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《Acta Geologica Sinica》 2000-01
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The Formation of Yanshanian Granitic Magma in Dabie Mountains: Dehydration or Aquifer Melting——With Tiantangzhai and Jiuzihe Granites as Examples

Wang Qiang Qiu Jiaxiang Wang RenjingGuangzhou Institute of Geochemistry,Chinese Academy of Sciences, Guangzhou, 510640 China University of Geosciences, Wuhan, 430074  
There are large areas of late Yanshanian granites in the Dabie erogenic belt, but the formation mode of the relevant granitic magma is still under discussion. Taking the typical Yanshaniangranites in the North Dabie block——the Tiantangzhai and Jiuzihe granites as examples, thewriters endeavour to discuss contain aspects of the formation mode of the granitic magma by studying the characteristics of the chemical compositions of biotite and hornblende of the granites and petrological features of enclaves in the intrusions, in the light of recent results of experimental petrology on dehydration melting and aquifer melting. It is suggested that:① Some biotites in the Tiantangzhai and Jiuzihe granites and their enclaves were residual minerals. ② Some of the hornblends could be new-born minerals, and others,residual ones.③ The banded bodies in granites were residuals of anatexis. ④The Tiantangzhai and Jiuzihe granites were formed by aquifer melting, and the South Dabie block could be the important source region of water.
【Fund】: 原地质矿产部基础研究项目“大别山1:5万九资河幅、张家嘴幅区域地质调查”基金
【CateGory Index】: P588.12
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