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《长春地质学院学报》 1996-01
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ANATEXIS ORIGIN AND TECTONIC ENVIRONMENT OF EARLY PROTEROZOIC K-FELDSPAR GRANITIC ROCKS IN DAQINGSHAN AREA

Cao Lin;Qu Yixiu(Changchun Univ.of Earth Seience,Changchun 130026)(Qinhuangdao College of Northeast Uni.)  
The K-feldspar granitic rocks in Daqingsban area are closely coexisted with the early proterozoic reworhed rock series. The geological,petrological and geochemical tharacteristics indicate that the K-feldspar granitic magma was generateel by the metamorphic anatexis of continental materials during the early proterozoic continent-continent collision-compression-thrusting,During crystallization,biotite adamellites syenogranites-alkali-feldspor granites were formed from early to late.The sovthward compression-thrusting made the K-feldspar granites outcrop in the direction E-W at the present time.
【Fund】: 国家自然科学基金
【CateGory Index】: P588.121
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