse 3D seismic dataset that allowed identification of potential iron-oxide resources at depth and helped to characterise key geological structures as well as a historical tailing in central Sweden.
Alba Zappone, Antonio Pio Rinaldi, Melchior Grab, Quinn Wenning, Clément Roques, Claudio Madonna, Anne Obermann, Stefano M. Bernasconi, Florian Soom, Paul Cook, Yves Guglielmi, Christophe Nussbaum, Domenico Giardini, and Stefan Wiemer
Solid Earth Discuss., https://doi.org/10.5194/se-2020-100, https://doi.org/10.5194/se-2020-100, 2020
Revised manuscript accepted for SE
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The success of geological storage of carbon dioxide is linked to the availability at depth of a capable reservoir and of an impermeable caprock. The sealing capacity of the caprock is a key parameter for the long-term CO2 containment. Faults crosscutting the caprock might represent preferential pathways for CO2 to escape. A decameter scale experiment of injection in a fault, monitored by an integrated network of multi-paramerter sensors shed light to the mobility of fluids within the fault.
Anke Dannowski, Heidrun Kopp, Ingo Grevemeyer, Dietrich Lange, Martin Thorwart, Jörg Bialas, and Martin Wollatz-Vogt
Solid Earth, 11, 873–887, https://doi.org/10.5194/se-11-873-2020, https://doi.org/10.5194/se-11-873-2020, 2020
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The Ligurian Sea opened ~30–15 Ma during the SE migration of the Calabrian subduction zone. Seismic travel time tomography reveals the absence of oceanic crust, documenting that the extension of continental lithosphere stopped before seafloor spreading initiated. The extension led to extreme crustal thinning and possibly exhumed mantle accompanied by syn-rift sedimentation. Our new interpretation of the crust's nature is important for plate reconstruction modelling related to the Alpine orogen.
Yury Alkhimenkov, Eva Caspari, Simon Lissa, and Beatriz Quintal
Solid Earth, 11, 855–871, https://doi.org/10.5194/se-11-855-2020, https://doi.org/10.5194/se-11-855-2020, 2020
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We perform a three-dimensional numerical study of the fluid–solid deformation at the pore scale. We show that seismic wave velocities exhibit strong azimuth-, angle- and frequency-dependent behavior due to squirt flow between interconnected cracks. We conclude that the overall anisotropy mainly increases due to squirt flow, but in some specific planes it can locally decrease as well as increase, depending on the material properties.
Eva Caspari, Andrew Greenwood, Ludovic Baron, Daniel Egli, Enea Toschini, Kaiyan Hu, and Klaus Holliger
Solid Earth, 11, 829–854, https://doi.org/10.5194/se-11-829-2020, https://doi.org/10.5194/se-11-829-2020, 2020
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A shallow borehole was drilled to explore the petrophysical and hydraulic characteristics of a hydrothermally active fault in the crystalline Aar massif of the Alps. A key objective of studying surficial features of this kind is to establish analogies with natural and deep-seated engineered hydrothermal systems. A wide range of geophysical borehole logs was acquired, which revealed a complex fracture network in the damage zone of the fault and a related compartmentalized hydraulic behavior.
Jürg Hunziker, Andrew Greenwood, Shohei Minato, Nicolás Daniel Barbosa, Eva Caspari, and Klaus Holliger
Solid Earth, 11, 657–668, https://doi.org/10.5194/se-11-657-2020, https://doi.org/10.5194/se-11-657-2020, 2020
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The characterization of fractures is crucial for a wide range of pertinent applications, such as geothermal energy production, hydrocarbon exploration, CO2 sequestration, and nuclear waste disposal. We estimate fracture parameters based on waves that travel along boreholes (tube waves) using a stochastic optimization approach.
Felix Kästner, Simona Pierdominici, Judith Elger, Alba Zappone, Jochem Kück, and Christian Berndt
Solid Earth, 11, 607–626, https://doi.org/10.5194/se-11-607-2020, https://doi.org/10.5194/se-11-607-2020, 2020
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Knowledge about physical properties at depth is crucial to image and understand structures linked with orogenic processes. We examined seismic velocities from core and downhole data from the COSC-1 borehole, Sweden, and calibrated our results with laboratory measurements on core samples. Despite a strong mismatch between the core and downhole velocities due to microcracks, mafic units are resolved at all scales, while at sample scale, strong seismic anisotropy correlates with the rock foliation.
