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《Acta Geological Sinica》 1988-03
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OROGENIC AND ANOROGENIC GRANITOIDS OF THE ALTAY MOUNTAINS,XINJIANG AND THEIR DISCRIMINATION CRITERIA

Zou Tianren(Institute of Mineral Deposits, Chinese Academy of Geological Sciences, Beijing) Cao Huizhi and Wu Boqing(Xinjiang Institute of Metallurgy and Geology, Ulumuqi)  
The grantioid rocks comprise 40% of the rocks exposed in the Altay Mountains area. Based on many years of study, they are divisible into two series; (1) the orogenic granitiod series generated in the marginal zone of compressional plate (the north belt), and (2) the anorogenic granitoid series generated at extensional plate boundaries (the south belt). The two series can be distinguished according to the following characters:
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