Zobrazeno 1 - 10
of 74
pro vyhledávání: '"Rebecca E. Bell"'
Autor:
Thomas A. J. Merry, Ian D. Bastow, Rita Kounoudis, Christopher S. Ogden, Rebecca E. Bell, Laurence Jones
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 22, Iss 9, Pp n/a-n/a (2021)
Abstract The eastern Mediterranean hosts, within the span of a few hundred kilometers, extensional, strike‐slip, and collision tectonics above a set of fragmenting subducting slabs. Slab roll‐back, toroidal flow, and lithospheric dripping/delamin
Externí odkaz:
https://doaj.org/article/92ebd5ebc12b4ffba8a3f91a0a43efe6
Autor:
Thilo Wrona, Alexander C. Whittaker, Rebecca E. Bell, Robert L. Gawthorpe, Haakon Fossen, Christopher A.‐L. Jackson, Marit Stokke Bauck
Publikováno v:
Basin Research
Our understanding of continental rifting is, in large parts, derived from the stratigraphic record. This record is, however, incomplete as it does not often capture the geomorphic and erosional signal of rifting. New 3D seismic reflection data reveal
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::95eb85b0934fafcc30d399bde55f5872
https://doi.org/10.1111/bre.12732
https://doi.org/10.1111/bre.12732
Publikováno v:
Basin Research. 35:483-486
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2b0c22417b217a6c29cd6fe13ce93a01
https://doi.org/10.1111/bre.12726
https://doi.org/10.1111/bre.12726
Autor:
Jonah S. McLeod, Alexander C. Whittaker, Rebecca E. Bell, Gary J. Hampson, Stephen E. Watkins, Sam A. S. Brooke, Nahin Rezwan, Joel Hook, Jesse R. Zondervan
Water and sediment transport in rivers are not uniform through time. In perennial rivers, sediment may be in motion for much of the year. However, intermittent rivers only transport bedload material during the most significant flow events, therefore
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2945669b8fa7d1cdb04acdae7fb106c2
https://doi.org/10.5194/egusphere-egu23-5318
https://doi.org/10.5194/egusphere-egu23-5318
Publikováno v:
Basin Research. 34:618-639
Extensional growth folds form ahead of the tips of propagating normal faults. These folds can accommodate a considerable amount of extensional strain and they may control rift geometry. Fold-related surface deformation may also control the sedimentar
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a482a054f27f4e76a772cd01449a45eb
https://doi.org/10.1111/bre.12633
https://doi.org/10.1111/bre.12633
Publikováno v:
Basin Research. 34:121-140
Continental rifting is accommodated by the development of normal fault arrays. Fault growth patterns control their related seismic hazards, as well as influencing the tectonostratigraphic evolution, resource extraction and CO2 storage potential of ri
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4e5838b2a7224e34746c3842355a3f78
https://doi.org/10.1111/bre.12613
https://doi.org/10.1111/bre.12613
Polygonal, layer-bound normal faults can extend over very large areas (>2,000,000 km2) of sedimentary basins. Best developed in very fine-grained rocks, these faults are thought to form during early burial in response to a range of diagenetic process
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::faeccc30abc2d59e9c0add04e2eba31b
http://hdl.handle.net/10044/1/101887
http://hdl.handle.net/10044/1/101887
Publikováno v:
AAPG Bulletin. 105:1679-1720
Studies of near-seabed datasets show that salt tectonics controls the distribution and architecture of deep-water reservoirs in many salt-influenced basins. It is typically difficult, however, to study the distribution and stratigraphic evolution of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::04314187788038cc174219266afdd20d
https://doi.org/10.1306/11182017340
https://doi.org/10.1306/11182017340
Continental breakup involves a transition from rapid, fault-controlled syn-rift subsidence to relatively slow, post-breakup subsidence induced by lithospheric cooling. Yet the stratigraphic record of many rifted margins contain syn-breakup unconformi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5d73297d398e2354960963a7bd9465e3
Autor:
Maomao Wang, Philip M. Barnes, Julia K. Morgan, Rebecca E. Bell, Gregory F. Moore, Ming Wang, Ake Fagereng, Heather Savage, Davide Gamboa, Robert N. Harris, Stuart Henrys, Joshu Mountjoy, Anne M. Tréhu, Demian Saffer, Laura Wallace, Katerina Petronotis
Publikováno v:
Earth and Planetary Science Letters. 605:118022
Calcareous rocks are commonly found in subduction zones, but few studies have investigated the consolidation and compactive deformation of these rocks prior to subduction, and their potential effects on subduction and accretionary processes are thus
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::56f26a287d66d181c19c71d3fa6b0dc8
https://doi.org/10.1016/j.epsl.2023.118022
https://doi.org/10.1016/j.epsl.2023.118022