Articles | Volume 3, issue 1
https://doi.org/10.5194/se-3-97-2012
© Author(s) 2012. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/se-3-97-2012
© Author(s) 2012. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Floating stones off El Hierro, Canary Islands: xenoliths of pre-island sedimentary origin in the early products of the October 2011 eruption
V. R. Troll
Dept. of Earth Sciences, CEMPEG, Uppsala University, Sweden
Istituto Nazionale di Geofisica e Vulcanologia, Rome, Italy
A. Klügel
Institute of Geosciences, University of Bremen, Germany
M.-A. Longpré
Dept. of Earth and Planetary Sciences, McGill University, Canada
S. Burchardt
Dept. of Earth Sciences, CEMPEG, Uppsala University, Sweden
F. M. Deegan
Laboratory for Isotope Geology, Swedish Museum of Natural History, Stockholm, Sweden
Dept. of Earth Sciences, CEMPEG, Uppsala University, Sweden
J. C. Carracedo
Dept. of Physics (Geology), GEOVOL, University of Las Palmas, Gran Canaria, Spain
S. Wiesmaier
Dept. of Earth and Environmental Sciences, Ludwig-Maximilians Universität (LMU), Munich, Germany
U. Kueppers
Dept. of Earth and Environmental Sciences, Ludwig-Maximilians Universität (LMU), Munich, Germany
B. Dahren
Dept. of Earth Sciences, CEMPEG, Uppsala University, Sweden
L. S. Blythe
Dept. of Earth Sciences, CEMPEG, Uppsala University, Sweden
T. H. Hansteen
Leibniz-Institute for Oceanography, IFM-GEOMAR, Kiel, Germany
C. Freda
Istituto Nazionale di Geofisica e Vulcanologia, Rome, Italy
D. A. Budd
Dept. of Earth Sciences, CEMPEG, Uppsala University, Sweden
E. M. Jolis
Dept. of Earth Sciences, CEMPEG, Uppsala University, Sweden
E. Jonsson
Geological Survey of Sweden, Uppsala, Sweden
Dept. of Earth Sciences, CEMPEG, Uppsala University, Sweden
F. C. Meade
School of Geographical and Earth Sciences, University of Glasgow, UK
Dept. of Earth Sciences, CEMPEG, Uppsala University, Sweden
C. Harris
Department of Geological Sciences, University of Cape Town, South Africa
S. E. Berg
Dept. of Earth Sciences, CEMPEG, Uppsala University, Sweden
L. Mancini
SYRMEP Group, Sincrotrone Trieste S.C.p.A, Basovizza, Trieste, Italy
M. Polacci
Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Pisa, 56124 Pisa, Italy
K. Pedroza
Dept. of Earth Sciences, CEMPEG, Uppsala University, Sweden
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Plate tectonics theory is the motion of rocky plates (lithosphere) over ductile zones (asthenosphere). The causes of the lithosphere–asthenosphere boundary (LAB) are controversial; however, petit-spot volcanism supports the presence of melt at the LAB. We conducted geochemistry, geochronology, and geochemical modeling of petit-spot volcanoes on the western Pacific Plate, and the results suggested that carbonatite melt and recycled oceanic crust induced the partial melting at the LAB.
Matthis Frey, Claire Bossennec, Lukas Seib, Kristian Bär, Eva Schill, and Ingo Sass
Solid Earth, 13, 935–955, https://doi.org/10.5194/se-13-935-2022, https://doi.org/10.5194/se-13-935-2022, 2022
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The crystalline basement is considered a ubiquitous and almost inexhaustible source of geothermal energy in the Upper Rhine Graben. Interdisciplinary investigations of relevant reservoir properties were carried out on analogous rocks in the Odenwald. The highest hydraulic conductivities are expected near large-scale fault zones. In addition, the combination of structural geological and geophysical methods allows a refined mapping of potentially permeable zones.
