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- W2898097540 abstract "Abstract The role of spatiotemporally varying tectonic forcing in the development of stratigraphic patterns along passive margins and continental rift basins has been recognized for decades, but the exact nature of the stratigraphic response is still debated. This study develops a coupled tectonic‐stratigraphic numerical model with a fixed absolute lake level and constant climate conditions to quantify the signatures of spatiotemporally varying tectonic forcing on the stratigraphic record. This model consists of a three‐dimensional rift basin with a range of geomorphic features and produces a number of well‐recognized stratigraphic patterns, which are commonly interpreted to be caused by lake‐/sea‐level or climate fluctuations. This study demonstrates that the shoreline and grain‐size front are decoupled through the adjustment of the depositional slope and sediment dispersal under spatiotemporally varying tectonic forcing, especially in underfilled basins. Under such a decoupled situation, the pathway of the migrating subsidence centre correlates with the pathway of the grain‐size front, a result of competition between spatiotemporally varying tectonic forcing and autogenic sediment transport. The model results also highlight the significance of three‐dimensional variability in the stratigraphic response to tectonic forcing, which may be overlooked or misinterpreted and suggests a high degree of uncertainty in re‐establishing the base‐level cycles from the stratigraphic record alone. Moreover, spectral analysis of the modelled stratigraphy and tectonic forcing suggests that low‐frequency tectonic signals are more likely to be recorded in the stratigraphy with a lag time, whereas high‐frequency tectonic signals are likely to be shredded, mixed with autogenic signals, or buffered through sediment‐routing systems. Finally, quantitative measurements of the stratigraphic architecture of the Nanpu sag in the Bohai Bay Basin, China are used to tune the numerical model of this study to illustrate how to evaluate the role of tectonic forcing on the development of characteristic stratigraphic sequences." @default.
- W2898097540 created "2018-11-02" @default.
- W2898097540 creator A5020856046 @default.
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- W2898097540 creator A5081054683 @default.
- W2898097540 date "2018-11-22" @default.
- W2898097540 modified "2023-09-25" @default.
- W2898097540 title "Stratigraphic response to spatiotemporally varying tectonic forcing in rifted continental basin: Insight from a coupled tectonic-stratigraphic numerical model" @default.
- W2898097540 cites W1558381798 @default.
- W2898097540 cites W1736033808 @default.
- W2898097540 cites W1774723856 @default.
- W2898097540 cites W1800719856 @default.
- W2898097540 cites W1955520095 @default.
- W2898097540 cites W1967415015 @default.
- W2898097540 cites W1968360886 @default.
- W2898097540 cites W1971245172 @default.
- W2898097540 cites W1972768340 @default.
- W2898097540 cites W1973530684 @default.
- W2898097540 cites W1976518101 @default.
- W2898097540 cites W1986966893 @default.
- W2898097540 cites W1995040253 @default.
- W2898097540 cites W1996383366 @default.
- W2898097540 cites W1996720026 @default.
- W2898097540 cites W2003554037 @default.
- W2898097540 cites W2005317113 @default.
- W2898097540 cites W2008461620 @default.
- W2898097540 cites W2015136608 @default.
- W2898097540 cites W2021158012 @default.
- W2898097540 cites W2023058606 @default.
- W2898097540 cites W2025447778 @default.
- W2898097540 cites W2025715657 @default.
- W2898097540 cites W2026303435 @default.
- W2898097540 cites W2034599543 @default.
- W2898097540 cites W2037047168 @default.
- W2898097540 cites W2043081497 @default.
- W2898097540 cites W2049143870 @default.
- W2898097540 cites W2051220980 @default.
- W2898097540 cites W2063603905 @default.
- W2898097540 cites W2065272856 @default.
- W2898097540 cites W2070671910 @default.
- W2898097540 cites W2074297072 @default.
- W2898097540 cites W2075223606 @default.
- W2898097540 cites W2078741041 @default.
- W2898097540 cites W2086486026 @default.
- W2898097540 cites W2086747528 @default.
- W2898097540 cites W2090791965 @default.
- W2898097540 cites W2092035606 @default.
- W2898097540 cites W2098362516 @default.
- W2898097540 cites W2098891607 @default.
- W2898097540 cites W2098951711 @default.
- W2898097540 cites W2101644114 @default.
- W2898097540 cites W2102264361 @default.
- W2898097540 cites W2105217815 @default.
- W2898097540 cites W2105612923 @default.
- W2898097540 cites W2106802871 @default.
- W2898097540 cites W2109855460 @default.
- W2898097540 cites W2114872918 @default.
- W2898097540 cites W2115621369 @default.
- W2898097540 cites W2115803110 @default.
- W2898097540 cites W2121595380 @default.
- W2898097540 cites W2122080497 @default.
- W2898097540 cites W2122452679 @default.
- W2898097540 cites W2123193848 @default.
- W2898097540 cites W2128560225 @default.
- W2898097540 cites W2130112574 @default.
- W2898097540 cites W2130432031 @default.
- W2898097540 cites W2132970916 @default.
- W2898097540 cites W2137903446 @default.
- W2898097540 cites W2140268962 @default.
- W2898097540 cites W2141845276 @default.
- W2898097540 cites W2154791439 @default.
- W2898097540 cites W2155745504 @default.
- W2898097540 cites W2158091870 @default.
- W2898097540 cites W2161036314 @default.
- W2898097540 cites W2168018662 @default.
- W2898097540 cites W2188755987 @default.
- W2898097540 cites W2295041602 @default.
- W2898097540 cites W2296222902 @default.
- W2898097540 cites W2298672701 @default.
- W2898097540 cites W2308483061 @default.
- W2898097540 cites W2391174902 @default.
- W2898097540 cites W2472806261 @default.
- W2898097540 cites W2494000845 @default.
- W2898097540 cites W2563506672 @default.
- W2898097540 cites W2615152542 @default.
- W2898097540 cites W2616603387 @default.
- W2898097540 cites W2742214855 @default.
- W2898097540 cites W2771305022 @default.
- W2898097540 cites W2775797458 @default.
- W2898097540 cites W2793306017 @default.
- W2898097540 cites W2802321867 @default.
- W2898097540 doi "https://doi.org/10.1111/bre.12322" @default.
- W2898097540 hasPublicationYear "2018" @default.