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Gold Veins Location in Deposits Originated by a Slanting Magma Intrusion Dike

机译:金矿位于倾斜岩浆侵入堤坝中的矿床中

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The location of gold veins, due to a slanting magma dike intrusion in a cold rock, considering earth surface effects is determined. The 400°C and 500°C isotherm evolution resulting from this magma intrusion are studied considering a 2-D model. In this analysis, it is shown that the isotherm envelopes are the most important surfaces. Analytic solutions have been found as a function of the angle a between the dike and the vertical planes. The present results are more general than previous ones in the contest of vertical dikes. Magma convection has been considered in a simplified way. The agreement found that the results in the work the actual vein sites at the gold mine, called Colombia, in the auriferous area of El Callao, located 180 Km south of Ciudad Guayana in Bolivar state, Venezuela, are much better than in previous works.
机译:考虑到地球表面效应,确定了冷岩中岩浆岩倾斜的侵入所导致的金矿脉位置。考虑到二维模型,研究了这种岩浆侵入导致的400°C和500°C等温线演变。在该分析中,表明等温线包络线是最重要的表面。已经发现解析解是堤坝和垂直平面之间的角度α的函数。在垂直堤防竞赛中,目前的结果比以前的结果更为笼统。已经以简化的方式考虑了岩浆对流。该协议发现,在工作中,委内瑞拉玻利瓦尔州瓜亚纳城以南180公里处的El Callao含金地区的哥伦比亚金矿的实际矿脉结果比以前的工作要好得多。

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