Zobrazeno 1 - 10
of 16
pro vyhledávání: '"Martina Kirilova"'
In August 2022, we organized a hybrid course within the European Universities “FORTHEM” Alliance, which integrated virtual and on-site teaching techniques, testing various didactic concepts that allowed simultaneous, collaborative work by groups
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::deab5e269a54cf2a94970de7798d7e48
https://doi.org/10.5194/egusphere-egu23-12309
https://doi.org/10.5194/egusphere-egu23-12309
The last two years of global pandemic forced many traditional classes to be cancelled and alternative teaching solutions to be sought, which triggered development of substantial virtual resources for training in geological field work. Virtual geology
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f75a49eb28475d729484c372fd4a3116
https://doi.org/10.5194/egusphere-egu22-5209
https://doi.org/10.5194/egusphere-egu22-5209
Autor:
Xianghui Xiao, Katrina Sauer, Richard Wirth, Soltice Morrison, François Renard, Martina Kirilova, David J. Prior, Virginia Toy, Klaus Gessner, Francesco Cappuccio, Risa Matsumura
Feedback between deformation mechanisms, fluid-rock interactions and porosity evolution in fault zone rocks has a crucial impact on their bulk rheology. Porosity formation within mid-crustal fault rocks (typically mylonites) can facilitate fluid flow
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7e348432409c2f4628bd46697c6b5243
https://doi.org/10.5194/egusphere-egu21-9399
https://doi.org/10.5194/egusphere-egu21-9399
Autor:
Steffen Abe, Virginia Toy, Till Sachau, Philipp Seelos, Sebastian G. Mutz, Selina S. Fenske, Martina Kirilova, Hagen Deckert, Paul D. Bons, Simon J. Buckley, Julian Owin, Conor Lewis, Bernhard Schuck
In September 2020, the Corona crisis offered us an opportunity to develop and test a blended real and virtual interdisciplinary field mapping class, as well as revealing the need for, and stimulating development of new web-based tools for structural
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::dbf8d31eb605888d182156e9673c4fca
https://doi.org/10.5194/egusphere-egu21-3581
https://doi.org/10.5194/egusphere-egu21-3581
Autor:
Martina Kirilova, Virginia Toy, Katrina Sauer, François Renard, Klaus Gessner, Richard Wirth, Xianghui Xiao
Porosity reduction in rocks from a fault core can cause fluid overpressure, and consequently influence the recurrence time of earthquakes. We investigated the porosity distribution in the New Zealand's Alpine Fault core in samples recovered during th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::60e4e80ddb692668581a1de0b18ebebc
https://doi.org/10.5194/se-2020-90
https://doi.org/10.5194/se-2020-90
Autor:
Cristiano Collettini, Virginia Toy, Toru Takeshita, Jeremy S. Rooney, Martina Kirilova, Carolina Giorgetti, Keith C. Gordon
Publikováno v:
Solid Earth, Vol 9, Pp 223-231 (2018)
Graphitization, or the progressive maturation of carbonaceous material, is considered an irreversible process. Thus, the degree of graphite crystallinity, or its structural order, has been calibrated as an indicator of the peak metamorphic temperatur
Autor:
Jamie Coussens, Weiren Lin, Ashley Coutts, Neil G. R. Broderick, Yusuke Kometani, Loren Mathewson, Arthur H. Hartog, Lisa Craw, Anja M. Schleicher, Naoki Kato, Simon C. Cox, Leeza Becroft, Steven Keys, Bernard Célérier, Jack N. Williams, Robert Langridge, Ben Melosh, Martin Zimmer, Jennifer Eccles, Alan Cooper, Calum J. Chamberlain, Deirdre Mallyon, Cécile Massiot, Douglas R. Schmitt, Luis Morales, Carolin Boese, Mai-Linh Doan, Harold Tobin, Carolyn Boulton, Norio Shigematsu, John Townend, M. J. Allen, André Niemeijer, Adrienn Lukacs, Daniel R. Faulkner, Robert Valdez, Damon A. H. Teagle, Julia Grochowski, David J. Prior, Phaedra Upton, Brett M. Carpenter, Anton Gulley, Nicolas C. Barth, Rupert Sutherland, G. Henry, Tamara Jeppson, Elisabetta Mariani, Jamie Howarth, Sam Taylor-Offord, Thomas Wiersberg, Martina Kirilova, Olivier Nitsch, Timothy A. Little, Katrina Sauer, Virginia Toy, Philippe Pezard, Osamu Nishikawa, Jason Grieve, Lucie Janku-Capova, Martha K. Savage, Katrina Jacobs, Jehanne Paris, C. D. Menzies, Konrad Weaver, Léa Remaud, Hiroshi Mori, Laura May Baratin, Jo Moore
Publikováno v:
Geochemistry, Geophysics, Geosystems. 18:4709-4732
Fault rock assemblages reflect interaction between deformation, stress, temperature, fluid, and chemical regimes on distinct spatial and temporal scales at various positions in the crust. Here we interpret measurements made in the hanging-wall of the