Zobrazeno 1 - 10
of 25
pro vyhledávání: '"Russell K. Davies"'
Publikováno v:
Geological Society, London, Special Publications. 496:223-252
SUMMARY The Holstein Field in the Gulf of Mexico consists of Pliocene, poorly lithified turbidite sands deposited in a ponded basin above an allochtonous salt tongue. Dense arrays of cataclastic deformation bands have been observed in core from wells
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cc6ec12d6c89416379f3d5c5257c83ea
https://doi.org/10.1144/sp496-2018-139
https://doi.org/10.1144/sp496-2018-139
Autor:
Christine Souque, John C. Lorenz, Philip Jones, Rob J. Knipe, Michael J. Welch, Russell K. Davies
Publikováno v:
Journal of Structural Geology. 122:11-26
Fracture corridors, elongated zones of narrowly spaced, highly connected, fractures, can generate the main fluid flow pathways in natural reservoirs and can be responsible for an early water break-through in hydrocarbon reservoirs. Understanding this
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d51b2775da33414dfa618c60a7f287cd
https://doi.org/10.1016/j.jsg.2018.12.004
https://doi.org/10.1016/j.jsg.2018.12.004
Publikováno v:
Marine and Petroleum Geology. 135:105411
Well and seismic data are used to constrain the geometry of traps formed in folds adjacent to salt walls/welds in two deep water subsalt oil fields (Fields A and B) in the northern Gulf of Mexico, USA. The fields are combined structural-stratigraphic
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0dedda3a94e7927958f8d31e0307ad9e
https://doi.org/10.1016/j.marpetgeo.2021.105411
https://doi.org/10.1016/j.marpetgeo.2021.105411
Publikováno v:
Geological Society, London, Special Publications. 459:79-100
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3314f80443e194362d507223871d18f3
https://doi.org/10.1144/sp459.5
https://doi.org/10.1144/sp459.5
Autor:
Russell K. Davies, B. Lindsey, J. Syrek, H. Adiguna, Van S. Mount, I. Matthews, Scott J. Wilkins, T. Butaud, C. Fenn
Publikováno v:
Fifth International Conference on Fault and Top Seals.
Summary We use core and image logs to characterize sub-seismic deformation at two adjacent sub-salt hydrocarbon fields, both of which are 3-way structural traps against salt. Microstructural analysis indicates that most of the deformation bands (DBs)
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::38c9b1a8de8ed026f612433df7ca980a
https://doi.org/10.3997/2214-4609.201902288
https://doi.org/10.3997/2214-4609.201902288
Publikováno v:
Fifth International Conference on Fault and Top Seals.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5cf1023d4d1446033f589f6c3b0cfaaa
https://doi.org/10.3997/2214-4609.201902281
https://doi.org/10.3997/2214-4609.201902281
Publikováno v:
Fifth International Conference on Fault and Top Seals.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e4f1e54fb8b57c7adc0093e62061a9d2
https://doi.org/10.3997/2214-4609.201902282
https://doi.org/10.3997/2214-4609.201902282
Publikováno v:
Geological Society, London, Special Publications. 406:281-309
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fcfed6a904a0cc7035ffed0329bc25d9
https://doi.org/10.1144/sp406.5
https://doi.org/10.1144/sp406.5
Publikováno v:
Tectonophysics. 474:473-492
When a mechanically layered section of rock is subject to a horizontal strain, faults often nucleate preferentially in one or more layers before propagating through the rest of the section. The result is a high density of small, low-throw faults with
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::76079c634f03d6bc44b52d38925c59b9
https://doi.org/10.1016/j.tecto.2009.04.025
https://doi.org/10.1016/j.tecto.2009.04.025
Publikováno v:
Tectonophysics. 471:186-202
A new kinematic model, based on the Trishear model, has been developed to simulate shearing and folding of a ductile interval sandwiched between two brittle layers, as faults propagate from the brittle layers into the ductile interval. This Quadshear
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d2d8dd6c6c6d9ab386bd3d5ceae74d52
https://doi.org/10.1016/j.tecto.2009.02.008
https://doi.org/10.1016/j.tecto.2009.02.008