Basin Research
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Foreland basin systemsA foreland basin system is defined as: (a) an elongate region of potential sediment accommodation that forms on continental crust between a contractional orogenic belt and the adjacent craton, mainly in response to geodynamic processes related to subduction and the resulting peripheral or retroarc fold‐thrust belt; (b) it consists of four discrete depozones, referred to as the ... hiện toàn bộ
Basin Research - Tập 8 Số 2 - Trang 105-123 - 1996
Vertical versus horizontal motions in the Alpine orogenic wedge: stratigraphic response in the foreland basinAbstract The long‐term (50 Myr) development of orogenic thrust wedges and their neighbouring foreland basins are inextricably linked. Foreland basins, such as occur nonh of the Alps, flanking the Pyrenees, east of the Apennines and south of the Himalayas, are characterized by an early underfilled (deep‐water) phase, followed by a filled (shallow‐marine) or overfille... ... hiện toàn bộ
Basin Research - Tập 4 Số 3-4 - Trang 215-232 - 1992
Macrogeomorphic evolution of the post‐Triassic Appalachian mountains determined by deconvolution of the offshore basin sedimentary recordA perplexing macrogeomorphic problem is the persistence of topography in mountain ranges that were initially formed by orogenic events hundreds of millions of years old. In this paper, we deconvolve the post‐Triassic macrogeomorphic history of a portion of one of these ranges, the central and northern Appalachians, using a well‐documented offshore isopach sedimentary record of the US Atlan... ... hiện toàn bộ
Basin Research - Tập 8 Số 3 - Trang 255-278 - 1996
Sedimentary and structural record of the Albian growth of the Bakio salt diapir (the Basque Country, northern Spain)Abstract However salt has a viscous rheology, overburden rocks adjacent to salt diapirs have a brittle rheology. Evidence of deformation within the overburden has been described from diapirs worldwide. Gravity‐driven deposits are also present along the flanks of several diapirs. The well‐known example from the L... hiện toàn bộ
Basin Research - Tập 26 Số 6 - Trang 746-766 - 2014
Tectonostratigraphic units and stratigraphic sequences of the nonmarine Songliao basin, northeast ChinaABSTRACT Through tectonostratigraphic analysis of the nonmarine, intracontinental Songliao basin in northeast China, four episodes of deformation are recognized: mantle upwelling, rift, postrift thermal subsidence and structural inversion. The episodes are related to regional geodynamics and plate motions. Each episode is associated with a specific stratigraphic sig... ... hiện toàn bộ
Basin Research - Tập 22 Số 1 - Trang 79-95 - 2010
New constraints on the Messinian sealevel drawdown from 3D seismic data of the Ebro Margin, western Mediterranean
Basin Research - Tập 23 Số 2 - Trang 123-145 - 2011
Stratigraphic record and palaeogeographical context of the Neogene basins in the Betic Cordillera, SpainAbstract The Betic Cordillera (Southern Spain) acquired its present configuration during the Neogene. The formation, evolution and total or partial destruction of Neogene sedimentary basins were highly controlled by the geodynamic situations and the positions of the basins in the Betic Cordillera. It is impossible to reconstruct the geometry of basin... ... hiện toàn bộ
Basin Research - Tập 4 Số 1 - Trang 21-36 - 1992
The synthetic seismic expression of the Messinian salinity crisis from onshore records: Implications for shallow‐ to deep‐water correlationsAbstract The onshore–offshore correlation of sedimentary successions is a common problem in basin analysis, but it becomes critical for the full understanding of the Messinian salinity crisis (MSC), a complex array of palaeoenvironmental events which affected the Mediterranean basin at the end of the Miocene. The outcrop records show that the Messinian stratigraphic... ... hiện toàn bộ
Basin Research - Tập 31 Số 6 - Trang 1121-1152 - 2019
A two‐step process for the reflooding of theM editerranean after theM essinianS alinityC risisAbstract TheM essinianS alinityC risis is well known to have resulted from a significant drop of theM editerranean sea level... ... hiện toàn bộ
Basin Research - Tập 24 Số 2 - Trang 125-153 - 2012
Role of fault interactions in controlling synrift sediment dispersal patterns: Miocene, Abu Alaqa Group, Suez Rift, Sinai, EgyptAlthough fault growth is an important control on drainage development in modern rifts, such links are difficult to establish in ancient basins. To understand how the growth and interaction of normal fault segments controls stratigraphic patterns, we investigate the response of a coarse‐grained delta system to evolution of a fault array in a Miocene half‐graben basin, Suez rift. The early M... ... hiện toàn bộ
Basin Research - Tập 11 Số 2 - Trang 167-189 - 1999
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