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《Scientia Geologica Sinica》 2001-02
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GEOCHEMISTRY OF EARLY CRETACEOUS ALKALINE RHYOLITES FROM HULUN LAKE, DAXING'ANLING AND ITS TECTONIC IMPLICATIONS

Ge Wenchun 1, 2 Li Xianhua 1 Lin Qiang 2 Sun Deyou 2 Wu Fuyuan 2 Yun Sunghyo 3 (1. Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640; 2. College of Earth Sciences, Jilin University, Changchun \ 130061;  
The upper part of rhyolites within the Shangkuli Formation in the Hulun Lake region, northern Daxing'anling, is characterized by high SiO 2 (75.41%~77.32%), total alkaline\|rich (Na 2O+K 2O=7.98%~8.74%), high Ga/Al, enriched in Y, Nb, Zr, and depleted in Al, Mg, Ca, Cr, Ti. Their chemical compositions are very similar to those of A type granites, but different from highly fractionated I and S type granites. These rhyolites, geochemically similar to those of A 1 type granites subdivided by Eby(1992), are the synchronous products of A type granite in this region. Five rhyolite samples yield a Rb Sr whole rock isochron age of 127±5 Ma, coeval with the age of 125±2 Ma of Yeliekede basalts in the Daxing'anling. It is therefore suggested that the bimodal magmatism occurred in a lithospheric extensional setting during the Early Cretacoues.
【Fund】: 国家自然科学基金! ( 49972 0 2 7);; 国家杰出青年科学基金! ( 4972 530 9)资助项目
【CateGory Index】: P588.1;P59
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