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《长春地质学院学报》 1992-02
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THE ESTABLISHMENT OF PRECA MBRIAN STRATA AND NEW RECOGNITION OF THE GEOTECTONIC EVOLUTION IN HAINAN ISLAND

Hou Wei Chen Huifang Liang Xinquan Wang Kefu(Changsha Institute of Geote ctonics, Academia Sinica)  
In this paper according to the systematic studies of Sm-Nd isochronic lines, the absol ute ages of plagioclase-hornblend and mi gmatic granitic gneiss of the Baoban Group are 1. 7 Ga and 1. 4 Ga respectively , and the absolute age of mianthite occurring in the migmatitic granite is 2. 9 Ga. These ages illustrate that these rocks were formed 1. 4 and 2. 9 Ga ago. Thirdly,the single-stage Pb-model isotopic ages of feldspar selected from the plagioclase-hornblend schist and migmatic granitic gneiss of the Baoban Group are 1.1 to 1. 2 Ga and 940 Ma respectively. Based on the results of the Rb-Sr whole -rock isochronic line, the metamorphic ages of the plagioclase hornblend schist in the Baoban Group and mica schist in the Baoban Group and the Shilu Group are 1. 34 Ga and 1. 22 Ga respectivly.Among the Precambrian strata in Hainan Island, the Bao.ban Group having the characteristics of granite-greenstone and containing basaltic komatiite makes up the Precambrian cristalline basement or the pre-geosynclinal structural layer, and the Shilu Group consisting of turbidite, felsic volcanis and sedimentary rocks and a Fe-bearing formation is a structural sublayer formed during the early stage of geosynclinal development.The evidence and characteristics ogeotectonisc evoluting of Hainan Island has undergone four stages, that is , pre-geosynclinal, geosynclinal, platform, diwa.
【CateGory Index】: P534.1;;P548
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