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- W2351289153 abstract "Recent investigation on paleoclimatic marks indicates that the evolution of thePermo--Triassic paleoclimates may be attributed to the onset, deve1opment and break-down of a megamonsoonal process. However, zonal distribution resumed in Late Trias-sic, which would be of paleogeographic implications. Late Triassic ooilitic limestone,which should be formed in a relatively arid condition, was reported from the Coron Is-land of the North Palawan Block. Thus paleoclimatically, the Late Triassic sequence inNorth Palawan can not be correlated with the equivalents in the South China and In-dochina blocks, but with that in the northern margin of the Indian block and that in theRyukyu Islands. The ooi1itic 1imestones from the North Palawan, India and Ryukyublocks represented the southern subtropical zone in the Late Triassic. This indicatesthat the position of the North Palawan Block in Late Triassic was far to south of the In-dochina and South China. There might be a Tethyan ocean in between. Understandingof the Mesozoic history of the South China Sea will undoubtedly shed light on deciphe-ring relevant Tethyan trace recorded in the South China Sea and its adjacent regions." @default.
- W2351289153 created "2016-06-24" @default.
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- W2351289153 date "2002-01-01" @default.
- W2351289153 modified "2023-09-25" @default.
- W2351289153 title "REVIEWS ON TETHYAN TRACE IN SOUTH CHINA SEAAND SOME ADJACENT REGIONS" @default.
- W2351289153 hasPublicationYear "2002" @default.
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