Geology and Metallogenic Conditions of Taishanmiao Gold Deposit in Ningshanxian of Shanxi Province

白海成

doi:10.16056/j.1005-7676.2018.03.012

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Geology and Metallogenic Conditions of Taishanmiao Gold Deposit in Ningshanxian of Shanxi Province

更新时间：2026-01-19

- Geology and Metallogenic Conditions of Taishanmiao Gold Deposit in Ningshanxian of Shanxi Province
- Issue 3, Pages: 44-49(2018)
- 作者机构：
  
  陕西省煤层气开发利用有限公司
- 作者简介：
- 基金信息：
- DOI：10.16056/j.1005-7676.2018.03.012
  CLC： P618.51
- Published：2018
- 稿件说明：
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[1]白海成.陕西省宁陕县太山庙金矿床成矿地质特征及成矿简析[J].能源研究与管理,2018(03):44-49.

白海成. Geology and Metallogenic Conditions of Taishanmiao Gold Deposit in Ningshanxian of Shanxi Province[J]. 2018, (3): 44-49.
[1]白海成.陕西省宁陕县太山庙金矿床成矿地质特征及成矿简析[J].能源研究与管理,2018(03):44-49. DOI： 10.16056/j.1005-7676.2018.03.012.

白海成. Geology and Metallogenic Conditions of Taishanmiao Gold Deposit in Ningshanxian of Shanxi Province[J]. 2018, (3): 44-49. DOI： 10.16056/j.1005-7676.2018.03.012.

摘要

太山庙金矿床的成矿物质来源于矿区北部的印支期胭脂坝黑云母二长花岗岩体。区内断裂构造发育较好

为成矿提供了运移通道

岩浆期后从岩浆中分泌出来的含矿气液沿着围岩中的裂隙向上运移

运移过程中受到多种成矿条件的影响

在构造破碎带适宜地段冷凝沉淀

历经长期的、多期次的成矿作用

最终富集成矿

区内找矿标志明显。

Abstract

The metallogenic material of gold deposit in Taishanmiao came from biotite monzonitic granite of Indosinian Rouge dam in the northern part of the mining area. The fault structures in the area are well developed

providing migration pathways for mineralization. After the magmatic phase

it migrates upward from the cracks in the magma. In the process of migration

it was affected by various metallogenic conditions. It condenses and precipitates in the suitable section of the tectonic fractured zone

after long-term and multi-phase mineralization

it eventually enriches the mineralization

and the prospecting marks are obvious in the area.

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