Zobrazeno 1 - 10
of 40
pro vyhledávání: '"Frank J. Peel"'
Publikováno v:
Frontiers in Earth Science, Vol 9 (2021)
The stratal architecture of deep-water minibasins is dominantly controlled by the interplay of two factors, structure growth and sediment supply. In this paper we explore the utility of a reduced-complexity, fast computational method (Onlapse-2D) to
Externí odkaz:
https://doaj.org/article/3d72210a6d504ae98ad7583675a4869b
Publikováno v:
SSRN Electronic Journal.
Publikováno v:
Basin Research. 33:427-446
In salt-detached gravity-gliding/spreading systems the detachment geometry is a key control on the downslope mobility of the supra-salt sequence. Here we used regional 3D seismic data to examine a salt-stock canopy in the northern Gulf of Mexico slop
The conventional area-balancing method uses a single regional slope, commonly parallel to basal detachment and generally horizontal, to restore a deformed geological section to an initial rectangular shape. However, most fold-thrust belts exhibit a w
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::41f42bcfa74f4983fe8e0128f845e2da
https://eprints.soton.ac.uk/454417/
https://eprints.soton.ac.uk/454417/
Publikováno v:
Dipòsit Digital de la UB
Universidad de Barcelona
Universidad de Barcelona
The relative timing between crustal extension and salt deposition can vary spatially along passive margin salt basins as continents unzip, or as the locus of extension shifts toward the embryonic ocean spreading center. Determining the relative timin
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ac60485ea525ea2c58af7e56bc4618f8
http://hdl.handle.net/2445/184443
http://hdl.handle.net/2445/184443
Publikováno v:
Basin Research. 32:453-484
Base-salt relief influences salt flow, producing three-dimensionally complex strains and multiphase deformation within the salt and its overburden. Understanding how base-salt relief influences salt-related deformation is important to correctly inter
Publikováno v:
Digital.CSIC. Repositorio Institucional del CSIC
instname
instname
Passive-margin salt basins tend to be much more deformed than their nonsalt equivalents, but they are by no means all the same. We used seismic data to study the Salina del Bravo region, northeast Mexico, to investigate the ways in which margin confi
Autor:
Oliver B. Duffy, Christopher A.-L. Jackson, Gillian M. Apps, Frank J. Peel, Naiara Fernandez, Michael R. Hudec
Publikováno v:
Fernandez, N, Duffy, O, Peel, F, Hudec, M, Apps, G & Jackson, C 2020, ' Minibasin mobility and obstruction on salt-detached slopes: implications for canopy dynamics and sediment routing ', EGU General Assembly 2020, Vienna, Austria, 3/05/20-8/05/20 . https://doi.org/10.5194/egusphere-egu2020-11125
In salt-detached gravity-gliding/spreading systems the detachment geometry is a key control on the downslope mobility of the supra-canopy (supra-salt) sequence. As supra-canopy minibasins translate downslope, they also subside into salt. If the base
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::662e94bdb1a0108181f58f2ed3723681
https://doi.org/10.5194/egusphere-egu2020-11125
https://doi.org/10.5194/egusphere-egu2020-11125
Publikováno v:
Muniz Pichel, L, Peel, F, Jackson, C A & Huuse, M 2018, ' Geometry and kinematics of salt-detached ramp syncline basins ', Journal of Structural Geology, vol. 115, pp. 208-230 . https://doi.org/10.1016/j.jsg.2018.07.016
Ramp-syncline basins (RSBs) are characterized by asymmetric depocentres formed by translation above salt detachments with basal steps. Recognition of these minibasins allows quantification of the magnitude and rates of overburden translation above a