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首页> 外文期刊>Ore Geology Reviews: Journal for Comprehensive Studies of Ore Genesis and Ore Exploration >The mechanisms of the infill textures and its implications for the five-floor zonation at the Dajishan vein-type tungsten deposit, China
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The mechanisms of the infill textures and its implications for the five-floor zonation at the Dajishan vein-type tungsten deposit, China

机译:中国大吉山脉状钨矿床充填构造的机理及其对五层带的意义

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Infill textures in thick veins are one of the most important characteristics in vein-type tungsten deposits, China. One of the prerequisites for forming these textures is low wallrock permeability, but its mechanisms have not been well understood. In this contribution, we investigated the mechanisms leading to low wallrock permeability at the Dajishan tungsten deposit by conducting finite element computer experiments. The numerical experiments suggest that the hydrostatic compression exerted by high-pressure fluids on the wallrock decreases the wallrock permeability significantly in a short geological time. The deeper part of the deposit is more likely to create low wallrock permeability and form infill textures than the shallower part. The hydrostatic compression also prohibits the fluid flow from the fracture zone to the country rock and limits water-rock interactions. Therefore, the hydrostatic compression facilitates both the fluid focusing and the high ore-formation efficiency in fracture zones. These conclusions help us better understand the mechanisms of infill textures and the five-floor zonation at Dajishan. (C) 2014 Elsevier B.V. All rights reserved.
机译:中国脉型钨矿床的最重要特征之一是厚脉中的填充纹理。形成这些纹理的先决条件之一是低围岩渗透率,但其机理尚未得到很好的理解。在这项贡献中,我们通过进行有限元计算机实验研究了导致大吉山钨矿床低围岩渗透率的机理。数值实验表明,高压流体在围岩上施加的静水压力会在较短的地质时间内显着降低围岩的渗透率。与较浅的部分相比,沉积物的较深部分更可能产生较低的围岩渗透率并形成填充纹理。静水压缩还阻止流体从裂缝区流到乡村岩石,并限制了水岩相互作用。因此,静水压缩既有利于流体聚集又有利于裂缝带的高成矿效率​​。这些结论有助于我们更好地了解大吉山的填充纹理和五层分区的机制。 (C)2014 Elsevier B.V.保留所有权利。

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