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• W2089075626 abstract "We present a 3D S-velocity model for the crust and upper mantle of the South China Sea and the surrounding regions, constrained from the analysis of over 12,000 of fundamental Rayleigh wave dispersion curves between 10 s and 150 s periods. The lateral resolution was found to vary from 2° to 4° with the increasing period over the study region. A robust scheme of Debayle and Sambridge allowed us to conduct the tomographic inversion efficiently for massive datasets. Group velocity maps varying with period show lateral heterogeneities, well related to the geological and tectonic features in the study region. The 3D S-velocity model was constructed from the 1D structure inversion of the tomographic group velocity dispersion curves at each node. The obtained average crustal structure is similar to the PREM model, while the average mantle velocity is typically lower than the global average. The complicated 3D structures reveal three prominent features correlated with geological divisions: sea basin regions, island and arc regions, and continental regions. The derived crustal and lithospheric thicknesses range from ∼15 to >50 km and from ∼60 to >140 km, respectively, with the thinnest in the South China Sea, the thickest in eastern Tibet and the Yangtze Block, and the medium in the South China Fold Belt, Indochina, and island arc regions. Our results further confirm that (1) a Mesozoic subduction zone, which is interpreted as the tectonic weak zone during the Paleogene, exists along the South China margin; (2) the influence of the Indochina extrusion along the Red River Fault is limited for the South China Sea region; (3) there is a slab remnant of the proto-South China Sea beneath Borneo. New findings suggest that the Mesozoic subduction zone should be built into any evolution model for the region, as well as the other two major tectonic boundaries of the Red River Fault and proto-South China Sea subduction zone." @default.
• W2089075626 created "2016-06-24" @default.
• W2089075626 creator A5045710703 @default.
• W2089075626 creator A5079759736 @default.
• W2089075626 date "2013-01-01" @default.
• W2089075626 modified "2023-10-11" @default.
• W2089075626 title "Crust and upper mantle structure and its tectonic implications in the South China Sea and adjacent regions" @default.
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• W2089075626 cites W1852502153 @default.
• W2089075626 cites W1899228812 @default.
• W2089075626 cites W1937531169 @default.
• W2089075626 cites W1965325889 @default.
• W2089075626 cites W1965835635 @default.
• W2089075626 cites W1971194925 @default.
• W2089075626 cites W1971218588 @default.
• W2089075626 cites W1971655295 @default.
• W2089075626 cites W1975914737 @default.
• W2089075626 cites W1984153792 @default.
• W2089075626 cites W1988822857 @default.
• W2089075626 cites W1989437964 @default.
• W2089075626 cites W1992680913 @default.
• W2089075626 cites W1995360942 @default.
• W2089075626 cites W2000232679 @default.
• W2089075626 cites W2000823413 @default.
• W2089075626 cites W2001386622 @default.
• W2089075626 cites W2003954276 @default.
• W2089075626 cites W2006737413 @default.
• W2089075626 cites W2008485243 @default.
• W2089075626 cites W2018314772 @default.
• W2089075626 cites W2019666583 @default.
• W2089075626 cites W2021029412 @default.
• W2089075626 cites W2022909854 @default.
• W2089075626 cites W2023150618 @default.
• W2089075626 cites W2025963416 @default.
• W2089075626 cites W2026562834 @default.
• W2089075626 cites W2032331952 @default.
• W2089075626 cites W2039267937 @default.
• W2089075626 cites W2043006619 @default.
• W2089075626 cites W2048635331 @default.
• W2089075626 cites W2048947717 @default.
• W2089075626 cites W2052584682 @default.
• W2089075626 cites W2054622555 @default.
• W2089075626 cites W2062221814 @default.
• W2089075626 cites W2067277226 @default.
• W2089075626 cites W2068365898 @default.
• W2089075626 cites W2072477581 @default.
• W2089075626 cites W2073437977 @default.
• W2089075626 cites W2074344814 @default.
• W2089075626 cites W2076954827 @default.
• W2089075626 cites W2081839958 @default.
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• W2089075626 cites W2083938344 @default.
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• W2089075626 cites W2090109495 @default.
• W2089075626 cites W2090171423 @default.
• W2089075626 cites W2091031232 @default.
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• W2089075626 cites W2101375010 @default.
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• W2089075626 cites W2119988086 @default.
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• W2089075626 cites W2128135732 @default.
• W2089075626 cites W2130734468 @default.
• W2089075626 cites W2131859675 @default.
• W2089075626 cites W2140270012 @default.
• W2089075626 cites W2148896769 @default.
• W2089075626 cites W2151463906 @default.
• W2089075626 cites W2153466932 @default.
• W2089075626 cites W2159344001 @default.
• W2089075626 cites W2163586810 @default.
• W2089075626 cites W2165198572 @default.
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• W2089075626 cites W4211215836 @default.
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• W2089075626 doi "https://doi.org/10.1016/j.jseaes.2012.10.037" @default.
• W2089075626 hasPublicationYear "2013" @default.
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