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秦岭—祁连造山带印支-燕山期构造与大型-超大型矿床的形成关系
引用本文:杜玉良,汤中立,蔡克勤,李文渊,张韬.秦岭—祁连造山带印支-燕山期构造与大型-超大型矿床的形成关系[J].矿床地质,2003,22(1):65-71.
作者姓名:杜玉良  汤中立  蔡克勤  李文渊  张韬
作者单位:1. 中国地质大学,北京,100083;西安地质矿产研究所,陕西,西安,710054
2. 甘肃省地质矿产勘查开发局,甘肃,兰州,730000
3. 中国地质大学,北京,100083
4. 西安地质矿产研究所,陕西,西安,710054
摘    要:印支-燕山期构造-岩浆热液活动,对秦岭-祁连造山带的区域成矿控制与影响作用十分显著,主要表现在该期北东向构造-岩浆活动不仅控制了金等矿产的形成,而且使先期形成的铜,铅锌等矿产发生了较强烈的改造和富集作用,该期北东向构造带与先期的北西、近东西向构造或含矿层交汇叠加部位,是形成大型-超大型矿床的重要条件。文章对秦岭-祁连造山带印支-燕山期构造-岩浆活动带的发育特征及其对大型-超大型矿床的控制与影响等进行了初步分析与探讨,提出了本区新一轮矿产勘查研究对策与思路。

关 键 词:地质学  秦岭-祁连造山带  印支-燕山期构造  大型-超大型矿床  富集作用  岩浆活动
文章编号:0258-7106(2003)01-0065-07

Relationship Between Indosinian-Yanshanian Tectonic Framework and Large-Superlarge Mineral Deposits in Qinling-Qilian Orogenic Belt
DU YuLiang ,TANG ZhongLi,CAI KeQin,LI WenYuan,ZHANG Tao.Relationship Between Indosinian-Yanshanian Tectonic Framework and Large-Superlarge Mineral Deposits in Qinling-Qilian Orogenic Belt[J].Mineral Deposits,2003,22(1):65-71.
Authors:DU YuLiang    TANG ZhongLi  CAI KeQin  LI WenYuan  ZHANG Tao
Institution:DU YuLiang 1,2,TANG ZhongLi3,CAI KeQin1,LI WenYuan2,ZHANG Tao 1,2
Abstract:It is obvious that the Indosinian-Yanshanian tectono-magmatic activities controlled and affected the ore-forming process of the Qinling-Qilian orogenic belt. This finds expression in the fact that the Indosinian-Yanshanian NE-trending structures not only controlled the mineralization of gold and other metallic minerals but also caused the considerable reformation and enrichment of the earlier-formed copper, zinc, lead and other minerals. Where the NE-trending structures intersected or are superimposed on the earlier-formed NW- and nearly EW-trending structures or ore-bearing formations, the large and superlarge mineral deposits are likely to be formed. In this paper, the characteristics of the Indosinian-Yanshanian tectono-magmatic belt which controlled and affected the formation of large-superlarge mineral deposits are analyzed and discussed, and new measures and thinking are put forward for carrying out a new round of mineral exploration in this region.
Keywords:geology  Qinling-Qilian orogenic belt  Indosinian-Yanshanian tectonic framework  reformation and enrichment  large-superlarge mineral deposits
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