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《Progress In Precambrian Research》 2000-04
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Khondalite event and Archean crust structure evolvement

YANG Zhen sheng, XU Zhong yuan, LIU Zheng hong (Earth science college of Jilin university, chang chun, 130016)  
Khondalite is a metasediment stratum unit which frequently occurred in Archean high-grade region. The khondalite character with aluminium-rich (graphite) sillimenite garnet-mica gneiss. Its concomitant with quartzite, calcium silicate rocks and magnesium-rich marble, assembled a suit of rock-stratum. A detailed investigation of the khondalite structure and stratum system is one of the signify achievement in Daqingshan of Inner Mongolia in resent years. Three sequence had been put forward from down to up. There are granite-mice gneiss assemblage, biotite-bering granite-mica gneiss assemblage, and marble assemblage and/or calamite gneiss assemblage. They are unconformity with granulite of Xinghe Complex in the bottom, and with slight metamorphosed Meidaizhao Complex of Peleoproterozoic in the top. According to the Sm-Nd isotopic data 2800 Ma of clinoaugite amphibolite, which intruded into khondalite, the age of khondalite should be in Mesoarchean. According to the regional stratotectonic framework of Archean, the khondalite series should be underlaying Neoachean Se'erteng Group in Daqingshan-Wulashan and Se'ertengshan areas. The investigation of the khondalite sequence and its position in the stratum system of Archean in Daqingshan region is very useful to study the high-grade region of adjacent areas. Considered to the universality distribution of the khondalite, and its egregious comparability with the high-grade region of Archean in the world, author suggested that using khondalite event represent the supercontinent craton which had been occurred in 3500-2800 Ma.
【CateGory Index】: P588.3
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