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- W2384977024 abstract "In the four geological structure units in northeastern part of the South China Sea, including Zhu I Depression of Zhujiangkou Basin, Dongsha Uplift, Chaoshan Depression and Taixinan Basin, developed early Cretaceous and early Jurassic marine strata. The marine strata have the seismic characteristics of large dip, middle frequency, and moderate continuity. The individual velocities calculated from stack velocities are between 4.3 and 5.0 km·s -1 . Those strata, which have structural features of downwarping type depression, are quite different from the Cenozoic strata with features of filling faulting type one. The residual Mesozoic sediment is 4 000 to 5 000m thick. The Dongsha—Penghu—Beigang Uplift Belt where Tethys died out is a suture belt between South China and South China Sea blocks, with a high magnetic anomaly and thick crust." @default.
- W2384977024 created "2016-06-24" @default.
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- W2384977024 date "2000-01-01" @default.
- W2384977024 modified "2023-09-25" @default.
- W2384977024 title "DISTRIBUTION AND GEOLOGICAL & GEOPHYSICAL CHARACTERISTICS OF MESOZOIC MARINE STRATA IN NORTHEASTERN PART OF SOUTH CHINA SEA" @default.
- W2384977024 hasPublicationYear "2000" @default.
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