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作 者:Zhuolong Yang Pujun Wang Yulong Huang Youfeng Gao Chongyang Chen 杨卓龙;王璞珺;黄玉龙;高有峰;陈崇阳
机构地区:[1]College of Earth Sciences,Jilin University,Changchun 130061,China [2]Research Center of Palaeontology and Stratigraphy,jilin University,Changchun 130026,China [3]College of Geographic Sciences and Tourism,jilin Normal University,Siping 136000,China
出 处:《Science Bulletin》2024年第16期2471-2473,共3页科学通报(英文版)
基 金:supported by the National Natural Science Foundation of China(42102129 and 41790453).
摘 要:During the late Paleozoic to early Mesozoic,a tectonic transition occurred in Northeast China,marking a shift from the Paleo-Asian Ocean to the Mongolian Okhotsk and Paleo-Pacific tectonic domains[1].As a result of regional compression induced by oceanic closure and continental collision,stratigraphic records from this period are scarce,but such records are essential for elucidating the tectonic and paleographic evolution of the region during the transition.
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