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作 者:Jianye Chen Jun Liu 陈建业;刘俊(Institute of Vertebrate Paleontology and Paleoanthropology,Chinese Academy of Sciences,China;Department of Earth Sciences,University of Hong Kong,China;College of Earth and Planetary Sciences,University of Chinese Academy of Sciences,China)
机构地区:[1]Institute of Vertebrate Paleontology and Paleoanthropology,Chinese Academy of Sciences,China [2]Department of Earth Sciences,University of Hong Kong,China [3]College of Earth and Planetary Sciences,University of Chinese Academy of Sciences,China
出 处:《National Science Review》2024年第10期166-169,共4页国家科学评论(英文版)
基 金:supported by the Strategic Priority Research Program of the Chinese Academy of Sciences(XDB26000000);the International Partnership Program of Chinese Academy of Sciences(132311KYSB20190010).
摘 要:The amalgamation of Pangea during the late Paleozoic is a major tectonic event in Earth history[1],but its process and timing is still not well understood,especially among its eastern margin.Two competing hypotheses exist on the collision time between the North China Block(NCB)and Pangea.
分 类 号:P54[天文地球—构造地质学]
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