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© 2015. American Geophysical Union. All Rights Reserved. Fault Zone Guided Waves (FZGWs) have been observed for the first time within New Zealand's transpressional continental plate boundary, the Alpine Fault, which is late in its typical seismic cy
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::770b61c70a89a4a1e6c111edad881fc2
https://doi.org/10.26686/wgtn.13818791
https://doi.org/10.26686/wgtn.13818791
Autor:
M Zimmer, T Wiersberg, K Weaver, R Valdez, H Tobin, D Teagle, S Taylor-Offord, N Shigematsu, A Schleicher, Martha Savage, K Sauer, DJ Prior, J Paris, O Nitsch, O Nishikawa, A Niemeijer, H Mori, L Morales, J Moore, C Menzies, B Melosh, L Mathewson, E Mariani, D Mallyon, A Lukacs, T Little, W Lin, R Langridge, Y Kometani, M Kirilova, S Keys, N Kato, K Jacobs, Jamie Howarth, G Henry, A Hartog, A Gulley, J Grochowski, J Grieve, D Faulkner, JD Eccles, L Craw, SC Cox, A Coutts, A Cooper, Calum Chamberlain, B Carpenter, N Broderick, Carolyn Boulton, CM Boese, L Becroft, N Barth, LM Baratin, MJ Allen, J Williams, P Pezard, DR Schmitt, P Upton, L Remaud, L Janku-Capova, T Jeppson, J Coussens, C Massiot, B Célérier, ML Doan, VG Toy, Rupert Sutherland, John Townend
Publikováno v:
Geochemistry Geophysics Geosystems (G3)
Geochemistry, Geophysics, Geosystems
Geochemistry, Geophysics, Geosystems, AGU and the Geochemical Society, 2017, 18 (12), pp.4709-4732. ⟨10.1002/2017GC007202⟩
Geochemistry, Geophysics, Geosystems, 2017, 18 (12), pp.4709-4732. ⟨10.1002/2017GC007202⟩
GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS
Geochemistry, geophysics, geosystems, 2017, Vol.18(12), pp.4709-4732 [Peer Reviewed Journal]
Geochemistry, Geophysics, Geosystems
Geochemistry, Geophysics, Geosystems, AGU and the Geochemical Society, 2017, 18 (12), pp.4709-4732. ⟨10.1002/2017GC007202⟩
Geochemistry, Geophysics, Geosystems, 2017, 18 (12), pp.4709-4732. ⟨10.1002/2017GC007202⟩
GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS
Geochemistry, geophysics, geosystems, 2017, Vol.18(12), pp.4709-4732 [Peer Reviewed Journal]
© 2017. American Geophysical Union. All Rights Reserved. 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
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::73fe2508d0a5b8fab1eee2bce6b7290c
http://gfzpublic.gfz-potsdam.de/pubman/item/escidoc:2885899
http://gfzpublic.gfz-potsdam.de/pubman/item/escidoc:2885899