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Discussion on the Transform of Paleotethys into the Pacific
作者姓名:SHAO  Ji'an
作者单位:Peking University,Beijing 100871,China
摘    要:1.IntroductionTherehavebeenalargeamountofresearchesontheN--SextendingPaleotethysinthePaleozoicandonthemodernE--WextendingPacificOceanintheCenozoic.ButfewhavetouchedonhowthePaleotethysevolvedintothemodemPacific,andthereareonlyguessesaboutthesitllationofthePaleo--Pacificbetweenthetwostages.ThispapertriestodiscussthedynamicmechanismofthePaleo--PacificplateandthecharacteristicsoftheactivitiesofEastAsiacontinentalmarginintheMesozoicthroughtheterranesfromPaleotethysremainingintheEastAsiacont…


Discussion on the Transform of Paleotethys into the Pacific
SHAO Ji'an.Discussion on the Transform of Paleotethys into the Pacific[J].大陆动力学(英文版),1997(1).
Authors:SHAO Ji'an
Abstract:Through research on terranes the characteristics and evolutionary history of the consumed Paleotethys are traced. The N-S extension of the Paleo-Pacific and activities of transform faults in the Mesozoic are deduced from the present distribution of the remnant fragments of the Paleotethys along the East Asia continental margin of the intermediate-high latitudes. Upon these facts a period (Late Triassic-Early Cretaceous) of continental margin activity of transform fault type in East Asia is defined. It was an important period when the tectonic framework of East Asia changed from a N-S extension of oceanic plates into an E-W extension. The East Asia continental margin has been affected by the subduction of modern Pacific plate since the Late Cretaceous.
Keywords:terrane  transform continental margin  Paleotethys  Paleo-Pacific  This work is supported by the Natural Science Foundation of China
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