APPLIED GEOPHYSICS
 
        首页  |  版权声明  |  期刊介绍  |  编 委 会  |  收录情况  |  期刊订阅  |  下载中心  |  联系我们  |  English
应用地球物理  2025, Vol. 22 Issue (4): 1284-1296    DOI: 10.1007/s11770-025-1182-3
论文 最新目录 | 下期目录 | 过刊浏览 | 高级检索 Previous Articles  |  Next Articles  
川西义敦岛弧海子山哈嘎拉岩体稀有金属地质-地球物理勘查研究
杨荣,彭宇,青莉,刘前坤*,郝雪峰*,吴晗,范俊波,陈红娟,杨涛
1. 四川综合地质调查研究所,四川成都 610081;2. 中国自然资源航空物探遥感中心,北京 100086;3. 西南交通大学,四川成都 611756;4. 成都理工大学,四川成都 610059
Integrated Geology-Geophysics Exploration of Rare Metal Deposits in the Yidun Island Arc Collisional Orogen
Yang rong, Peng yu, Qing li, Liu Qian-kun*, Hao Xue-feng*, Wu han, Fan jun-bo, Chen hong-juan, Yang tao
1. Sichuan Institute of Comprehensive Geological Survey, Chengdu 610081 2. Aerogeophysical Survey and Remote Sensing Center, Ministry of Natural Resources, P.R.China, Beijing 100086 3. Southwest Jiaotong University, Chengdu 611756 4. Chengdu University of Technology, Chengdu 610059
 全文: PDF (0 KB)   HTML ( KB)   输出: BibTeX | EndNote (RIS)      背景资料
摘要 川西义敦岛弧燕山晚期岩体带是稀有金属成矿的重要区域,然而其深部资源潜力及成矿规律仍不明确。本研究通过系统的地质调查和大功率激电测深技术,对该区域中部哈嘎拉岩体北部内、外接触带的稀有金属矿化脉群进行了详细研究。结果表明,矿化脉体规模显著,脉宽可达15米,长度超过850米,含有经济价值的锂、铍、铌、钽、钨和锡。深部电法探测显示,这些矿脉在深部显著延伸,表明资源潜力巨大。这项研究不仅揭示了该地区稀有金属资源的经济潜力,还为岛弧环境下稀有金属成矿机制提供了新的见解。
服务
把本文推荐给朋友
加入我的书架
加入引用管理器
E-mail Alert
RSS
作者相关文章
关键词义敦岛弧   稀有金属   哈嘎拉岩体   激发极化法   矿化脉体     
Abstract: The Late Yanshanian granite belt in the Yidun Island Arc of western Sichuan constitutes a critical rare metal metallogenic zone along the eastern margin of the Tibetan Plateau, yet its deep-seated resource distribution has remained poorly understood. Focusing on the northern contact zone of Hagala rock mass, this study innovatively integrates geological mapping, high-power induced polarization (IP) sounding (AB/2=1500m, MN=20m), and 3D modeling to systematically constrain the spatial architecture and resource potential of deep-seated ore bodies. Key fi ndings include: (1) Surface discovery of 12 NW-trending pegmatitetype Nb-Ta-Li-Be veins, with the No.3 principal vein exhibiting maximum dimensions (850m length ×5-15m width) and average grades of 0.031% Ta?O? and 0.017% Nb?O? - significantly exceeding industrial thresholds (0.012%), while Li?O (0.55%) and Rb?O (0.24%) reach cutoff grades; (2) IP sounding reveals spatial correlation between deep high-resistivity anomalies (4,684 Ω·m) and low polarization rates (1.28%), with 3D inversion demonstrating NE-dipping extensions exceeding 800m depth, establishing a geometrically constrained mineralization model of 2.28 million m3 volume; (3) Resource estimates for the No.3 vein yield 35,000 tonnes Li?O and 15,000 tonnes Rb?O, with 1,981 tonnes Ta?O? and 1,086 tonnes Nb?O? metal content, confi rming large-scale rare metal deposit potential. The developed geology-geophysics collaborative exploration framework establishes a paradigm for rare metal prospecting in collisional orogenic belts.
Key wordsYidun Island Arc    Rare metals    Geophysical exploration    Geological mineral exploration   
收稿日期: 2025-01-07;
基金资助:四川省科技厅科研项目(2024NSFSC0093)、四川省地质调查研究院科研项目(SCIGS-CZDZX-2024001)、“稀有稀土战略资源评价与利用四川省重点实验室”联合资助。
通讯作者: 刘前坤 (Email: 623014947@qq.com ); 郝雪峰 (Email:hao-xuefeng@qq.com).     E-mail: 623014947@qq.com;hao-xuefeng@qq.com
作者简介: Yang Rong, male, graduated with a bachelor's degree in Applied Geophysics from Chengdu University of Technology in 2000 and obtained a master's degree from Chengdu University of Technology in 2012. Currently, he works at Sichuan Institute of Comprehensive Geological Survey, mainly engaged in geophysical exploration, geochemical exploration, software and information technology. E-mail: 30376331@qq.com.
引用本文:   
. 川西义敦岛弧海子山哈嘎拉岩体稀有金属地质-地球物理勘查研究[J]. 应用地球物理, 2025, 22(4): 1284-1296.
. Integrated Geology-Geophysics Exploration of Rare Metal Deposits in the Yidun Island Arc Collisional Orogen[J]. APPLIED GEOPHYSICS, 2025, 22(4): 1284-1296.
 
没有本文参考文献
[1] 宋滔, 刘云, 王赟, 李斌. 直流电阻率法和时间域激发极化法各向异性反常现象数值模拟[J]. 应用地球物理, 2021, 18(1): 117-127.
版权所有 © 2011 应用地球物理
技术支持 北京玛格泰克科技发展有限公司