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- W2890623186 abstract "Based on approximately 11,000 km of seismic reflection data collected across the South China Sea oceanic basin, we describe the sedimentary filling characteristics of the basin since its Oligocene opening, as well as connections between this history and contemporaneous regional tectonic events. The seismic lines are spaced ~50 km apart, and the data are tied to International Ocean Discovery Program (IODP) Expedition 349 drilling data. Basin filling occurred in three phases, with basin-wide mean sedimentation rates increasing through time. During the Oligocene to middle Miocene, sediments accumulated primarily in the northern East and Northwest Sub-basins, with a mean basin-wide sedimentation rate of 8 m/m.y. The presence of these deposits over deep basement floor indicates that seafloor spreading initiated in these northern regions. During the late Miocene, deposition occurred primarily in the Northwest Sub-basin and partly in the southern East Sub-basin, with a mean basin-wide sedimentation rate of 30 m/m.y. Basin filling during this time seems to have been linked to slip reversal of the Red River Fault and collision of the North Palawan Block with the Luzon Arc. During the Pliocene and Pleistocene, sediments accumulated rapidly in the northeastern and southern East Sub-basin and the Southwest Sub-basin. The mean basin-wide sedimentation rate was 70 m/m.y. Basin filling during this phase seems to have been associated with the Taiwan and North Palawan collisions, SCS subduction along the Manila Trench, and Tibetan Plateau uplift. Gravity flow deposits predominate throughout the basin fill." @default.
- W2890623186 created "2018-09-27" @default.
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- W2890623186 date "2018-09-20" @default.
- W2890623186 modified "2023-10-16" @default.
- W2890623186 title "Sedimentary filling characteristics of the South China Sea oceanic basin, with links to tectonic activity during and after seafloor spreading" @default.
- W2890623186 cites W1220849975 @default.
- W2890623186 cites W1503982874 @default.
- W2890623186 cites W1572902931 @default.
- W2890623186 cites W1584140374 @default.
- W2890623186 cites W1626503910 @default.
- W2890623186 cites W1703584781 @default.
- W2890623186 cites W1848101001 @default.
- W2890623186 cites W1924599695 @default.
- W2890623186 cites W1964701098 @default.
- W2890623186 cites W1970179993 @default.
- W2890623186 cites W1972607454 @default.
- W2890623186 cites W1978088230 @default.
- W2890623186 cites W1979580006 @default.
- W2890623186 cites W1980536885 @default.
- W2890623186 cites W1984516506 @default.
- W2890623186 cites W1993302034 @default.
- W2890623186 cites W1997969348 @default.
- W2890623186 cites W2002775898 @default.
- W2890623186 cites W2016063989 @default.
- W2890623186 cites W2016353602 @default.
- W2890623186 cites W2019907607 @default.
- W2890623186 cites W2022061231 @default.
- W2890623186 cites W2022909854 @default.
- W2890623186 cites W2028692588 @default.
- W2890623186 cites W2041774199 @default.
- W2890623186 cites W2042634809 @default.
- W2890623186 cites W2044174965 @default.
- W2890623186 cites W2045878430 @default.
- W2890623186 cites W2046056394 @default.
- W2890623186 cites W2053421938 @default.
- W2890623186 cites W2053526094 @default.
- W2890623186 cites W2054661457 @default.
- W2890623186 cites W2060200559 @default.
- W2890623186 cites W2066181729 @default.
- W2890623186 cites W2068365898 @default.
- W2890623186 cites W2079173265 @default.
- W2890623186 cites W2082478724 @default.
- W2890623186 cites W2083269442 @default.
- W2890623186 cites W2085627371 @default.
- W2890623186 cites W2087228625 @default.
- W2890623186 cites W2087665583 @default.
- W2890623186 cites W2089684878 @default.
- W2890623186 cites W2091031232 @default.
- W2890623186 cites W2093744811 @default.
- W2890623186 cites W2094318628 @default.
- W2890623186 cites W2098479229 @default.
- W2890623186 cites W2109562069 @default.
- W2890623186 cites W2126392070 @default.
- W2890623186 cites W2141028564 @default.
- W2890623186 cites W2142464185 @default.
- W2890623186 cites W2142958225 @default.
- W2890623186 cites W2144432096 @default.
- W2890623186 cites W2153222505 @default.
- W2890623186 cites W2153590446 @default.
- W2890623186 cites W2156794045 @default.
- W2890623186 cites W2163270853 @default.
- W2890623186 cites W2170993908 @default.
- W2890623186 cites W2242144373 @default.
- W2890623186 cites W2254037092 @default.
- W2890623186 cites W2259996563 @default.
- W2890623186 cites W2309593205 @default.
- W2890623186 cites W2314947924 @default.
- W2890623186 cites W2340543405 @default.
- W2890623186 cites W2401955519 @default.
- W2890623186 cites W2412014301 @default.
- W2890623186 cites W2503851567 @default.
- W2890623186 cites W2551125798 @default.
- W2890623186 cites W2582000454 @default.
- W2890623186 cites W2755173514 @default.
- W2890623186 cites W2791699993 @default.
- W2890623186 cites W2800100284 @default.
- W2890623186 cites W2807886691 @default.
- W2890623186 cites W3182875964 @default.
- W2890623186 cites W384515273 @default.
- W2890623186 cites W4246753566 @default.
- W2890623186 cites W4248518744 @default.
- W2890623186 cites W4254498379 @default.
- W2890623186 cites W624697050 @default.
- W2890623186 doi "https://doi.org/10.1080/00206814.2018.1522603" @default.
- W2890623186 hasPublicationYear "2018" @default.
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