The position of Cathaysia in Nuna and during the Nuna-Rodinia transition  

华夏板块在努纳超大陆及努纳-罗迪尼亚转换期的位置

作　　者：Chuan Yang Zheng-Xiang Li Yang Li Xian-Hua Li 杨传;李正祥;李扬;李献华

机构地区：[1]State Key Laboratory of Palaeobiology and Stratigraphy,Nanjing Institute of Geology and Palaeontology,Chinese Academy of Sciences,Nanjing 210008,China [2]Earth Evolution and Dynamics Research Center(EDRC),Laoshan Laboratory,Qingdao 266237,China [3]Earth Dynamics Research Group(EDRG),School of Earth and Planetary Sciences,Curtin University,Perth WA 6845,Australia [4]School of Earth and Space Sciences,Peking University,Beijing 100871,China [5]State Key Laboratory of Lithospheric Evolution,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China

出　　处：《Science Bulletin》2024年第17期2693-2697,共5页科学通报（英文版）

基　　金：National Key Research and Development Program of China (2022YFF0800100);Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences (E221110015)。

摘　　要：The assembly and breakup of Nuna and Rodinia, two successive supercontinents in the Proterozoic, provide key evidence for the establishment of supercontinent cycles. Reliable palaeogeographic reconstructions at the cores of the two supercontinents are critical for understanding the evolution and geodynamics of the supercontinent cycles. In addition, there are fundamental aspects of the Nuna-Rodinia transition that remain poorly understood, including the ways in which Nuna broke up and Rodinia assembled, either through introversion [1] or extroversion [2].

关 键 词：CONTINENT RODINIA TRANSITION 

分 类 号：P542[天文地球—构造地质学]