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河西走廊成矿带区域成矿规律及找矿方向

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赵国斌, 杨合群, 余吉远, 谭文娟, 赵民, 余超, 朱永新, 艾宁, 向连格. 2023. 河西走廊成矿带区域成矿规律及找矿方向[J]. 地球学报, 44(4): 660-672. doi: 10.3975/cagsb.2022.101702
引用本文: 赵国斌, 杨合群, 余吉远, 谭文娟, 赵民, 余超, 朱永新, 艾宁, 向连格. 2023. 河西走廊成矿带区域成矿规律及找矿方向[J]. 地球学报, 44(4): 660-672. doi: 10.3975/cagsb.2022.101702
shu
ZHAO Guo-bin, YANG He-qun, YU Ji-yuan, TAN Wen-juan, ZHAO Min, YU Chao, ZHU Yong-xin, AI Ning, XIANG Lian-ge. 2023. Metallogenic Regularity and Prospecting Direction in the Hexi Corridor Metallogenic Belt, China. Acta Geoscientica Sinica, 44(4): 660-672. doi: 10.3975/cagsb.2022.101702
Citation: ZHAO Guo-bin, YANG He-qun, YU Ji-yuan, TAN Wen-juan, ZHAO Min, YU Chao, ZHU Yong-xin, AI Ning, XIANG Lian-ge. 2023. Metallogenic Regularity and Prospecting Direction in the Hexi Corridor Metallogenic Belt, China. Acta Geoscientica Sinica, 44(4): 660-672. doi: 10.3975/cagsb.2022.101702
shu

河西走廊成矿带区域成矿规律及找矿方向

  • 1. 中国地质调查局西安地质调查中心, 陕西西安 710054;

  • 2. 甘肃省地质调查院, 甘肃兰州 730000;

  • 3. 宁夏回族自治区地质调查院, 宁夏银川 750021

  • 基金项目:

    本文由中国地质调查局项目“中国矿产地质志”(编号: DD20221695

    DD20190379

    DD20160346)和“祁连-秦岭铜镍钴金战略性矿产调查评价”项目(编号: DD20230334)联合资助

详细信息
    作者简介: 赵国斌, 男, 1978 年生。硕士, 正高级工程师。主要从事成矿规律及矿产预测研究。E-mail: 531522461@qq.com

  • 中图分类号: P612

Metallogenic Regularity and Prospecting Direction in the Hexi Corridor Metallogenic Belt, China

  • 1. Xi’an Center, China Geological Survey, Xi’an, Shaanxi 710054;

  • 2. Geological Survey of Gansu Province, Lanzhou, Gansu 730000;

  • 3. Geological Survey Institute of Ningxia Hui Autonomous Region, Yinchuan, Ningxia 750021

    摘要
  • 河西走廊成矿带是分布于祁连地区最北部的Ⅲ级成矿单元(全国统一编号为Ⅲ-20), 目前共有235处矿产地, 形成了石油、煤、凹凸棒石黏土、萤石、石膏、芒硝、石灰岩、天然石英砂、铁、铜、金、钨等40 余种矿产。该成矿带以沉积成矿作用为主, 其次为流体、岩浆、变质和表生成矿作用, 可分为11 种矿床类型, 主要成矿期为华力西期、加里东期、燕山期和喜马拉雅期。河西走廊成矿带可进一步划分为2 个成矿亚带, 分别为玉门—民乐成矿亚带和山丹—中卫—泾源成矿亚带。根据构造空间、成矿时间、成矿作用和矿种等四要素的耦合关系, 河西走廊成矿带厘定了10 个矿床成矿系列, 包括4 个沉积作用有关矿床成矿系列、3 个流体作用有关矿床成矿系列、1 个岩浆作用有关矿床成矿系列、1 个变质作用有关矿床成矿系列和1 个表生作用有关矿床成矿系列。通过细分成矿时段和细化成矿地质作用, 进一步解析出16 个矿床成矿亚系列, 并建立了47 个矿床式。根据区内地质、矿产、物探、化探和遥感信息, 河西走廊成矿带共圈出5 个综合预测区, 为下一步找矿工作指出了方向。
    The Hexi corridor metallogenic belt is a III-level metallogenic unit distributed in the north of the Qilian region (national number III-20).There are 235 mineral deposits in this metallogenic belt, comprising more than 40 types of minerals, including petroleum, coal, attapulgite clay, fluorite, gypsum, mirabilite, limestone, quartz sand, iron, copper, gold, and tungsten.The major mineralization process is sedimentation, followed by hydrothermalism, magmatism, metamorphism, and supergenesis.These deposits can be divided into 11 types, and the main metallogenic periods are Variscan, Caledonian, Yanshanian, and Himalayan.This metallogenic belt can be further divided into two metallogenic sub-belts: Yumen-Minle and Shandan-Zhongwei-Jingyuan.According to the coupling relationship of the four elements of tectonic space, metallogenic time, mineralization, and mineral species, 10 minerogenetic series of mineral deposits have been determined in the Hexi corridor metallogenic belt, including four minerogenetic series of mineral deposits related to sedimentation, three minerogenetic series of mineral deposits related to hydrothermalism, one minerogenetic series of mineral deposits related to magmatism, one minerogenetic series of mineral deposits related to metamorphism, and one minerogenetic series of mineral deposits related to supergenesis.By subdividing metallogenic periods and mineralization, 16 minerogenetic subseries of mineral deposits and 47 deposit types were established.Based on the geological, mineral, geophysical, geochemical, and remote sensing information, five comprehensive prediction areas were delineated in the Hexi corridor metallogenic belt, which provide a direction for future prospecting work.
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