地质与资源2012，Vol.21Issue(1)：27-34,8.
中国东北古亚洲与古太平洋构造域演化与转换
THE EVOLUTION AND TRANSFORMATION OF PALEO-ASIA AND PALEO-PACIFIC TECTONIC DOMAIN OF NORTHEAST CHINA
摘要
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 Paleo-Asian 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 basin-and-mountain system, dominated by the Marginal Pacific Tectonic Domain, finally formed in Early Cretaceous.关键词
古亚洲构造域/古亚洲洋/古太平洋及其构造域/滨太平洋构造域/演化与转换Key words
Paleo-Asia Tectonic Domain/ Paleo-Asian Ocean/ Paleo-Pacific Ocean and its tectonic domain/ Marginal Pacific Tectonic Domain/ evolution and transformation分类
天文与地球科学引用本文复制引用
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):27-34,8.基金项目
中国地质调查局项目“古亚洲洋构造体制与滨太平洋构造体制叠加转变综合调查和研究”(基[2010]矿评01-19-01)资助. （基[2010]矿评01-19-01）
