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吉林省安图县旭阳屯金矿床特征及矿产成因浅析

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旭阳屯金矿床属中低温变质热液矿床,矿石是以含金石英脉型和含金蚀变岩型为主.矿床规模为小型,矿床处于华北板块北缘东段多金属成矿带上,矿床含矿热液流体沿着北东向压扭性断裂上侵,具有多期脉动形成特点.矿床矿体多赋存在太古界老牛沟岩组区域变质岩中.矿体主要受硅化蚀变体和北东向压扭性构造控制.矿床外围和深部找矿潜力巨大.
Analysis on characteristics and mineral genesis of Xuyangtun gold deposit in Antu County,Jilin Province
The Xuyangtun gold deposit belongs to a medium low temperature metamorphic hydrothermal deposit,and the ore is mainly composed of gold-bearing quartz veins type and gold-bearing altered rock type.The deposit is small in scale and located on the eastern section of the northern margin of North China Plate's polymetallic metallogenic belt.Ore-forming hydrothermal fluids ascended along northeast-trending compression and torsional faults,exhibiting multi-stages pulsating formation characteristics.The ore deposits and bodies are mostly found in metamorphic rocks of the Archean Laoniugou For-mation.The ore body is mainly controlled by silicified alteration bodies and northeast-oriented compressional and torsional structures.There is significant exploration potential exists in the peripheral and deeper parts of this deposit.

Ore body trendcompression-torsion structuredeposit characteristicsgenesis of depositXuyangtun

梁敬、李明涛、马冰心、周庆日、孔伟思

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吉林省有色金属地质勘查局六○七队,吉林吉林市 132013

矿体走向 压扭性构造 矿床特征 矿床成因 旭阳屯

2024

吉林地质
吉林省地质矿产勘查开发局

吉林地质

影响因子:0.263
ISSN:1001-2427
年,卷(期):2024.43(3)