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广西大厂锡矿“东岩墙”地质特征与控矿作用 被引量:12

The geological characteristics and ore-controlling role of the east dyke in Dachang deposit in Guangxi
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摘要 "东岩墙"位于广西大厂铜坑-长坡锡矿(大厂主体矿山)东侧,一直被认为是单一花岗斑岩岩墙。文章研究认为"东岩墙"除了花岗斑岩外,还有次玄武岩、闪长玢岩及构造破碎带。"东岩墙"是一SN向、多期次构造-岩浆活动带,是大厂锡矿的主要控岩控矿构造。 East dyke is located at Tongkeng -- Changpo tin mine on the eastern side in Guangxi Dachang. It has always been regarded as a single granite--porphyry dyke. Through the research, the authors found that for the composition of east rock wall, in addition to granite--porphyry, there are sub--basalt, diorite porphyry and tectonic fracture zone. The east dyke is actually a north--south, multi--phase tectonic--magmatic belt. It is the main ore and rock controlling structure of Dachang tin deposit.
出处 《矿产与地质》 2009年第5期406-411,共6页 Mineral Resources and Geology
关键词 锡矿床 控岩控矿构造 构造岩浆带 广西大厂 tin deposit, ore and rock controlling structure, tectonomagmatic belt, Dachang of Guangxi
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  • 1秦德先,洪托,田毓龙,等.广西大厂锡矿92号矿体地质与技术经济[M].北京:地质出版社,2002.
  • 2秦德先.近年在我国三个特大型锡矿床中相继发现的火山(成矿)作用及其科学意义[J].昆明理工大学学报(理工版),2008,33(1):123-124. 被引量:14
  • 3李昌年.火成岩微量元索岩石学[M].武汉:中国地质大学出版社,1992.
  • 4Qin Dexian, Chen Jianwen, Zhao Rusong. Geology and geochemistry of the super-large modified emanated-sedimenrary Daehang TinDeposit in Guanxi provice[A]. Papers to 30thIGC [C]. 1996:495-498.

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