越南与原生金有关的岩浆岩的地质构造和年龄

Q3 Earth and Planetary Sciences
Le Tuan, Nguyen Hoang, Vu Cam
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引用次数: 0

摘要

许多学者都对越南的金矿研究很感兴趣。迄今为止,越南境内的地质矿产研究已确定有数百处金矿。与越南原生金有关的构造已被确定为长山褶皱带/东印度支那块体和中越复合地层,对应于古生代早期内部内容的山地带和变质程度较高的地区。与成矿带相关的岩浆构造主要在 P3-T1 期含金,越南的原生金与褶皱构造密切相关。越南原生金的矿石类型为石英-多金属硫化物-金(银)和石英-硫化物-金。我们的研究成果有助于为寻找越南原生金指明方向。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Geological Structures and Age of the Magmatic Rocks Related to Primary Gold in Vietnam
The research on gold in Vietnam has been interesting to many authors. So far, studies on Geology-Minerals on the territory of Vietnam have determined that there are hundreds of gold mineralization. The structures related to primary gold in Vietnam have identified as Truong Son Fold Belt/ East Indochina Block and Sino-Vietnam composit Terran corresponding to Mountain belt internal contents early Paleozoic and Areas with high metamorphism. The magma formations associated with the mineralization zone contain gold mainly in the P3-T1 period, primary gold in Vietnam is closely related to the folding structure. Primary gold in Vietnam is an ore type of quartz-polymetallic sulfide-gold (silver) and quartz-sulfur-gold. Our research results have contributed to orienting the search for primary gold in Vietnam.
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来源期刊
Iraqi Geological Journal
Iraqi Geological Journal Earth and Planetary Sciences-Geology
CiteScore
1.80
自引率
0.00%
发文量
152
审稿时长
7 weeks
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