Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Heijn van Gent"'
Publikováno v:
Interpretation. 2:SM101-SM117
The late Permian Zechstein evaporites in the northern Netherlands were exceptionally well imaged in ![Formula][1] of prestack depth migration 3D seismic data. Seismic reflections of a 30–150-m-thick Zechstein 3 anhydrite-carbonate stringer, which w
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bba3a14819b4759b8e9570c49836e265
https://doi.org/10.1190/int-2014-0037.1
https://doi.org/10.1190/int-2014-0037.1
Publikováno v:
Tectonophysics. 512:12-21
We performed Discrete Element Method (DEM) simulations of the formation of normal faults in a brittle-cohesive material above a basement fault, focusing on the formation of open fractures and cavities in areas of low normal stress, i.e. near the surf
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::52149e811ec5f0e076c2fe79ea3f2664
https://doi.org/10.1016/j.tecto.2011.09.008
https://doi.org/10.1016/j.tecto.2011.09.008
Autor:
Loic Bazalgette, Heijn van Gent, Eilard Hindericus Hoogerduijn Strating, Marc Holland, Najwa Yassir, János Urai
Publikováno v:
Earth and Planetary Science Letters. 304:399-406
Dilatant fractures in normal fault zones are widely recognized as major pathways of fluid flow in the upper crust where the ratio of rock strength and effective stress is suitable for their formation, but the structure of these fracture networks in 3
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5e3fd8373c0d3abd65c94a9e2f4ba57a
https://doi.org/10.1016/j.epsl.2011.02.017
https://doi.org/10.1016/j.epsl.2011.02.017
Publikováno v:
Journal of Structural Geology. 33:292-311
We present a first look at the large-scale, complexly folded and faulted internal structure of Zechstein salt bodies in NW Europe using 3D reflection seismic reflection data from two surveys on the Groningen High and the Cleaver Bank High. We focus o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2508e461fce921987100ed04bbfbd1f4
https://doi.org/10.1016/j.jsg.2010.07.005
https://doi.org/10.1016/j.jsg.2010.07.005
Publikováno v:
Journal of the Geological Society 168(2), 393-406 (2011). doi:10.1144/0016-76492010-047
Classically, the North Sea Chalk is interpreted as having been deposited under quiet, homogeneous pelagic conditions with local redeposition in slumps and slides. Recent observations of highly discontinuous reflection patterns on 2D and 3D seismic re
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::016fa8fccd053e6a59d3983f36caf8e4
https://doi.org/10.1144/0016-76492010-047
https://doi.org/10.1144/0016-76492010-047
Publikováno v:
Journal of Structural Geology. 32:1375-1391
We present analogue models of the formation of dilatant normal faults and fractures in carbonate fault zones, using cohesive hemihydrate powder (CaSO 4 ·½H 2 O). The evolution of these dilatant fault zones involves a range of processes such as frag
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::354bf65f8df78d2c81afb406d86dcabd
https://doi.org/10.1016/j.jsg.2009.05.006
https://doi.org/10.1016/j.jsg.2009.05.006
Publikováno v:
Journal of Structural Geology. 32:537-553
Over the last years, field-based studies have shown that fault surfaces can exhibit a considerable self-affine topography. It is reasonable to assume that similar undulations are also present in fault interpretations from 3D reflection seismic data,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::28d9e77e93da1d0cd33fd5d208a56fef
https://doi.org/10.1016/j.jsg.2010.03.003
https://doi.org/10.1016/j.jsg.2010.03.003