Ernest Rutter, Julian Mecklenburgh, and Yusuf Bashir
Solid Earth, 13, 725–743, https://doi.org/10.5194/se-13-725-2022, https://doi.org/10.5194/se-13-725-2022, 2022
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Peleg Haruzi, Regina Katsman, Matthias Halisch, Nicolas Waldmann, and Baruch Spiro
Solid Earth, 12, 665–689, https://doi.org/10.5194/se-12-665-2021, https://doi.org/10.5194/se-12-665-2021, 2021
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Zhen M. G. Li, Hao Y. C. Wang, Qian W. L. Zhang, Meng-Yan Shi, Jun-Sheng Lu, Jia-Hui Liu, and Chun-Ming Wu
Solid Earth Discuss., https://doi.org/10.5194/se-2020-95, https://doi.org/10.5194/se-2020-95, 2020
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This manuscript provides the first evidence of ultra-high metamorphism in the Paleozoic Dunhuang orogenic belt (NW China). Though no coesite or diamond was found in the samples or in this orogen, the geothermobarometric computation results and petrographic textures all suggest that the garnet clinopyroxenite experienced ultra-high pressure metamorphism, and SIMS U-Pb dating of titanite indicates that the post peak, subsequent tectonic exhumation of the UHP rocks occurred in the Devonian.
Johannes Stefanski and Sandro Jahn
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Alice Vho, Pierre Lanari, Daniela Rubatto, and Jörg Hermann
Solid Earth, 11, 307–328, https://doi.org/10.5194/se-11-307-2020, https://doi.org/10.5194/se-11-307-2020, 2020
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This study presents an approach that combines equilibrium thermodynamic modelling with oxygen isotope fractionation modelling for investigating fluid–rock interaction in metamorphic systems. An application to subduction zones shows that chemical and isotopic zoning in minerals can be used to determine feasible fluid sources and the conditions of interaction. Slab-derived fluids can cause oxygen isotope variations in the mantle wedge that may result in anomalous isotopic signatures of arc lavas.
Xin Zhong, Evangelos Moulas, and Lucie Tajčmanová
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In this study, we present a 1-D visco-elasto-plastic model in a spherical coordinate system to study the residual pressure preserved in mineral inclusions. This allows one to study how much residual pressure can be preserved after viscous relaxation. An example of quartz inclusion in garnet host is studied and it is found that above 600–700 °C, substantial viscous relaxation will occur. If one uses the relaxed residual quartz pressure for barometry, erroneous results will be obtained.
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Solid Earth, 11, 125–159, https://doi.org/10.5194/se-11-125-2020, https://doi.org/10.5194/se-11-125-2020, 2020
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Understanding the anatomy of active magmatic plumbing systems is essential to define the heat source(s) feeding geothermal fields. Mineral-melt thermobarometry and fractional crystallization (FC) models were applied to Quaternary volcanic products of the Los Humeros Caldera (Mexico). Results point to a magmatic system controlled by FC processes and made of magma transport and storage layers within the crust, with significant implications on structure and longevity of the geothermal reservoir.
Tomoaki Morishita, Naoto Hirano, Hirochika Sumino, Hiroshi Sato, Tomoyuki Shibata, Masako Yoshikawa, Shoji Arai, Rie Nauchi, and Akihiro Tamura
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Ariadni A. Georgatou and Massimo Chiaradia
Solid Earth, 11, 1–21, https://doi.org/10.5194/se-11-1-2020, https://doi.org/10.5194/se-11-1-2020, 2020
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We study the petrographical and geochemical occurrence of magmatic sulfide minerals in volcanic rocks for areas characterised by different geodynamic settings, some of which are associated with porphyry (Cu and/or Au) and Au epithermal mineralisation. The aim is to investigate the role of magmatic sulfide saturation processes in depth for ore generation in the surface.
Massimiliano Tirone
Solid Earth, 10, 1409–1428, https://doi.org/10.5194/se-10-1409-2019, https://doi.org/10.5194/se-10-1409-2019, 2019
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The prevalent assumption in solid Earth science is that if we have different lithologies in the mantle they are separately in chemical equilibrium and together in chemical disequilibrium; this is the condition that at the moment defines a chemically heterogeneous mantle. The main contribution of this study is to show that this may not be the case. We can have (partial) chemical equilibration between the two and still observe a chemically heterogeneous mantle.