Ines Dumke and Christian Berndt
Solid Earth, 10, 1989–2000, https://doi.org/10.5194/se-10-1989-2019, https://doi.org/10.5194/se-10-1989-2019, 2019
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Knowing the velocity with which seismic waves travel through the top of the crust is important both for identifying anomalies, e.g. the presence of resources, and for geophysical data evaluation. Traditionally this has been done by using empirical functions. Here, we use machine learning to derive better seismic velocity estimates for the crust below the oceans. In most cases this methods performs better than empirical averages.
Tobias Nickschick, Christina Flechsig, Jan Mrlina, Frank Oppermann, Felix Löbig, and Thomas Günther
Solid Earth, 10, 1951–1969, https://doi.org/10.5194/se-10-1951-2019, https://doi.org/10.5194/se-10-1951-2019, 2019
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An active CO2 degassing site in the western Eger Rift, Czech Republic, was investigated with a 6.5 km long geophysical survey using a specific large-scale geoelectrical setup, supported by shallow geoelectrical surveys and gravity measurements. The experiment reveals unusually low resistivities in the sediments and basement below the degassing area of less than 10 Ω and provides a base for a custom geological model of the area for a future 400 m deep research drilling in this area.
Adrià Meléndez, Clara Estela Jiménez, Valentí Sallarès, and César R. Ranero
Solid Earth, 10, 1857–1876, https://doi.org/10.5194/se-10-1857-2019, https://doi.org/10.5194/se-10-1857-2019, 2019
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A new code for anisotropic travel-time tomography is presented. We describe the equations governing the anisotropic ray propagation algorithm and the modified inversion solver. We study the sensitivity of two medium parameterizations and compare four inversion strategies on a canonical model. This code can provide better understanding of the Earth's subsurface in the rather common geological contexts in which seismic velocity displays a weak dependency on the polar angle of ray propagation.
Clàudia Gras, Daniel Dagnino, Clara Estela Jiménez-Tejero, Adrià Meléndez, Valentí Sallarès, and César R. Ranero
Solid Earth, 10, 1833–1855, https://doi.org/10.5194/se-10-1833-2019, https://doi.org/10.5194/se-10-1833-2019, 2019
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We present a workflow that combines different geophysical techniques, showing that a detailed seismic velocity model can be obtained even for non-optimal data sets, i.e. relatively short-offset, band-limited streamer data recorded in deep water. This fact has an important implication for the Marine seismic community, suggesting that many of the existing data sets should be revisited and analysed with new techniques to enhance our understanding of the subsurface, as in the Alboran Basin case.
Juan Alcalde, Clare E. Bond, Gareth Johnson, Armelle Kloppenburg, Oriol Ferrer, Rebecca Bell, and Puy Ayarza
Solid Earth, 10, 1651–1662, https://doi.org/10.5194/se-10-1651-2019, https://doi.org/10.5194/se-10-1651-2019, 2019
Carla Patricia Bárbara, Patricia Cabello, Alexandre Bouche, Ingrid Aarnes, Carlos Gordillo, Oriol Ferrer, Maria Roma, and Pau Arbués
Solid Earth, 10, 1597–1619, https://doi.org/10.5194/se-10-1597-2019, https://doi.org/10.5194/se-10-1597-2019, 2019
Timothy R. H. Davies, Maurice J. McSaveney, and Natalya V. Reznichenko
Solid Earth, 10, 1385–1395, https://doi.org/10.5194/se-10-1385-2019, https://doi.org/10.5194/se-10-1385-2019, 2019
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Griffith (1921) assumed that energy used to create new surface area by breaking intact rock immediately becomes surface energy which is not available for further breakage. Our lab data disprove this assumption; we created much more new surface area, 90 % on submicron fragments, than the energy involved should allow. As technology allows ever smaller fragments to be measured, continued use of the Griffith assumption will lead to incorrect energy budgets for earthquakes and rock avalanches.
