巴林杰奖章演说

V. Masaitis
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引用次数: 13

摘要

-陆地撞击坑是重要的地质和地貌学对象,不仅对科学研究而且对工业和商业目的都具有重要意义。这些构造可能含有受某些形态、构造或岩性因素控制的靶岩(包括原生成矿矿)热力转化直接产生的商品矿物,并暴露在火山口中。铁和铀矿石、有色金属、钻石、煤、油页岩、碳氢化合物、矿泉水和其他原材料都出现在撞击坑中。冲击形态结构可用于气体或液体废物的地下储存。地表陨石坑可以作为水力发电的水库。这些环形结构可能在其他方面对社会有价值。对它们的科学研究在比较行星学、陆地地质学和其他自然科学领域尤为重要。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The Barringer Medal Address
— Terrestrial impact craters are important geological and geomorphological objects that are significant not only for scientific research but for industrial and commercial purposes. The structures may contain commercial minerals produced directly by thermodynamic transformation of target rocks (including primary forming ores) controlled by some morphological, structural or lithological factors and exposed in the crater. Iron and uranium ores, nonferrous metals, diamonds, coals, oil shales, hydrocarbons, mineral waters and other raw materials occur in impact craters. Impact morphostructures may be used for underground storage of gases or liquid waste material. Surface craters may serve as reservoirs for hydropower. These ring structures may be of value to society in other ways. Scientific investigation of them is especially important in comparative planetology, terrestrial geology and in other divisions of the natural sciences.
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