Zobrazeno 1 - 10
of 18
pro vyhledávání: '"Samuel H. Haines"'
Autor:
Mari Hamahashi, Judith A. Hubbard, Rafael V. Almeida, Samuel H. Haines, Lewis A. Owen, Sanjita Mishra, Soma Nath Sapkota
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 23, Iss 9, Pp n/a-n/a (2022)
Abstract To investigate the subsurface structure surrounding the Main Frontal Thrust (MFT) in central Nepal, we drilled and cored sediments to depths of 45–100 m at 10 sites. Our boreholes were located along previously acquired high‐resolution se
Externí odkaz:
https://doaj.org/article/c7ef7b71c7be4073ba347a0816107509
Autor:
Soma Nath Sapkota, Samuel H Haines, Amaury Vallage, Cyrielle Guérin, Chanda Basnet Shah, Magali Riesner, Laurent Bollinger, Judith Hubbard, Marthe Lefevre, T. Kandel
Publikováno v:
Scientific Reports
Scientific Reports, Vol 11, Iss 1, Pp 1-18 (2021)
Scientific Reports, 2021, 11, pp.2553-2571. ⟨10.1038/s41598-021-00297-4⟩
Scientific Reports, Vol 11, Iss 1, Pp 1-18 (2021)
Scientific Reports, 2021, 11, pp.2553-2571. ⟨10.1038/s41598-021-00297-4⟩
The largest (M8+) known earthquakes in the Himalaya have ruptured the upper locked section of the Main Himalayan Thrust zone, offsetting the ground surface along the Main Frontal Thrust at the range front. However, out-of-sequence active structures h
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::58a782604655da7f6bebd0d822943fc4
http://europepmc.org/articles/PMC8563945
http://europepmc.org/articles/PMC8563945
Publikováno v:
Sumatra Subduction Zone
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::986aa307a617053f446558e745f7d251
https://doi.org/10.14379/iodp.proc.362.204.2020
https://doi.org/10.14379/iodp.proc.362.204.2020
Autor:
Ben A. van der Pluijm, Samuel H Haines
Publikováno v:
Geological Society of America Abstracts with Programs.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::61f6cf9aa70d9a482aeeca470943b4a4
https://doi.org/10.1130/abs/2020am-359921
https://doi.org/10.1130/abs/2020am-359921
Publikováno v:
Lithosphere. 8:587-600
Both the sources and pathways of fluid circulation are key factors to understanding the evolution of low-angle normal fault (LANF) systems and the distribution of mineral deposits in the upper crust. In recent years, several reports have shown the pr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::edfccf103eeeed42befb860a5fc77ef8
https://doi.org/10.1130/l483.1
https://doi.org/10.1130/l483.1
Publikováno v:
Earth and Planetary Science Letters. 408:57-65
The mechanics of slip on low-angle normal faults (LANFs) remain an enduring problem in structural geology and fault mechanics. In most cases, new faults should form rather than having slip occur on LANFs, assuming values of fault friction consistent
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4649ae7bf17454a90f304942730b6910
https://doi.org/10.1016/j.epsl.2014.09.034
https://doi.org/10.1016/j.epsl.2014.09.034
Publikováno v:
Journal of Structural Geology. 51:206-225
Clay-rich fault rocks have long been recognized to host distinctive fabric elements, and fault rock fabric is increasingly thought to play a fundamental role in fault mechanical behaviour in the brittle regime. Although the geometries of fabric eleme
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3841613fe43204a56f2f5e5ed21dde1b
https://doi.org/10.1016/j.jsg.2013.01.002
https://doi.org/10.1016/j.jsg.2013.01.002
Publikováno v:
Geological Society of America Abstracts with Programs.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::dd3d892f7af3d5f4dd97cab77e282f31
https://doi.org/10.1130/abs/2016am-286082
https://doi.org/10.1130/abs/2016am-286082
Publikováno v:
Geological Society of America Abstracts with Programs.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a41b0441ea76bffc8cf1a6066a899d03
https://doi.org/10.1130/abs/2016am-286047
https://doi.org/10.1130/abs/2016am-286047
Autor:
Samuel H Haines, Ben A. van der Pluijm
Publikováno v:
Journal of Structural Geology. 43:2-32
Neoformed minerals in shallow fault rocks are increasingly recognized as key to the behavior of faults in the elasto-frictional regime, but neither the conditions nor the processes which wall-rock is transformed into clay minerals are well understood
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c3f5640e48b68434ea8af33dd1cebd56
https://doi.org/10.1016/j.jsg.2012.05.004
https://doi.org/10.1016/j.jsg.2012.05.004