Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Effat Behboudi"'
Publikováno v:
Journal of Petroleum Science and Technology, Vol 8, Iss 3, Pp 42-52 (2018)
The presence of gas hydrate and associated gas in the Makran Accretionary Prism, offshore Iran, has been confirmed by various seismic indicators, including the bottom-simulating reflector (BSR), amplitude blanking, and bright spot. The pre-stack anal
Externí odkaz:
https://doaj.org/article/5b226c5309384d9295ae5355b24aacca
Quantitative stress data is crucial to understanding the mechanical behaviour of faults and the variation of interface slip behaviours at subduction zones. The Hikurangi Subduction Margin (HSM), New Zealand is characterized by along-strike variations
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::27bc20ae59debe9cdaf9469ca2e7e5c6
https://doi.org/10.5194/egusphere-egu23-8512
https://doi.org/10.5194/egusphere-egu23-8512
Quantifying tectonic stress magnitudes is crucial in understanding crustal deformation processes, fault geomechanics, and variable plate interface slip behaviors in subduction zones. The Hikurangi Subduction Margin (HSM), New Zealand is characterized
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3a35efe3d69beb978118632ed52f31b4
https://doi.org/10.22541/essoar.167169871.10981139/v1
https://doi.org/10.22541/essoar.167169871.10981139/v1
Quantifying the contemporary stress state of the Earth’s crust is critical for developing a geomechanical understanding of the behavior of brittle deformation (fractures and faults).In this study we characterize the shallow contemporary stress stat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::552732fafb124ccb3a042ea012c01fb8
https://doi.org/10.5194/egusphere-egu22-8802
https://doi.org/10.5194/egusphere-egu22-8802
Knowledge of the contemporary in-situ stress orientations in the Earth's crust can improve our understanding of active crustal deformation, geodynamic processes, and seismicity in tectonically acti...
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c17a5bdb547326c1b5a152bdbbc0a7dd
https://doi.org/10.1002/essoar.10508845.1
https://doi.org/10.1002/essoar.10508845.1
The state of stress in the shallow crust of the Hikurangi Subduction Margin hangingwall, New Zealand
Knowledge of in situ stress fields is critical for a better understanding of deformation, faulting regime, and earthquake processes in seismically active margins such as the Hikurangi Subduction Margin (HSM), North Island, New Zealand. In this study,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e8e509b6d714c01f391ddb099ba2d577
https://doi.org/10.5194/egusphere-egu21-10217
https://doi.org/10.5194/egusphere-egu21-10217
Autor:
P. Barnes, H. Lee, Effat Behboudi, M. Paganoni, Katerina Petronotis, Leah J. LeVay, David D. McNamara, Ake Fagereng, Ingo Pecher, Heather M. Savage, Laura M. Wallace, Demian M. Saffer, Hung Yu Wu, Ann E. Cook, G. Kim
Publikováno v:
Geophysical Research Letters
We constrain orientations of the horizontal stress field from borehole image data in a transect across the Hikurangi Subduction Margin. This region experiences NW‐SE convergence and is the site of recurrent slow slip events. The direction of the ho
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7124863ed71f3c2873c85b5ed57c5aa1
Autor:
Effat Behboudi, Ivan Lokmer, David McNamara, Tom Manzocchi, Laura Wallace, Demian Saffer, Philip Barnes, Ingo Pecher, Hikweon Lee, Gil Young Kim, Hung-Yu Wu, Katerina Petronotis, Leah LeVay, Iodp Expedition372 Scientists, Iodp Expedition375 Scientists
The Hikurangi Subduction Margin (HSM) of New Zealand is well-known for its variable seismic behaviour along strike, and across the Pacific-Australian subduction interface. Pacific-Australian plate motion is accommodated by a combination of slow slip
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::61e09f0612f66709a2fd37ba0fe907e1
https://doi.org/10.5194/egusphere-egu2020-20603
https://doi.org/10.5194/egusphere-egu2020-20603