魏凯里河、北韦塔尔和马鲁古西南部的金属矿产潜力

Subhan Arif, Nurul Dzakiya, Maulana Mairatu Tuheteru
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摘要

现代社会,随着工业的发展,对作为技术原材料的金属的需求不断增加。金属被广泛应用于建筑、汽车、电子和可再生能源等各个领域。然而,目前使用的金属供应有限,并在供应和环境影响方面带来了挑战。为了克服这些限制,必须寻找新的金属资源。通过全面的地质研究,特别是在尚未被广泛勘探的地区,可以发现新金属矿藏存在的潜力。本研究关注的一个地区是马鲁古西南部乌哈克村的魏凯里河。本研究旨在探索马鲁古西南部 Weikeri 河地区和 Uhak 村的金属沉积潜力。本研究采用地表地质调查技术,通过文献研究阶段和实地地质研究阶段进行。野外研究旨在获取岩性、地质结构、蚀变和矿化数据。野外研究结果表明,研究地点由水下火山岩组成。岩石蚀变条件以安山岩岩性中的阳起石蚀变类型为主,包括熔岩和以尖晶石和岩屑形式存在的侵入体。其他蚀变为箭状和硅化。发现的矿化条件是角砾岩石英脉系统。所发现的矿物是黄铁矿、方铅矿和黄铜矿形式的硫化物矿物。这些矿物在地表的存在比例为 1-3%。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Potential of Metal Minerals in the Weikeri River, North Wetar, and Southwest Maluku
The modern era, demand for metals as raw materials in technology continues to increase along with industrial development. Metals are used in various sectors, such as construction, automotive, electronics, and renewable energy. However, the availability of currently used metals is limited and poses challenges in terms of supply and environmental impact. To overcome these limitations, it is important to search for new metal resources. The potential for the existence of new metal deposits can be discovered through comprehensive geological research, especially in areas that have not been widely explored. One area of interest for this research is the Weikeri River, Uhak Village, Southwest Maluku. This research aims to explore the potential for metal deposition in the Weikeri River area and Uhak Village, Southwest Maluku. Using surface geological survey techniques, this research was carried out through a literature study stage and then a field geology study. Field studies are aimed at obtaining lithology, geological structure, alteration, and mineralization data. The results of field research show that the research location is composed of underwater volcanic rocks. Rock alteration conditions are dominated by the propylitic alteration type in andesite lithology, both in lava and in intrusions in the form of dikes and sills. Other alterations are argillic and silicified. The mineralization condition found was a brecciated quartz vein system. The resulting minerals found were sulfide minerals in the form of pyrite, galena, and chalcopyrite. The percentage of the presence of these minerals ranges from 1–3% on the surface.
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