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- W2353167639 abstract "Study results from paleomagnetics of seven seamounts in the southwestern basin of the South China Sea indicate that since middle Miocene they have moved southward for 4 degrees of latitude, at the average rate of about 2.4 cm/a. The southwestern basin at first turned clockwise andthen anticlockwise. Such a movement pattern shows that the South China margin had been rifted and opened southeastward due to collision between the Indian plate and the Eurasian plate, meanwhile it has been affected by the eastern tectonic movement. The southwestern basin of the South China Sea has gradually evolved from the continental crust to the oceanic crust after the continental margin was rifted." @default.
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- W2353167639 date "2002-01-01" @default.
- W2353167639 modified "2023-09-25" @default.
- W2353167639 title "A Study on Paleomagnectics of Seamounts in the Southwestern Basin of the South China Sea" @default.
- W2353167639 hasPublicationYear "2002" @default.
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