Ben Mather and Javier Fullea
Solid Earth, 10, 839–850, https://doi.org/10.5194/se-10-839-2019, https://doi.org/10.5194/se-10-839-2019, 2019
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The temperature in the crust can be constrained by the Curie depth, which is often interpreted as the 580 °C isotherm. We cast the estimation of Curie depth, from maps of the magnetic anomaly, within a Bayesian framework to properly quantify its uncertainty across the British Isles. We find that uncertainty increases considerably for deeper Curie depths, which demonstrates that generally this method is only reliable in hotter regions, such as Scotland and Northern Ireland.
Andrzej Górszczyk, Stéphane Operto, Laure Schenini, and Yasuhiro Yamada
Solid Earth, 10, 765–784, https://doi.org/10.5194/se-10-765-2019, https://doi.org/10.5194/se-10-765-2019, 2019
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In order to broaden our knowledge about the deep lithosphere using seismic methods, we develop leading-edge imaging workflows integrating different types of data. Here we exploit the complementary information carried by seismic wavefields, which are fundamentally different in terms of acquisition setting. We cast this information into our processing workflow and build a detailed model of the subduction zone, which is subject to further geological interpretation.
Miłosz Mężyk, Michał Malinowski, and Stanisław Mazur
Solid Earth, 10, 683–696, https://doi.org/10.5194/se-10-683-2019, https://doi.org/10.5194/se-10-683-2019, 2019
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The Precambrian East European Craton is one of the most important building blocks of the European plate. Unlike in Scandinavia, its crystalline crust in Poland is concealed beneath younger sediments. Reprocessing of ca. 950 km regional reflection seismic profiles acquired during shale gas exploration in NE Poland revealed reflectivity patterns interpreted as signs of Svekofennian orogeny, proving a similar mechanism of Paleoproterozoic crustal formation across the Baltic Sea.
Anke Dannowski, Heidrun Kopp, Frauke Klingelhoefer, Dirk Klaeschen, Marc-André Gutscher, Anne Krabbenhoeft, David Dellong, Marzia Rovere, David Graindorge, Cord Papenberg, and Ingo Klaucke
Solid Earth, 10, 447–462, https://doi.org/10.5194/se-10-447-2019, https://doi.org/10.5194/se-10-447-2019, 2019
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The nature of the Ionian Sea crust has been the subject of scientific debate for more than 30 years. Seismic data, recorded on ocean bottom instruments, have been analysed and support the interpretation of the Ionian Abyssal Plain as a remnant of the Tethys oceanic lithosphere with the Malta Escarpment as a transform margin and a Tethys opening in the NNW–SSE direction.
Martin Staněk and Yves Géraud
Solid Earth, 10, 251–274, https://doi.org/10.5194/se-10-251-2019, https://doi.org/10.5194/se-10-251-2019, 2019
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Granite is suitable to host geothermal wells or disposals of hazardous waste and in these cases the rock porosity and permeability are critical. Our detailed porosity and permeability data on variously deformed Lipnice granite yield a span of 5 orders of magnitude in permeability between the least and the most deformed facies. To facilitate the estimation of porosity and permeability in similar settings, we provide optical and chemical data on the characteristic minerals of each facies.
David Marti, Ignacio Marzan, Jana Sachsenhausen, Joaquina Alvarez-Marrón, Mario Ruiz, Montse Torne, Manuela Mendes, and Ramon Carbonell
Solid Earth, 10, 177–192, https://doi.org/10.5194/se-10-177-2019, https://doi.org/10.5194/se-10-177-2019, 2019
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A detailed knowledge of the very shallow subsurface has become of crucial interest for modern society, especially if it hosts critical surface infrastructures such as temporary waste storage sites. The use of indirect methods to characterize the internal structure of the subsurface has been successfully applied, based on the 3-D distribution of seismic velocities and well-log data, which are of great interest for civil engineering companies.
