| 注册
首页|期刊导航|地质找矿论丛|内蒙古大井子铜锡矿床控矿构造特征及成矿流体运移

内蒙古大井子铜锡矿床控矿构造特征及成矿流体运移

董业才 邢全力 王建超 徐文杰

地质找矿论丛2025,Vol.40Issue(2):197-205,9.
地质找矿论丛2025,Vol.40Issue(2):197-205,9.DOI:10.6053/j.issn.1001-1412.2025.02.007

内蒙古大井子铜锡矿床控矿构造特征及成矿流体运移

Characteristics of ore-controlling structure and migration of ore-forming fluids in the Dajingzi Cu-Sn deposit,Inner Mongolia

董业才 1邢全力 2王建超 1徐文杰1

作者信息

  • 1. 中国有色桂林矿产地质研究院有限公司,广西桂林 541004
  • 2. 中国有色集团沈阳矿业投资有限公司,辽宁 沈阳 110014
  • 折叠

摘要

Abstract

The characteristics of ore-controlling structure in the Dajingzi deposit are studied.The ore-controlling structure of ore bodies can be classified to four styles:upward tension-torsion,downward slip,mixed ore-forming,and late ore-breaking.Migration of ore-forming fluids is related to the subvolcanic uplift.During early thermal uplift,the ore-forming fluids filled along tension-torsion faults,forming steep veins with narrow amplitude.As magma cools,the ore-forming fluids filled along inter formation slip faults,forming gentle veins with wide amplitude.In the late stage subvolcanoes collapsed under the influ-ence of gravity,resulting in the ore-breaking structure.Ore bodies are controlled by different structural styles and differences of mineralization characteristics result from the different ore fluid migration.The a-bove mentioned not only explain why the veins are distributed in groups or belts in NW-NWW direction,but also provide an important basis for prospecting similar concealed deposits in other sections of the Da-jingzi ore field.

关键词

次火山热隆/控矿构造样式/成矿流体运移/铜锡矿床/岩浆侵入/层间滑动断裂

Key words

subvolcanic themal uplift structure/ore-controlling structural styles/migration of ore-forming fluids/Cu-Sn deposit/magma intrusion/inter formation slip fault

分类

天文与地球科学

引用本文复制引用

董业才,邢全力,王建超,徐文杰..内蒙古大井子铜锡矿床控矿构造特征及成矿流体运移[J].地质找矿论丛,2025,40(2):197-205,9.

基金项目

中国有色集团科技计划项目"大兴安岭南段稀有-铜多金属找矿关键勘查技术研究与示范"(编号:2023KJZX02)、"大型有色金属矿山深边部找矿预测及综合技术示范研究"(编号:2018KJJH07)、"金属矿床快速预测定位关键技术与示范"(编号:2017KJJH02)共同资助. (编号:2023KJZX02)

地质找矿论丛

1001-1412

访问量0
|
下载量0
段落导航相关论文