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作 者:ZHANG Sheng FANG Shi SHAO Hongjun WANG Silin ZHAO Yun PING Shuaifei
机构地区:[1]College of Earth Sciences,Jilin University,Changchun 130061,China [2]Key Laboratory of Marine Reservoir Evolution and Hydrocarbon Enrichment Mechanisms,Ministry of Education,Beijing 100083,China [3]Key Laboratory for Evolution of Past Life and Environments in Northeast Asia(Jilin University),Ministry of Education,Changchun 130061,China [4]Key Laboratory of Mineral Resources Evaluation of Northeast Asia,Ministry of Natural Resources,Changchun 130061,China [5]Key Laboratory for Oil Shale and Coexisting Minerals,Jilin University,Changchun 130061,China [6]China Coal Energy Heilongjiang Coal Chemical Co..Ltd.Harbin 154854,China [7]College of Earth Research,Jilin University,Changchun 30026,China
出 处:《Acta Geologica Sinica(English Edition)》2020年第2期568-571,共4页地质学报(英文版)
基 金:the National Natural Science Foundation(grant no.41472173);the Ministry of Land and Resources Outstanding Youth Science and Technology Talent Training Program of China(grant no.201311111);the National Oil Shale Geological Survey and Evaluation Program(grant no.dkyd201908-02).
摘 要:Many studies have focused on the Cretaceous evolution of NE China,including the 973 Scientific Exploration Well Work program,which completed two drill holes in this area.The Cretaceous Basin Group of eastern NE China is highly altered,so the evolution,controlling factors and interpretation of the Early Cretaceous Dasanjiang Basin are controversial,and fundamental aspects of the rocks are poorly understood.The Boli Basin is the largest Cretaceous basin within NE China,but the temporal and spatial extent of Mesozoic strata within this basin,especially the Dongshan Formation,arc not well-known.
关 键 词:CRETACEOUS BASIN BASIN
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