Alessandro Lechmann, David Mair, Akitaka Ariga, Tomoko Ariga, Antonio Ereditato, Ryuichi Nishiyama, Ciro Pistillo, Paola Scampoli, Fritz Schlunegger, and Mykhailo Vladymyrov
Solid Earth, 9, 1517–1533, https://doi.org/10.5194/se-9-1517-2018, https://doi.org/10.5194/se-9-1517-2018, 2018
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Muon tomography is a technology, similar to X-ray tomography, to image the interior of an object, including geologically interesting ones. In this work, we examined the influence of rock composition on the physical measurements, and the possible error that is made by assuming a too-simplistic rock model. We performed numerical simulations for a more realistic rock model and found that beyond 300 m of rock, the composition starts to play a significant role and has to be accounted for.
Alireza Malehmir, Bo Bergman, Benjamin Andersson, Robert Sturk, and Mattis Johansson
Solid Earth, 9, 1469–1485, https://doi.org/10.5194/se-9-1469-2018, https://doi.org/10.5194/se-9-1469-2018, 2018
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Interest and demand for green-type energy usage and storage are growing worldwide. Among several, thermal energy storage that stores energy (excess heat or cold) in fluids is particularly interesting. For an upscaling purpose, three seismic profiles were acquired within the Tornquist suture zone in the southwest of Sweden and historical crustal-scale offshore BABEL lines revisited. A number of dykes have been imaged and implications for the storage and tectonic setting within the zone discussed.
Cited articles
Baig, A., Campillo, M., and Brenguier, F.: Denoising seismic noise cross
correlations, J. Geophys. Res., 114, 2156–2202,
https://doi.org/10.1029/2008JB006085, 2009.
Barazza, F., Malisan, P., and Carniel, R.: Improvement of H/V technique by
rotation of the coordinate system, Commun. Nonlinear Sci., 14, 182–193, 2009.
Bensen, G. D., Ritzwoller, M. H., Barmin, M. P., Levshin, A. L., Lin, F.,
Moschetti, M. P., and Yang, Y.: Processing seismic ambient noise data to
obtain reliable broad-band surface wave dispersion measurements, Geophys.
J. Int., 169, 1239–1260, 2007.
Boué, P., Poli, P., Campillo, M. P., and Roux, P.: Reverberations, coda
waves and ambient noise: Correlations at the global scale and retrieval of
the deep phases, Earth Planet. Sc. Lett., 391, 137–145,
https://doi.org/10.1016/j.epsl.2014.01.047, 2014.
Bruneton, M., Pedersen, H. A., Farra, V., Arndt, N. T., Vacher, P., Achauer,
U., and Grad, M.: Complex lithospheric structure under the central Baltic
Shield from surface wave tomography, J. Geophys. Res.-Sol.
Ea., 109, B10303, https://doi.org/10.1029/2003JB002947, 2004.
Campillo, M.: Phase and correlation of “random” seismic fields and the
reconstruction of the Green function, Pure Applied Geophysics, 163,
475–502, https://doi.org/10.1007/s00024-005-0032-8, 2006.
Cheng, F., Xia, J., Xu, Y., Xu, Z., and Pan, Y.: A new passive seismic
method based on seismic interferometry and multichannel analysis of surface
waves, J. Appl. Geophys., 117, 126–135, 2015.
Dortman, N. B.: Petrophysics. A Handbook, Book 1, Rocks and Minerals, Nedra, Moscow, 1992.
Douze, E. J. and Laster, S. J.: Statistics of semblance, Geophysics, 44,
1999–2003, https://doi.org/10.1190/1.1440953, 1979.
Groos, J. C., Bussat, S., and Ritter, J. R. R.: Performance of different
processing schemes in seismic noise cross-correlations, Geophys. J.
Int., 188, 498–512, 2012.
Heinonen, S., Imaña, M., Snyder, D. B., Kukkonen, I. T., and Heikkinen, P. J.:
Seismic reflection profiling of the Pyhäsalmi
VHMS-deposit: A complementary approach to the deep base metal exploration in
Finland, Geophysics, 77, WC15–WC23, 2012.
Janik, T., Kozlovskaya, E., Heikkinen, P., Yliniemi, J., and Silvennoinen,
H.: Evidence for preservation of crustal root beneath the Proterozoic
Lapland-Kola orogen (northern Fennoscandian shield) derived from P and S
wave velocity models of POLAR and HUKKA wide-angle reflection and refraction
profiles and FIRE4 reflection transect, J. Geophys. Res.-Sol. Ea., 114, B06308, https://doi.org/10.1029/2008JB005689, 2009.
