| 内蒙古中部地区金矿床控矿构造类型 |
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| 引用本文： | 梁一鸿,张业明.内蒙古中部地区金矿床控矿构造类型[J].黄金,1993,14(2):5-9. |
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| 作者姓名： | 梁一鸿 张业明 |
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| 作者单位： | 长春地质学院
(梁一鸿，孙德育)，宜昌地质研究所(张业明) |
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| 摘 要： |
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| 关 键 词： | 金矿 控矿构造类型 内蒙古 |
The types of ore-controlling structures for gold deposits In the area of Central Inner Mongolia |
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| Liang Yihong Sun Deyu Zhang Yeming.The types of ore-controlling structures for gold deposits In the area of Central Inner Mongolia[J].Gold,1993,14(2):5-9. |
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| Authors: | Liang Yihong Sun Deyu Zhang Yeming |
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| Affiliation: | Liang Yihong Sun Deyu Zhang Yeming
(Changchun University of (Yicang Institute
Earth Science) of Geology) |
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| Abstract: | According to structural analysis of typical gold deposits in Central Inner Mongolia, the ore-controlling structures of gold deposits in the area are classified into three types, i.e.duetile shear zone, kink-bands and brittle faults.
A ductile shear zone can be an ore-controlling tectonic zone, also a relatively enriched zone of gold and can control gold deposits directly during ductile shea-ring. There are special ore-bearing spaces in a kink-band.They are expanded fractures parallel to the strike direction of the bed near kink band, the tensional fractures obliquely crossing the strike direction of the bed near the kink band, and the saddle spaces in the turning part of the kink band. Brittle faults In the area can be divided into three types, the east-west faults formed before mineralization, the NNE faults formed during mineralization and the east-west faults formed after mineralization. It is favorable for mineralization when the east-west faults formed before mineralization are opened during mineralization. |
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| Keywords: | gold deposit ductile shear zone kink band fractural structure types of ore-controlling structure |
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