末造山带金矿成矿环境

N. Duke
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引用次数: 0

摘要

这个思想项目的重点是造山带内黄金富集的时间和地点,造山带是由板块相互作用产生的最复杂的构造环境。笔者从事黄金勘探工作已有50多年,并借此机会反思“我认为我学到了什么”。当被大量直接的实地证据所压倒,再加上大量的岩石学和地球化学数据,几乎不可能“只见树木不见森林”。通常,报告特定的“数据集”被当作科学的目标,而真正的问题,即所有证据加起来意味着什么,从来没有涉及到。这是退后一步,从更大的角度看待区域变质作用和热变质作用、深部成矿作用和火山作用以及热液环境下的海相和陆相沉积作用所描绘的更大图景的努力。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The Metallogenic Setting of Terminal Orogenic Gold Deposits
This thought project is focused on the time and place of gold concentration within orogens, the most complex of the tectonic settings resulting from plate interactions. The author has been engaged in gold exploration over his 50-year career and takes this occasion for reflection on “what I think I learned”. When overwhelmed by the wealth of immediate field evidence, combined with the mountains of petrographic and geochemical data it is nigh impossible “to see the forest for the trees”. All too often reporting of specific “data sets” passes as the goal of science while the real problem, i.e. what all the evidence in combination adds up to, is never engaged. This is an effort to step back and take a larger view of the bigger picture painted by the various roles played by regional and thermal metamorphism, plutonism and volcanism, as well as marine and terrestrial sedimentation within hydrothermal environments of gold concentration.
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