1. 中国地质大学(武汉)地球科学学院
2. 湖北省地质局第四地质大队
纸质出版:2025
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林子晗, 夏元, 张航川, 等. 幕阜山岩体北缘鄂南地区构造特征与构造控矿作用[J]. 地质科技通报, 2025,44(2):257-269.
林子晗, 夏元, 张航川, et al. 幕阜山岩体北缘鄂南地区构造特征与构造控矿作用[J]. Bulletin of Geological Science and Technology, 2025, 44(2): 257-269.
林子晗, 夏元, 张航川, 等. 幕阜山岩体北缘鄂南地区构造特征与构造控矿作用[J]. 地质科技通报, 2025,44(2):257-269. DOI: 10.19509/j.cnki.dzkq.tb20230525.
林子晗, 夏元, 张航川, et al. 幕阜山岩体北缘鄂南地区构造特征与构造控矿作用[J]. Bulletin of Geological Science and Technology, 2025, 44(2): 257-269. DOI: 10.19509/j.cnki.dzkq.tb20230525.
江南造山带中段幕阜山地区发育规模巨大的早白垩世Li-Be-Cs-Nb-Ta等稀有金属和Pb-Zn-Cu-Au-Sb等有色金属岩浆-热液成矿系统。幕阜山岩体南、北缘的湘东北和鄂南地区具有相同的成矿物质基础,但现有矿产勘探成果差距明显,可能是构造变形差异所致。本研究通过构造解析、古应力场反演以及矿床分布规律,探讨了鄂南地区的构造控矿作用。构造解析表明E-W走向江南断裂形成于新元古代,保存了三叠纪由S向N的逆冲作用、晚白垩世断层上盘向SE的正断作用和古近纪E-W走向左行剪切作用;而NE-SW走向长坪断裂形成于中侏罗世燕山运动,记录了早白垩世晚期左行走滑、晚白垩世正断作用和古近纪晚期右行走滑。基于断层滑移矢量反演的古应力场揭示鄂南地区经历了早白垩世晚期走滑(近N-S向最大主应力)、晚白垩世NW-SE走向伸展、古近纪早期走滑(NE-SW向最大主应力)和古近纪中-晚期NE-SW走向伸展的应力场演化历史。结合研究区的金属矿床分布特征,认为鄂南地区NE-SW走向主干断裂的次级近平行断裂或与其相交的NW-SE走向和近E-W走向断裂具有较好的金属矿产勘探潜力。
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