Francesco Giuntoli, Pierre Lanari, and Martin Engi
Solid Earth, 9, 167–189, https://doi.org/10.5194/se-9-167-2018, https://doi.org/10.5194/se-9-167-2018, 2018
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Continental high-pressure terranes in orogens offer insight into deep recycling and transformation processes that occur in subduction zones. These remain poorly understood, and currently debated ideas need testing. We document complex garnet zoning in eclogitic mica schists from the Sesia Zone (western Italian Alps). These retain evidence of two orogenic cycles and provide detailed insight into resorption, growth, and diffusion processes induced by fluid pulses under high-pressure conditions.
Francesco Giuntoli, Pierre Lanari, Marco Burn, Barbara Eva Kunz, and Martin Engi
Solid Earth, 9, 191–222, https://doi.org/10.5194/se-9-191-2018, https://doi.org/10.5194/se-9-191-2018, 2018
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Subducted continental terranes commonly comprise an assembly of subunits that reflect the different tectono-metamorphic histories they experienced in the subduction zone. Our challenge is to unravel how, when, and in which part of the subduction zone these subunits were juxtaposed. Our study documents when and in what conditions re-equilibration took place. Results constrain the main stages of mineral growth and deformation, associated with fluid influx that occurred in the subduction channel.
Elizaveta Kovaleva, Håkon O. Austrheim, and Urs S. Klötzli
Solid Earth, 8, 789–804, https://doi.org/10.5194/se-8-789-2017, https://doi.org/10.5194/se-8-789-2017, 2017
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This is a study of unusual coronae textures formed by zircon in granulitic metapelites, Ivrea–Verbano Zone (northern Italy). Zircon coronas occur in two generations: (1) thick (5–20 µm) crescent-shaped aggregates and (2) thin (≤ 1 µm) thread-shaped and tangled coronae. Both are found in the same petrological context, so that the difference between two generations is very conspicuous. Formation of zircon coronae is attributed to the two-stage decomposition of Fe–Ti oxides, a rich source of Zr.
Paula Ogilvie and Roger L. Gibson
Solid Earth, 8, 93–135, https://doi.org/10.5194/se-8-93-2017, https://doi.org/10.5194/se-8-93-2017, 2017
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Coronas are vital clues to the presence of arrested reaction in metamorphic rocks. We review formation mechanisms of coronas and approaches utilized to model their evolution in P–T–X space. Forward modelling employing calculated chemical potential gradients allows a far more nuanced understanding of the intricacies that govern metamorphic reaction. These models have critical implications for the limitations and opportunities coronas afford in interpreting the evolution of metamorphic terranes.
Faisal Khan, Frieder Enzmann, and Michael Kersten
Solid Earth, 7, 481–492, https://doi.org/10.5194/se-7-481-2016, https://doi.org/10.5194/se-7-481-2016, 2016
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X-ray microtomography image processing involves artefact reduction and image segmentation. The beam-hardening artefact is removed, applying a new algorithm, which minimizes the offsets of the attenuation data points. For the segmentation, we propose using a non-linear classifier algorithm. Statistical analysis was performed to quantify the improvement in multi-phase classification of rock cores using and without using our advanced beam-hardening correction algorithm.
Linda Luquot, Vanessa Hebert, and Olivier Rodriguez
Solid Earth, 7, 441–456, https://doi.org/10.5194/se-7-441-2016, https://doi.org/10.5194/se-7-441-2016, 2016
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To evaluate oil and gas production, accurate characterization (usually based on laboratory experiments) of reservoir rock properties needs to be performed. X-ray scanning samples enable obtaining 3-D images of the rock inner structure from which those properties can be obtained using images processing. This article shows that these two approaches are complementary and yield consistent results. Moreover, image-based calculations allow to save a huge amount of time compared to lab-based measures.
E. Berrezueta, B. Ordóñez-Casado, and L. Quintana
Solid Earth, 7, 37–53, https://doi.org/10.5194/se-7-37-2016, https://doi.org/10.5194/se-7-37-2016, 2016
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The aim of this article is to describe and interpret qualitative and quantitative changes at the rock matrix scale of Cretaceous sandstones (northern Spain) exposed to supercritical CO2 and brine. Experimental CO2-rich brine injection was performed in a reactor chamber under realistic conditions of deep saline formations (P ≈ 7.8 MPa, T ≈ 38 °C and 24 h exposure time). SEM and optical microscopy, aided by optical image processing and chemical analyses were used to study the rock samples.
