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作 者:Yu-Sheng Wan Dun-Yi Liu Biao Song
机构地区:[1]Beijing SHRIMP Center, Institute of Geology, Chinese Academy of Geological Sciences
出 处:《Science Bulletin》2019年第10期641-643,共3页科学通报(英文版)
基 金:supported by the National Natural Science Foundation of China(41472169);the Key Program of the Ministry of Nature and Resources of China(121201102000150012)
摘 要:The formation, composition and evolution of the oldest continental crust is the logical starting point for discussing the differentiation and development of the crust-mantle system and the tectonic evolution of the Earth. Searching for and identifying the oldest continental crust and investigating the processes and periodicity of crust formation and its subsequent development into cratons is a primary scientific topic of worldwide research [1]. The other important issues related to early Precambrian evolution include identifying tectonic divisions and determining the onset of plate tectonics. However, the rarity of preserved ancient continental crust due to its long-term reworking makes this research extremely challenging. Thus, finding and identifying the oldest rocks and zircons is the beginning of very exciting and important research. The occurrence of >3.8 Ga rocks in northern and eastern Canada, West Greenland and eastern Antarctica are difficult to access and so it is important to identify other occurrences of such rocks.
关 键 词:The FORMATION oldest CONTINENTAL CRUST eastern ANTARCTICA
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