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《Geotectonica Et Metallogenia》 2007-03
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GEOCHEMICAL CHARACTERISTICS OF BASALTIC ANDESITES FROM DAHALAJUNSHAN FORMATION,SOUTHESTERN TEKESI (XINJIANG):PETROGENESIS AND ITS TECTONIC SIGNIFICANCE

SUN Linhua1,2, PENG Touping1 and WANG Yuejun1(1.CAS Key Laboratory of Isotope Geochronology and Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou, GD 510640, China; 2.Graduate School of the Chinese Academy of Science, Beijing 100049, China)  
The basaltic andesites from Dahalajunshan Formation in southeastern Tekesi County, Xinjiang, are of calc-alkaline composition, and show depletion in HFSEs (e.g., Nb, Ta) and enrichment in LILEs. Moreover, the ratios of strongly incompatible elements are distinct from those for the primitive, depleted and enriched mantle, indicating involvement of crustal components in the mantle source. Based on field geological observation of the contemporaneous volcanics from Xinyuan and its surrounding areas, it is proposed in the paper that western Tianshan was in a convergent rather than an extensional setting during early-late Carboniferous. The mantle source region might have undergone metasomatism related to subducted sediments and the derived magma may have experienced significant fractional crystallization of olivine and clinopyroxene during the magmatic process.
【Fund】: 国家自然科学基金(项目编号:40421303 40304039)资助
【CateGory Index】: P583
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