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Spatial Distribution and Ages of Alkaline Intrusive Rocks in China and Related Tectonics

Spatial Distribution and Ages of Alkaline Intrusive Rocks in China and Related Tectonics

作     者:YUAN Zhongxin BAI Ge 

作者机构:Institute of Mineral Deposits Chinese Academy of Geological Sciences 26 Baiwanzhuang Beijing 100037 

出 版 物:《Acta Geologica Sinica(English Edition)》 (地质学报(英文版))

年 卷 期:1998年第72卷第4期

页      面:363-381页

核心收录:

学科分类:0709[理学-地质学] 070901[理学-矿物学、岩石学、矿床学] 07[理学] 

主  题:alkaline intrusive rock spatial distribution age tectonic China 

摘      要:: On the basis of the geological data from 220 intrusions and isotope ages of 115 rock bodies, the paper discusses the distribution of 18 alkaline intrusive rock belts along deep faults and their relations to the plate tectonic activity. In view of the presence of a large amount of Variscan alkaline rocks of deep-source character, it is inferred that mantle diapirism was very strong in China during the Variscan. Besides anorogenic and postorogenic alkaline granites, there also occur alkaline granites formed in the terminal orogenic stage when the regional tectonic activity was of compressional nature. Finally, the paper discusses the tectonic environment of the Maoniuping nordmarkite in Mianning county, Sichuan province, and the authors consider it to be a compressional environment originating after rift closing.

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