青海省锡铁山铅锌矿床沉积盆地构造与找矿方向浅议

李正明; 王备战; 展卫露; 战嘉华; 郭文波; 王宏宇; 董星; 李增涛

doi:10.12401/j.nwg.2023173

青海省锡铁山铅锌矿床沉积盆地构造与找矿方向浅议

1.
西部矿业股份有限公司，青海西宁　810000

2.
西安西北有色物化探总队有限公司，陕西西安　710068

基金项目: 西北有色地质矿业集团地质科技项目“复杂条件下深部矿产高分辨电磁探测关键技术研究与工程示范”（XBDKKJ202101）。

详细信息

作者简介: 李正明（1987−），男，工程师，主要从事矿山地质工作。E−mail：455084813@qq.com

通讯作者: 王备战（1970−），男，高级工程师，主要从事矿产勘查工作。E−mail：728567950@qq.com。

中图分类号: P618.42；P618.43

收稿日期: 2022-10-05

修回日期: 2023-09-05

刊出日期: 2025-02-20

Discussion on Structure and Prospecting Direction of Xitieshan Lead-zinc Deposit Sedimentary Basin in Qinghai Province

1.
Western Mining Co., Ltd., Xining 810000, Qinghai, China

2.
Xi’an Northwest Non-ferrous Geophysical and Chemical Exploration Group Co., Ltd, Xi'an 710068, Shaanxi, China

More Information

Corresponding author: WANG Beizhan, 728567950@qq.com

Received Date: 05 October 2022

Revised Date: 05 September 2023

Publish Date: 20 February 2025

摘要

摘要:
锡铁山铅锌矿床位于柴达木盆地北缘，矿体主要产于奥陶系滩间山群O₃tn^a-2正常沉积岩段。对深部构造的探测和原始成矿环境的恢复一直是勘查研究工作的重点。矿山以往深部找矿投入了瞬变电磁法（TEM）和可控源音频大地电磁测深法（CSAMT），对深部的结构、构造反映不够清楚，找矿效果也不理想。2020年首次投入了高分辨广域电磁法（WEFM），取得了较好的勘查效果。笔者结合已有的地质资料，对广域电磁法成果进行综合分析，初步认为锡铁山铅锌矿床原始沉积盆地走向为EW向，属于南高北低的抬斜式盆地。受NE-SW向的斜向推覆作用，形成目前盆地的构造形态；同时推测盆地内部存在两条主要的同生断裂。笔者依据同生断裂和已知矿体的空间位置预测了找矿靶区，指出了锡铁山沉积盆地内铅锌矿的找矿方向。
- 锡铁山铅锌矿 /
- 原始沉积盆地 /
- 广域电磁法 /
- 斜向推覆 /
- 找矿方向
Abstract:
Xitieshan lead-zinc deposit is located in the northern margin of Qaidam Basin, and the ore body is mainly produced in the normal sedimentary rock section of O₃tn^a-2 of the Ordovician Tanjianshan Group. The exploration of deep structures and the restoration of the original metallogenic environment have always been the focus of exploration and research work. In the past, transient electromagnetic method (TEM) and controlled source audio frequency magnetotelluric sounding (CSAMT) were used in deep prospecting of the mine, which did not reflect the deep structure and structure clearly enough, and the prospecting effect was not ideal. In 2020, the high-resolution wide area electromagnetic method (WEFM) was put into use for the first time, and good exploration results were achieved. Based on the existing geological data and the comprehensive analysis of the results of the wide area electromagnetic method, this paper preliminarily believes that the original sedimentary basin of the Xitieshan lead-zinc deposit is oriented in the east-west direction and belongs to an uplifted basin with the south high and the north low. Due to the NE－SW oblique nappe, the current structural form of the basin was formed; At the same time, it is speculated that there are two main contemporaneous faults in the basin. Based on the syngenetic faults and the spatial location of known ore bodies, this paper predicts the prospecting target area and points out the prospecting direction of lead-zinc deposits in the Xitieshan sedimentary basin.
- Xitieshan lead-zinc mine /
- primitive sedimentary basin /
- WFEM /
- oblique nappe action /
- prospecting direction

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图 1 锡铁山铅锌矿区地质简图（据魏俊浩等，2015）

Figure 1.

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图 2 推测深部成矿通道在地表的投影范围示意图

Figure 2.

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图 3 锡铁山铅锌矿区015线断面及推断成果图

Figure 3.

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图 4 锡铁山铅锌矿区找矿靶区预测图

Figure 4.

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表 1 岩矿石电性参数统计表

Table 1. Statistical table of electrical parameters of rocks and ores

岩（矿）石名称	块数	电阻率ρ（Ω·m）
岩（矿）石名称	块数	变化范围	几何平均值
块状铅锌矿	34	0.1～11	0.2
碳质绿泥片岩	6	90～810	170
碳质二云片岩	27	14～400	55
钙质绿泥片岩	83	800～3700	1800
绢云绿泥片岩	23	530～7570	2290
含碳片麻岩	57	140～8860	1400
片麻岩	55	440～6000	1560
紫色砂砾岩	37	26～2800	1160
角闪岩	95	180～8100	1400
大理岩	56	650～2500	1240

下载: 导出CSV

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