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黑龙江团结沟金矿区花岗斑岩体与金矿化的关系 被引量:9

The relation between gold mineralization and granite porphyry mass of TuanJieGou Gold Field,Heilongjiang Province
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摘要 团结沟金矿区花岗斑岩为岩株状产出的浅成超浅成侵入体。斑岩体内有两期矿化;早期发生在隐爆角砾岩带内,呈环形分布;晚期发生在北西西、北北西构造带内。斑岩体不仅提供成矿热液,也提供部分矿质。 The granite porphyry occurred in TuanJieGou Gold Field is rock plant like hypabyssal/super hypabyssal intrusive mass.Two phases of mineralization took place in porphyry mass.The early phase of it took place in the belt of concealed explosive breccia presenting ringlike distribution while the later phase of it happened in the northwest by west/northwest by north structural belt.The porphyry mass provided not only mineralizing hydrothermal solution but also a part of mineral matter.
作者 李碧乐 王健
机构地区 长春科技大学
出处 《黄金》 CAS 北大核心 1998年第3期3-6,共4页 Gold
关键词 斑岩体 隐爆角砾岩 金矿床 叠加矿化 金矿 porphyry mass concealed explosive breccia northwest by west/northwest by north structural belt superimposed mineralization TuanJieGou Gold Deposit
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参考文献2

  • 1李成范,刘新三.黑龙江省团结淘斑岩金矿的成矿作用.金银矿产选集(第四集),1985.
  • 2江雄新等.团结淘金矿床主要地质特征及其成矿作用.金矿地质论文集,北京:地质出版社,1986.

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