首页> 外文期刊>大地构造与成矿学(英文版) >NUMERICAL GEODYNAMIC MODELLING OF COUPLED MECHANO-THERMO-HYDROLOGICAL PROCESSES AND ITS APPLICATION IN PREDICTIVE EXPLORATION IN THE FENGHUANGSHAN ORE FIELD, TONGLING
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NUMERICAL GEODYNAMIC MODELLING OF COUPLED MECHANO-THERMO-HYDROLOGICAL PROCESSES AND ITS APPLICATION IN PREDICTIVE EXPLORATION IN THE FENGHUANGSHAN ORE FIELD, TONGLING

机译:铜陵凤山矿田耦合热力水文过程数值地球动力学模拟及其在预测勘探中的应用

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摘要

Mineralisation is the result of the coupled multi-geodynamic processes in the crust. The coupled mechano-thermo-hydrological (MTH) processes are the basic physical processes that govern the location of the hydrothermal mineralization, which can be simulated in the computer by using of the numerical codes, such as FLAC. The numerical modeling results can be used not only to explain the features of existing ore deposits, but also to predict the favorable mineralization locations. This paper has summarized the basic equations describing coupled MHT processes in the water-saturated porous rocks, the principles of FLAC, and its application to the MHT processes related to copper mineralization in the Fenghuangshan ore field. We used the FLAC to simulate the syn-deformation cooling and fluid flowing evolution after the intrusion was emplaced and solidified. The modeling results suggest a most prospective exploration area where the subsequent exploration supported the prediction and the test bore hole disclosed the high quality copper ore bodies in the target, demonstrating a positive role of the numerical MTH modeling in facilitating predictive ore discovery.
机译:矿化是地壳中多重地球动力学过程耦合的结果。机械-热力水文(MTH)过程是控制水热矿化位置的基本物理过程,可以通过使用数字代码(例如FLAC)在计算机中对其进行模拟。数值模拟结果不仅可以用来解释现有矿床的特征,而且可以用来预测有利的矿化位置。本文总结了描述饱和水孔隙岩中MHT耦合过程的基本方程式,FLAC原理及其在凤凰山矿田与铜矿化相关的MHT过程中的应用。我们使用FLAC来模拟侵入体放置和固化后的同相变形冷却和流体流动演变。建模结果表明了最有前途的勘探区域,后续的勘探支持了该预测,并且测试钻孔揭示了目标中的高质量铜矿体,证明了数值MTH建模在促进预测矿石发现方面的积极作用。

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