左旋走滑背景下的矿柱形成:对保加利亚西南部布列兹尼奇地区金银米林卡马克矿床地图的解释

IF 0.2 Q4 GEOSCIENCES, MULTIDISCIPLINARY
Dian Strahilov, P. Doychev, I. Dimitrov
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引用次数: 0

摘要

本文介绍了保加利亚西南部一个著名金矿的构造解释。解释依据是在找矿过程中收集的地质图和构造资料。研究结果表明,低阶左旋剪切体系是由区域左旋剪切作用形成的,在剪切拉张和剪切压缩的共同作用下,形成了成矿空间。这两种机制打开了张力裂缝,扩大了先前形成的里德尔断层,并弯曲了矿脉和断层。当结构在区域剪切间隙的压缩象限中逆时针旋转从而产生屈曲结构时,就会发生屈曲。矿脉已在主剪切带的扩展区域和沿先前形成的扩大的里德尔剪切带形成。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Ore shoots formation in a sinistral strike-slip setting: an interpreted from the map of the Au-Ag Milin Kamak deposit in the Breznic area, Southwest Bulgaria
This work presents а structural interpretation of a well-known gold deposit from SW Bulgaria. The interpretation is based on the geological map and structural data, collected during the prospecting. The data indicates that а regional sinistral shearing was responsible for a low rank sinistral shear system, which created ore depositional space by the combined action of shear extension and compression. The two mechanisms opened tension gashes, dilated previously formed Riedel faults and buckled the veins and the faults. The buckling happened, when the structures were rotated anticlockwise in the compressional quadrant of the space between the regional shears thus creating buckling structures. Ore shoots have been formed in the extended domains of the main shear and along the dilated previously formed Riedel shears.
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