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- W2373657472 abstract "According to the buried depth of Moho discontinuity,velocity structure of upper mantle and the computed results of tectonic subsidence and thermal evolution,the crust mantle coupling model and vertical evolution of lithosphere of the South China Sea region was discussed in the present paper.The lithosphere of South China Sea region consists of the crust and solid layer of mantle.The buried depth of Moho discontinuity gradually deepens from the South China Sea Basin,slope and shelf to the continent and is 9 13 km in the basin with the typical oceanic crust,15 28 km in the margin (30 32 km locally)and 28 30 km in the southeast China coast area with the deepest to be more than 36 km.The seismic S wave velocity structure of upper mantle in the South China Sea region is characteristic of the regional blocking and vertical layering.The depth change of the bottom of lithosphere is positively correlated with that of the velocity of mantle.The buried depth of Moho discontinuity generally shows the mirror relation to the topography.The thickness of mantle lithosphere presents the complementarity with that of the crust.The bottoms of Moho and lithosphere are of flyover structure and form the crust mantle coupling model with the thick crust,thin mantle in the continent and thin crust,thick mantle in the ocean.The lithospheric evolution of South China Sea region since the end of Cretaceous was mianly a process of marginal rifting,seafloor spreading and regional subsidence.The present crust mantle coupling model clearly resulted from the vertical lithospheric evolution.Three stages were mostly recognized from the evolution history:(1)the marginal rifting from the end of Cretaceous to middle Eocene;(2)the seafloor spreading during the late of middle Eocene and the early of Miocene;and (3)regional subsidence since the late of Miocene." @default.
- W2373657472 created "2016-06-24" @default.
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- W2373657472 date "1999-01-01" @default.
- W2373657472 modified "2023-09-24" @default.
- W2373657472 title "CRUST MANTLE COUPLING MODEL AND VERTICAL EVOLUTION OF LITHOSPHERE OF SOUTH CHINA SEA REGION" @default.
- W2373657472 hasPublicationYear "1999" @default.
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