安徽大别山及邻区区域地质调查进展与问题讨论

汤加富; 钱存超; 娄清

doi:10.12097/j.issn.1671-2552.2001.02.005

汤加富, 钱存超, 娄清. 2001: 安徽大别山及邻区区域地质调查进展与问题讨论. 地质通报, 20(2): 128-136. DOI: 10.12097/j.issn.1671-2552.2001.02.005

引用本文:

汤加富, 钱存超, 娄清. 2001: 安徽大别山及邻区区域地质调查进展与问题讨论. 地质通报, 20(2): 128-136. DOI: 10.12097/j.issn.1671-2552.2001.02.005

TANG Jia-fu, QIAN Cun-chao, LOU Qing. 2001: Progress in regional geological surveys in the Dabie Mountains,Anhui,and theiradjacent areas: with a discussion. Geological Bulletin of China, 20(2): 128-136. DOI: 10.12097/j.issn.1671-2552.2001.02.005

Citation:

TANG Jia-fu, QIAN Cun-chao, LOU Qing. 2001: Progress in regional geological surveys in the Dabie Mountains,Anhui,and theiradjacent areas: with a discussion. Geological Bulletin of China, 20(2): 128-136. DOI: 10.12097/j.issn.1671-2552.2001.02.005

安徽大别山及邻区区域地质调查进展与问题讨论

Progress in regional geological surveys in the Dabie Mountains,Anhui,and theiradjacent areas: with a discussion

摘要

摘要: 通过对覆盖安徽大别山及邻区的地质调查和深入研究,重建了区内各个地段的构造地层序列及其对比方案,阐明了区内3期构造变形特征、构造型式与形成时期;确定了大量新元古代碱性变质花岗岩的存在;对榴辉岩的成因、形成时代,以及区内是否存在蓝片岩-黄片岩-榴辉岩的变质分带等提出了不同认识。在此基础上,对大别造山带形成机理提出了非印支期碰撞造山的认识。

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