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Tectono-sedimentary evolution of active extensional basins

Basin Research, 2000
We present conceptual models for the tectono‐sedimentary evolution of rift basins. Basin architecture depends upon a complex interaction between the three‐dimensional evolution of basin linkage through fault propagation, the evolution of drainage and drainage catchments and the effects of changes in climate and sea/lake level.
Gawthorpe, R. L., Leeder, M. R.
openaire   +2 more sources

Rift-related sedimentary evolution and its response to tectonics and climate changes: A case study of the Guaizihu sag, Yingen-Ejinaqi Basin, China

, 2020
Distinguished from most existing rift basin evolutionary models, the succession of deep-water deposits in the Guaizihu sag were mainly developed during rift initiation instead of the greatest tectonic subsidence phase.
Yunchao Hou   +6 more
semanticscholar   +1 more source

Similar Oligo-Miocene tectono-sedimentary evolution of the Paratethyan branches represented by the Moldavidian Basin and Maghrebian Flysch Basin

, 2020
A comparison of the stratigraphic record between two different branches of the Tethys is attempted for the first time. This study concerns the main Oligocene-Miocene tectono-sedimentary events in the Cenozoic units of the Moldavidian Basin (Romanian ...
M. Martín-Martín   +3 more
semanticscholar   +1 more source

Tectono-sedimentary evolution of the Late Ediacaran to early Cambrian trough in central Sichuan Basin, China: New insights from 3D stratigraphic forward modelling

Precambrian Research, 2020
Several conceptual models have been proposed on the tectono-sedimentary evolution of the Late Sinian to early Cambrian “aulacogen” in the central Sichuan Basin, China.
Jianliang Liu   +3 more
semanticscholar   +1 more source

Reviews of the Mesoproterozoic to Neoproterozoic sedimentary sequences and new constraints on the tectono-sedimentary evolution of the southern margin of the North China Craton

Journal of Asian Earth Sciences, 2019
The North China Craton (NCC) is thought to experience multi-stage extensional events after the breakup of the Columbia (Nuna) Supercontinent, and even during the assembly of the Rodinia Supercontinent.
Pengfei Zuo   +7 more
semanticscholar   +1 more source

Musings over sedimentary basin evolution

Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1982
Field geologists and explorationists are of necessity immersed in numerous very detailed surface and subsurface observations. They are often perplexed by the choice of relatively simple geophysical models that so elegantly explain the origin and evolution of sedimentary basins.
openaire   +1 more source

Middle Jurassic–Early Cretaceous tectono-sedimentary evolution of the southwestern Iberian Basin (central Spain): Major palaeogeographical changes in the geotectonic framework of the Western Tethys

, 2019
The Middle Jurassic-Early Cretaceous tectono-sedimentary evolution of the southwestern part of the intraplate Iberian Basin (Spain) was mostly controlled by the Alto Tajo-Montes Universales (ATMU) and Landete-Teruel (LT) faults.
M. Aurell   +6 more
semanticscholar   +1 more source

Kimmeridgian–Berriasian stratigraphy and sedimentary evolution of the central Iberian Rift System (NE Spain)

Cretaceous research (Print), 2019
Sequence-stratigraphic, biostratigraphic and strontium-isotopic data have made it possible to update what is known of the stratigraphy and sedimentary evolution of the Kimmeridgian–Berriasian synrift successions recorded in four subbasins (Aguilon ...
M. Aurell   +12 more
semanticscholar   +1 more source

Early Cretaceous sedimentary evolution of the northern Lhasa terrane and the timing of initial Lhasa-Qiangtang collision

Gondwana Research, 2019
Lower Cretaceous strata in the Baingoin basin of the northern Lhasa terrane record initial collision between the Lhasa and Qiangtang blocks, followed by the early uplift of central Tibet.
Wen Lai   +5 more
semanticscholar   +1 more source

Evolution of Sedimentary Basins: ABSTRACT

AAPG Bulletin, 1983
Simple extensional models that involve stretching by listric faulting in the brittle upper crust and plastic flow in the lower lithosphere have been shown to account for the subsidence history of various sedimentary basins, continental shelves, and the Central graben in the North Sea.
openaire   +1 more source

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