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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:

第43卷

期数:

2021年第02期

页码:

291-314

栏目:

基础地质与矿产地质

出版日期:

2021-03-15

文章信息/Info

Title:

Structural Deformation and Mineralization of NNE-striking Gold-bearing Veins in Xiaoqinling Area, Central China

文章编号:

1672-6561(2021)02-0291-24

作者:

陈虹¹; 2; 牟培吉¹; 3; 张欢欢⁴; 朱桂繁¹; 5; 董红毅⁴; 王宏晖¹; 2

(1. 中国地质科学院地质力学研究所,北京 100081; 2. 自然资源部古地磁与古构造重建重点实验室,北京 100081; 3. 中国地质大学(北京)地球科学与资源学院,北京 100083; 4. 陕西地矿第六地质队有限公司,陕西 西安 710611; 5. 自然资源实物地质资料中心,河北 廊坊 065201)

Author(s):

CHEN Hong¹; 2;  MU Pei-ji¹; 3;  ZHANG Huan-huan⁴;  ZHU Gui-fan¹; 5; DONG Hong-yi⁴;  WANG Hong-hui¹; 2

(1. Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China; 2. Key Laboratory of Paleomagnetism and Tectonic Reconstruction of Ministry of Natural Resources, Beijing 100081, China; 3. School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China; 4. Shaanxi Geological and Mineral Sixth Geological Team Co., Ltd., Xi'an 710611, Shaanxi, China; 5. Cores and Samples Center of Natural Resources, Langfang 065201, Hebei, China)

关键词:

控矿构造;  金矿脉;  剪切变形;  燕山期;  印支期;  石英脉型金矿;  多金属硫化物;  小秦岭

Keywords:

ore-controlling structure;  gold-bearing vein;  shear deformation;  Yanshanian;  Indo-sinian;  quartz vein-type gold deposit;  polymetallic sulfide;  Xiaoqinling

分类号:

P613

DOI:

10.19814/j.jese.2021.01031

文献标志码:

A

摘要:

小秦岭金矿田位于华北克拉通南缘的华熊地块北缘,发育有产出于不同走向剪切带内的金矿脉。但是,目前研究和认识对矿脉和剪切带、以及不同方向矿脉之间的构造关系并不清晰。选择小秦岭中部善车峪一带的典型NNE向矿脉开展构造变形与矿化特征研究。结果表明:NNE向金矿脉以右阶排列的石英脉透镜体为特征,主体产状为120°∠70°; 矿脉产出于与之近平行的左行逆冲剪切带内,并改造了早期近EW向剪切带,其所处构造应力场环境为近EW向水平伸展; 矿体的主要矿石矿物为方铅矿、黄铁矿、闪锌矿等多金属硫化物,这些金属矿物多呈条带状或条纹状沿剪切面理或小角度斜交的张剪性面理贯入,显示与左行逆冲变形同期形成的特征。构造变形序列和矿化特征对比分析显示,小秦岭地区NNE向矿脉叠加改造了近EW向矿脉,其构造应力场环境分别与早白垩世和晚三叠世区域应力场特征一致。前人对于岩浆作用、成矿流体和成矿时代等方面的研究结果认为,小秦岭地区经历了印支期和燕山期两期构造与成矿作用的叠加,从而推测NNE向金矿脉应形成于燕山期陆内构造变形阶段,而近EW向矿脉可能形成于印支期华北板块和扬子板块碰撞拼贴阶段。

Abstract:

The Xiaoqinling gold orefield is located on the northern margin of Huaxiong block in the southern margin of North China Craton. There are some gold-bearing veins occurring in the shear deformation belts with different strikes. The structural relationships between the gold-bearing veins and shear deformation belts, as well as the veins with different strikes, are still poorly understood. Structural deformation and mineralization characteristics of the NNE-striking vein, which is located at Shancheyu area in the central of Xiaoqinling area, were analyzed. The results show that the NNE-striking veins, which mainly trend to 120° with dip of 70°, are characterized by lenticular quartz veins with a right-stepping echelon arrangement. The vein occurs in a nearly parallel sinistral thrust shear belt and superimposes on an earlier nearly EW shear belt, where the stress field is nearly EW horizontal extension. The main ore minerals contain the galena, pyrite, sphalerite and other polymetallic sulfide, which are banded and striped intruded along the shear or transtensional foliation with small angle to the shear foliation, and are also concurrent with the sinistral thrust deformation. Comparative analysis of deformation sequence and mineralization characteristics reveals that the NNE-striking veins superimpose on the nearly EW-striking veins in Xiaoqinling area, and the tectonic stress field corresponds to the Early Cretaceous and Late Triassic, respectively. Previous studies on magmatism, ore-bearing fluid and mineralization age indicate that the superimposition of tectonic and metallogenic processes are developed in Indosinian and Yanshanian in Xiaoqinling area, it is indicated that the NNE-striking veins should have been formed in Yanshanian intracontinental deformation stage, while the nearly EW-striking veins might have been formed in Indosinian continental collision between North China and Yangtze plates.

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备注/Memo

备注/Memo:

收稿日期:2021-01-27; 修回日期:2021-02-15投稿网址:http:∥jese.chd.edu.cn/
基金项目:国家自然科学基金项目(41772217); 中国地质调查局地质调查项目(12120114014101)
作者简介:陈 虹(1982-),男,湖南澧县人,中国地质科学院地质力学研究所副研究员,理学博士,2000～2004年在长安大学地质学专业攻读学士学位,2004～2007年在长安大学构造地质学专业攻读硕士学位,E-mail:chhzxm8281@163.com。

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