Kobranova, W. N.: Petrophysics, Nedra, Moscow, 1986.
Kukkonen, I., Heikkinen, P., Elo, S., Heinonen, S.,Laitinen, J., and HIRE
Working Group of the Geological Survey of Finland: HIRE Seismic Reflection
Survey in the Kemi Cr mining area, northern Finland, Report Q23/2009/64,
2009.
Lehtonen, M. and O'Brien, H.: Mantle transect of the Karelian Craton from
margin to core based on PT data from garnet and clinopyroxene xenocrysts in
kimberlites, Bulletin of Geological Society of Finland, 81, 79–102, 2009.
Li, G., Niu, F., Yang, Y., and Xie, J.: An investigation of time–frequency
domain phase-weighted stacking and its application to phase-velocity
extraction from ambient noise's empirical Green's functions, Geophys.
J. Int., 212, 1143–1156, 2018.
Liu, X., Ben-Zion, Y., and Zigone, D.: Frequency domain analysis of errors
in cross-correlations of ambient seismic noise, Geophysical Supplements to
the Monthly Notices of the Royal Astronomical Society, 207, 1630–1652,
2016.
Malehmir, A., Durrheim, R., Bellefleur, G., Urosevic, M., Juhlin, C., White,
D. J., Milkereit, B., and Campbell, G.: Seismic methods in mineral exploration and
mine planning: A general overview of past and present case histories and a
look into the future, Geophysics, 77, WC173–WC190, 2012.
Mulargia, F.: The seismic noise wavefield is not diffuse, J.
Acoust. Soc. Am., 131, 2853–2858, 2012.
Nakamura, Y.: A method for dynamic characteristics estimation of subsurface
using microtremor on the ground surface, QR Railway Tech. Res. Inst., 30,
25–33, 1989.
Nakata, N., Chang, J. P., Lawrence, J. F., and Boué, P.: Body wave
extraction and tomography at Long Beach, California, with ambient-noise
interferometry, J. Geophys. Res.-Sol. Ea., 120,
1159–1173, 2015.
Neidell, N. and Turhan Taner, M.: Semblance and other coherency measures
for multichannel data, Geophysics, 36, 482–497, 1971.
Panea, I., Draganov, D., Almagro Vidal, C., and Mocanu, V.: Retrieval of
reflections from ambient noise recorded in the Mizil area, Romania,
Geophysics, 79, Q31–Q42, 2014.
Place, J. A. P., Malehmir, A., Högdahl, K., Juhlin, C., and
Persson Nilsson, K.: Seismic characterization of the Grängesberg iron deposit and its mining-induced structures, central Sweden:
Interpretation, 3, SY41–SY56, https://doi.org/10.1190/INT-2014-0212.1, 2015.
Poli, P., Pedersen, H. A., Campillo, M., and the POLENET/LAPNET Working
Group: Emergence of body waves from cross-correlation of short period
seismic noise, Geophys. J. Int., 188, 549–588, 2012a.
Poli, P., Pedersen, H., Campillo, M., and LAPNET Working Group: Body-wave
imaging of Earth's mantle discontinuities from ambient seismic noise,
Science, 338, 1063–1065, https://doi.org/10.1126/science.1228194, 2012b.
Poli, P., Campillo, M., Pedersen, H., and the POLENET/LAPNET Working Group:
Noise directivity and group velocity tomography in a region with small
velocity contrasts: the northern Baltic shield application to the northern
Baltic Shield, Geophys. J. Int., 192, 413–424, https://doi.org/10.1093/gji/ggs034, 2013.
Phạm, T.-S., Tkalčić, H., Sambridge, M., and Kennett, B. L. N.: Earth's
correlation wavefield: Late coda correlation, Geophys. Res. Lett.,
45, 3035–3042, https://doi.org/10.1002/2018GL077244, 2018.
Rost, S. and Thomas, C.: Array seismology: methods and applications, Rev.
Geophys., 40, 2-1–2-27, https://doi.org/10.1029/2000RG000100, 2002.