S. Wiesmaier, D. Morgavi, C. J. Renggli, D. Perugini, C. P. De Campos, K.-U. Hess, W. Ertel-Ingrisch, Y. Lavallée, and D. B. Dingwell
Solid Earth, 6, 1007–1023, https://doi.org/10.5194/se-6-1007-2015, https://doi.org/10.5194/se-6-1007-2015, 2015
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We reproduced in an experiment the mixing of two different magmas by bubbles. Bubbles form filaments when dragging portions of one magma into another and thus mingle both magmas. Bubble mixing must be an accelerating process in nature, because formed filaments are channels of low resistance for subsequently rising bubbles. In natural gas-rich magmas, this may be an important mechanism for magma mixing. Natural samples from Axial Seamount show evidence for bubble mixing.
M. Ledevin, N. Arndt, A. Davaille, R. Ledevin, and A. Simionovici
Solid Earth, 6, 253–269, https://doi.org/10.5194/se-6-253-2015, https://doi.org/10.5194/se-6-253-2015, 2015
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We investigate the composition, physical and rheological properties of fluids at the origin of Palaeoarchean chert dikes in South Africa. The dikes formed by repetitive hydraulic fracturing as overpressured oceanic fluids were released at low temperatures as a siliceous slurry. The gelation capacity of silica conferred the chert precursor a viscoelastic, probably thixotrope behaviour. It is an additional step to understand fluid circulations towards the ocean floor, the habitat of early life.
K. Jamshidi, H. Ghasemi, V. R. Troll, M. Sadeghian, and B. Dahren
Solid Earth, 6, 49–72, https://doi.org/10.5194/se-6-49-2015, https://doi.org/10.5194/se-6-49-2015, 2015
I. V. Ashchepkov, N. V. Alymova, A. M. Logvinova, N. V. Vladykin, S. S. Kuligin, S. I. Mityukhin, H. Downes, Yu. B. Stegnitsky, S. A. Prokopiev, R. F. Salikhov, V. S. Palessky, and O. S. Khmel'nikova
Solid Earth, 5, 915–938, https://doi.org/10.5194/se-5-915-2014, https://doi.org/10.5194/se-5-915-2014, 2014
S. Bouquain, N. T. Arndt, F. Faure, and G. Libourel
Solid Earth, 5, 641–650, https://doi.org/10.5194/se-5-641-2014, https://doi.org/10.5194/se-5-641-2014, 2014
M. Nasrabady, F. Rossetti, T. Theye, and G. Vignaroli
Solid Earth, 2, 219–243, https://doi.org/10.5194/se-2-219-2011, https://doi.org/10.5194/se-2-219-2011, 2011
Cited articles
Aparicio, A., Bustillo, M. A., Garcia, R., and Araña, V.: Metasedimentary xenoliths in the lavas of the Timanfaya eruption (1730-1736, Lanzarote, Canary Islands): metamorphism and contamination processes, Geol. Mag., 143, 181–193, 2006.
Aparicio, A., Tassinari, C. C. G., Garcia, R., and Araña, V.: Sr and Nd isotope composition of the metamorphic, sedimentary and ultramafic xenoliths of Lanzarote (Canary Islands): Implications for magma sources, J. Volcanol. Geotherm. Res., 189, 143–150, 2010.
Araña, V. and Ibarrola, E.: Rhyolitic pumice in the basaltic pyroclasts from the 1971 eruption of Teneguía volcano, Canary Islands, Lithos, 6, 273–278, 1973.
Berg, S.: Constraining crustal volatile release in magmatic conduits by synchrotron X-ray μ-CT. Examensarbete vid Institutionen för geovetenskaper, Uppsala Universitet, ISSN 1650-6553 Nr. 225, 2011.
Brun, F., Mancini, L., Kasae, P., Favretto, S., Dreossi, D., and Tromba, G.: Pore3D: A software library for quantitative analysis of porous media: Nucl. Instr. Methods Phys. Res. Sect. A, 615, 326–332, 2010.
