Abstract：The Paleo-Asia Tectonic Domain between the Sino-Korea, Tarim and Siberia old landmasses presented not only in Pre-Mesozoic, but also in Mesozoic-Cenozoic period. The Paleo-Asia Tectonic Domain does not equal to the PaleoAsian Ocean and corresponding tectonic domain. Being a part of the Paleo-Aisa Tectonic Domain, the Paleo-Asian Ocean appeared in Late Cambrian-Ordovician, and ended in Middle Triassic. The Paleo-Pacific Ocean and its tectonic domain formed in Late Paleozoic, and transformed into the Marginal Pacific Tectonic Domain in Post-Indosinian epoch. It coexisted with the Paleo-Asia Tectonic Domain, to form the intraplate orogenic belt, partial basin-and-mountain structure and northeastern highlands in the two tectonic domains during the Late Triassic-Jurassic epoch. The NNE-striking basinand-mountain system, dominated by the Marginal Pacific Tectonic Domain, finally formed in Early Cretaceous.
王五力, 郭胜哲. 中国东北古亚洲与古太平洋构造域演化与转换[J]. 地质与资源, 2012, 21(1): 27-34.
WANG Wu-li, GUO Sheng-zhe. THE EVOLUTION AND TRANSFORMATION OF PALEO-ASIA AND PALEO-PACIFIC TECTONIC DOMAIN OF NORTHEAST CHINA. GEOLOGY AND RESOURCES, 2012, 21(1): 27-34.
2012, Vol. 21 
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