Hundalee Fault, North Canterbury, New Zealand: Late Quaternary activity and regional tectonics_Supplementary Information

Autor: Barrell, David J.A., Stirling, Mark W., Williams, Jack N., Sauer, Katrina M., van den Berg, Ella J.

This document is a Supplement to the paper: Barrell, DJA, Stirling MW, Williams JN, Sauer KM, van den Berg E. Hundalee Fault, North Canterbury, New Zealand: Late Quaternary activity and regional tectonics. New Zealand Journal of Geology and Geophysic

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::40bb5b400465363561cb27d3ebc5732d

Micro- And nano-porosity of the active Alpine Fault zone, New Zealand

Autor: Kirilova, Martina, Toy, Virginia, Sauer, Katrina, Renard, Francois, Gessner, Klaus, Wirth, Richard, Xiao, Xianghui, Matsumura, Risa

Publikováno v: Kirilova, Martina Toy, Virginia Sauer, Katrina Renard, Francois Gessner, Klaus Wirth, Richard Xiao, Xianghui Matsumura, Risa . Micro- And nano-porosity of the active Alpine Fault zone, New Zealand. Solid Earth (SE). 2020, 11(6), 2425-2438
Solid Earth (SE)

Externí odkaz: http://hdl.handle.net/10852/85740
https://www.duo.uio.no/bitstream/handle/10852/85740/2/se-11-2425-2020.pdf

Evolution of microporosity and permeability of quartzofeldspathic rocks during changes in crustal conditions and tectonite fabric

Autor: Toy, Virginia, Adam, Ludmila, Gerbi, Christopher, Hellmann, Roland, Johnson, Scott, Kirilova, Martina, Kluge, Emma, Lockner, David, Plümper, Oliver, Sauer, Katrina, Song, Won Joon, Wirth, Richard

Publikováno v: EGU
EGU, May 2019, Vienna, Austria. pp.2019-4596

International audience; Most crustal rocks contain some microporosity that can host fluids and allow them to permeate, which in turn impacts their physical properties and rheology. Using electron microscopic methods we have examined the nature of mic

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::de31ef4cc9bacde9d572dc16559eacea
https://hal.archives-ouvertes.fr/hal-02353136

Extreme hydrothermal conditions at an active plate-bounding fault

Autor: Sutherland, Rupert, Townend, John, Toy, Virginia, Upton, Phaedra, Coussens, Jamie, Allen, Michael, Baratin, Laura-May, Barth, Nicolas, Becroft, Leeza, Boese, Carolin, Boles, Austin, Boulton, Carolyn, Broderick, Neil GR, Janku-Capova, Lucie, Carpenter, Brett M, Célérier, Bernard, Chamberlain, Calum, Cooper, Alan, Coutts, Ashley, Cox, Simon, Craw, Lisa, Doan, Mai-Linh, Eccles, Jennifer, Faulkner, Dan, Grieve, Jason, Grochowski, Julia, Gulley, Anton, Hartog, Arthur, Howarth, Jamie, Jacobs, Katrina, Jeppson, Tamara, Kato, Naoki, Keys, Steven, Kirilova, Martina, Kometani, Yusuke, Langridge, Rob, Lin, Weiren, Little, Timothy, Lukacs, Adrienn, Mallyon, Deirdre, Mariani, Elisabetta, Massiot, Cécile, Mathewson, Loren, Melosh, Ben, Menzies, Catriona, Moore, Jo, Morales, Luiz, Morgan, Chance, Mori, Hiroshi, Niemeijer, Andre, Nishikawa, Osamu, Prior, David, Sauer, Katrina, Savage, Martha, Schleicher, Anja, Schmitt, Douglas R, Shigematsu, Norio, Taylor-Offord, Sam, Teagle, Damon, Tobin, Harold, Valdez, Robert, Weaver, Konrad, Wiersberg, Thomas, Williams, Jack, Woodman, Nick, Zimmer, Martin

Publikováno v: Nature, vol 546, iss 7656

Temperature and fluid pressure conditions control rock deformation and mineralization on geological faults, and hence the distribution of earthquakes. Typical intraplate continental crust has hydrostatic fluid pressure and a near-surface thermal grad

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::89b465ad6584a3131322a6a7e7b390a3
https://escholarship.org/uc/item/5345t6p6

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