Carracedo, J. C., Rodríguez Badiola, E., Guillou, H., De La Nuez, J., and Pérez Torrado, F. J.: Geology and volcanology of La Palma and El Hierro, Western Canaries, Estudios Geológicos, 57, 1–124, 2001.
Coello, J. J.: Sobre el origen de la "restingolita", Actualidad Volcánica de Canarias- Noticias, 10 Oct 2011, http://www.avcan.org/?m=Noticias&N=911, 2011.
Collier, J. S. and Watts, A. B.: Lithospheric response to volcanic loading by the Canary Islands: constraints from seismic reflection data in their flexural moat, Geophys. J. Int., 147, 660–676, 2001.
Criado, C. and Dorta, P.: An unusual "blood rain" over the Canary Islands (Spain) The storm of January 1999, J. Arid. Environ., 55, 765–783, 1999.
Gee, M. J. R., Masson, D. G., Watts, A. B., and Allen, P. A.: The Saharan debris flow: an insight into the mechanism of long runout submarine debris flows, Sedimentology, 46, 317–335, 1999.
Gimeno, D.: Informe realizado para el Ayuntamiento de El Pinar, El Hierro, Islas Canarias, sobre un piroclasto de la erupción en curso, Internal report, 10 Oct 2011.
Guillou, H., Carracedo, J. C., Pérez Torrado, F. J., and Rodríguez Badiola, E.: K-Ar ages and magnetic stratigraphy of a hotspot-induced, fast grown oceanic island: El Hierro, Canary Islands, J. Volcanol. Geotherm. Res. 73, 141–155, 1996.
Hammer, J. E., Cashman, K. V., Hoblitt, R. P., and Newman, S.: Degassing and microlite crystallization during pre-climactic events of the 1991 eruption of Mt. Pinatubo, Philippines, Bull. Volcanol., 60, 355–380, 1999.
Hansteen, T. H. and Troll, V. R.: Oxygen isotope composition of xenoliths from the oceanic crust and volcanic edifice beneath Gran Canaria (Canary Islands): consequences for crustal contamination of ascending magmas, Chem. Geol., 193, 181–193, 2003.
Hansteen, T. H., Klügel, A., and Schmincke, H.-U.: Multi-stage magma ascent beneath the Canary Islands: evidence from fluid inclusions, Contrib. Mineral. Petrol., 132, 48–64, 1998.
Harris, C., Smith, H. S., and le Roex, A. P.: Oxygen isotope composition of phenocrysts from Tristan da Cunha and Gough Island lavas: Variation with fractional crystallization and evidence for assimilation, Contrib. Mineral. Petrol., 138, 164–175, 2000.
Harris, C., Whittingham, A. M., Milner, S. C., and Armstrong, R. A.: Oxygen isotope geochemistry of the silicic volcanic rocks of the Etendeka/Paraná Province: source constraints, Geology, 18, 1119–1121, 1990.
Hoernle, K. A.: Geochemistry of Jurassic ocean crust beneath Gran Canaria (Canary Islands): implications for crustal recycling and assimilation, J. Petrol., 39, 859–880, 1998.
IGN; Instituto Geográfico Nacional, Ministerio de Fomento, Servicio de Información Sísmica, http://www.ign.es/ign/resources/volcanologia/HIERRO.html, 2011.
Klügel, A., Hansteen, T. H., and Schmincke, H.-U.: Rates of magma ascent and depths of magma reservoirs beneath La Palma (Canary Islands), Terra Nova, 9, 117–121, 1997.
Klügel, A., Schmincke, H.-U., White, J. D. L., and Hoernle, K. A.: Chronology and volcanology of the 1949 multi-vent rift-zone eruption on la Palma (Canary Islands), J. Volcanol. Geotherm. Res., 94, 267–282, 1999.
Krastel, S. and Schmincke, H.-U.: Crustal structure of northern Gran Canaria deduced from active seismic tomography, J. Volcanol. Geotherm. Res., 115, 153–177, 2002.
McLeod, P. and Sparks, R. S. J.: The dynamics of xenolith assimilation, Contrib. Mineral. Petrol., 132, 21–33, 1998.
Pellicer, J. M.: Estudio geoquímico del vulcanismo de la isla del Hierro, Archipiélago Canario, Estudios Geol., 35, 15–29, 1979.