Sambridge, M.: Geophysical inversion with a neighbourhood algorithm – I.
Searching a parameter space, Geophys. J. Int., 138,
479–494, 1999.
Schimmel, M., Stitsmann, E., and Gallart, J.: Using instantaneous phase
coherence for signal extraction from ambient noise data at a local to a
global scale, Geophys. J. Int., 184, 494–506, 2011.
Schweitzer, J., Fyen, J., Mykkeltveit, S., Gibbons, S. J., Pirli, M.,
Kühn, D., and Kværna, T.: Seismic Arrays in New Manual of
Seismological Observatory Practice (NMSOP-2), German Research Centre for
Geosciences, ISBN 3-9808780-0-7.9, 1–80, 2012.
Shapiro, N. M. and Campillo, M.: Emergence of broadband Rayleigh waves from
correlations of the ambient seismic noise, Geophys. Res. Lett., 31, L07614, https://doi.org/10.1029/2004GL019491,
2004.
Shirzad, T. and Shomali, Z. H.: Extracting seismic body and Rayleigh waves
from the ambient seismic noise using the rms-stacking method, Seismol.
Res. Lett., 86, 173–180, 2015.
Silvennoinen, A.: Kuusamon ja Rukatunturin kartta-alueiden kalliopera –
Espoo, Geological Survey of Finland, Espoo, Finland, 1991.
Silvennoinen, H. and Kozlovskaya, E.: 3D structure and physical properties
of the Kuhmo Greenstone Belt (eastern Finland): Constraints from gravity
modelling and seismic data and implications for the tectonic setting,
J. Geodyn., 43, 358–373, 2007.
Silvennoinen, H., Kozlovskaya, E., Kissling, E., Kosarev, G., and
POLENET/LAPNET working group: A new Moho boundary map for the northern
Fennoscandian Shield based on combined controlled-source seismic and
receiver function data, GeoResJ, 1, 19–32, 2014.
Tiira, T., Janik, T., Kozlovskaya, E., Grad, M., Korja, A., Komminaho, K.,
and Brückl, E.: Crustal Architecture of the Inverted Central Lapland
Rift along the HUKKA 2007 Profile, Pure Appl. Geophys., 171,
1129–1152, 2014.
Ventosa, S., Schimmel, M., and Stutzmann, E.: Extracting surface waves, hum and
normal modes: time-scale phase-weighted stack and beyond, Geophys. J. Int.,
211, 30–44, https://doi.org/10.1093/gji/ggx284, 2017.
Vidal, C. A., Draganov, D., Van der Neut, J., Drijkoningen, G., and
Wapenaar, K.: Retrieval of reflections from ambient noise using illumination
diagnosis, Geophys. J. Int., 198, 1572–1584, 2014.
Vinnik, L., Oreshin, S., Makeyeva, L., Peregoudov, D., Kozlovskaya, E.,
Pedersen, H., and Jämsen, T.: Anisotropic lithosphere under the
Fennoscandian shield from P receiver functions and SKS waveforms of the
POLENET/LAPNET array, Tectonophysics, 628, 45–54, 2014.
Wapenaar, K., Draganov, D., and Robertsson, J. (Eds.): Seismic
interferometry: History and present status, Society of Exploration
Geophysicists, Geophysics Reprint Series No. 26, ISBN 978-1-56080-150-4,
2008.
Wapenaar, K., Draganov, D., Snieder, R., Campman, X., and Verdel, A.:
Tutorial on seismic interferometry: Part 1 – Basic principles and
applications, Geophysics, 75, 75A195, https://doi.org/10.1190/1.3457445, 2010.
Weihed, P., Arndt, N., Billström, K., Duchesne, J.-C., Eilu, P.,
Martinsson, O., Papunen, H., and Lahtinen, R.: Precambrian geodynamics and ore
formation: The Fennoscandian Shield, Ore Geol. Rev., 27,
273–322, https://doi.org/10.1016/j.oregeorev.2005.07.008, 2005.
Yliniemi, J., Kozlovskaya, E., Hjelt, S. E., Komminaho, K., Ushakov, A., and
SVEKALAPKO Seismic Tomography Working Group: 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.
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