Perugini, D., Poli, G., Petrelli, M., De Campos C. P., and Dingwell, D. B.: Time-scales of recent Phlegrean Fields eruptions inferred from the application of a "diffusive fractionation" model of trace elements, Bull. Volcanol. 72, 431–447, 2010.
Polacci, M., Mancini, L., and Baker, D. R.: The contribution of synchrotron X-ray computed microtomography to understanding volcanic processes, J. Synchrotron Rad., 17, 215–221, https://doi.org/10.1107/S0909049509048225, 2010.
Rodriguez-Badiola, E., Pérez-Torrado, F. J., Carracedo, J. C., and Guillou, H.: Geoquímica del edificio volcanic Teide-Pico Viejo y las dorsales noreste y noroeste de Tenerife, in: Los volcanes del Parque Nacional del Teide/El Teide, Pico Viejo y las dorsales activas de Tenerife. Madrid: Organismo Autónomo Parques Nacionales Ministerio De Medio Ambiente, edited by: Carracedo, J. C., 129–186, 2006.
Savin, S. M. and Epstein, S.: The oxygen and hydrogen isotope geochemistry of ocean sediments and shales, Geochim, Cosmochim. Acta, 34, 43–63, 1969.
Schmincke, H.-U. and Graf, G.: DECOS / OMEX II, Cruise No. 43. METEOR-Berichte 20001, Univ. Hamburg, 1–99, 2000.
Sheppard, S. M. F. and Harris, C.: Hydrogen and oxygen isotope geochemistry of Ascension Island lavas and granites: variation with crystal fractionation and interaction with seawater, Contrib. Mineral. Petrol., 91, 74–81, 1985.
Sparks, R. S. J. and Marshall, L. A.: Thermal and mechanical constraints on mixing between mafic and silicic magmas, J. Volcanol. Geotherm. Res. 29, 99–124, 1986.
Stillman, C. J., Bennell-Baker, M. J., Smewing, J. D., Fuster, J. M., Muñoz, M., and Sagredo, J.: Basal complex of Fuerteventura (Canary Islands) is an oceanic intrusive complex with rift-system affinities, Nature, 257, 469–471, 1975.
Stroncik, N. A., Klügel, A., and Hansteen, T. H.: The magmatic plumbing system beneath El Hierro (Canary Islands): constraints from phenocrysts and naturally quenched basaltic glasses in submarine rocks, Contrib. Mineral. Petrol., 157, 593–607, 2009.
Sumita, M. and Schmincke, H.-U.: Tephra event stratigraphy and emplacement of volcaniclastic sediments, Mogán and Fataga stratigraphic intervals, Part I: mineral and chemical stratigraphy of volcaniclastic units and correlation to the subaerial record, in: Proc. ODP, Sci. Results, 157, College Station, TX (Ocean Drilling Program), edited by: Weaver, P. P. E., Schmincke, H.-U., Firth, J. V., and Duffield, W., 219–266, https://doi.org/10.2973/odp.proc.sr.157.114.1998, 1998.
Troll, V. R. and Schmincke, H.-U.: Magma mixing and crustal recycling recorded in ternary feldspar from compositionally zoned peralkaline ignimbrite "A", Gran Canaria, Canary Islands, J. Pet., 43, 243–270, 2002.
Troll, V. R., Sachs, P. M., Schmincke, H.-U., and Sumita, M.: The REE-Ti mineral chevkinite in comenditic magmas from Gran Canaria, Spain: a SYXRF-probe study, Contrib. Mineral. Petrol., 145, 730–741, 2003.
Vennemann, T. W. and Smith, H. S.: The rate and temperature of reaction of CLF3 with silicate minerals, and their relevance to oxygen isotope analysis, Chem. Geol., 86, 83–88, 1990.
Wiesmaier, S.: Magmatic differentiation and bimodality in oceanic island settings – implications for the petrogenesis of magma in Tenerife, Spain, PhD thesis, University of Dublin, Trinity College, 2010.
Ye, S., Canales, J. P., Rhim, R., Danobeitia, J. J., and Gallart, J.: A crustal transect through the northern and northeastern part of the volcanic edifice of Gran Canaria, Canary Islands, J. Geodyn., 28, 3–26, 1999.
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