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

卷:

第46卷

期数:

2024年第01期

页码:

96-113

栏目:

基础地质与矿床地质

出版日期:

2024-01-15

文章信息/Info

Title:

Mineralization Series and Prospecting Direction of Salt and Groundwater Mineral Deposits in Qaidam Basin, China

文章编号:

1672-6561(2024)01-0096-18

作者:

潘 彤¹; 2; 贾建团²; 3*; 李东生²; 3; 郭廷峰¹; 李小龙³; 韩 光²; 3; 张晓冬²; 3; 张绍栋¹; 刘久波²; 3; 汪青川²; 3; 苗 青²; 3

(1. 青海省地质矿产勘查开发局,青海 西宁 810008; 2. 青海省柴达木盆地盐湖资源勘探研究重点实验室,青海 格尔木 816099; 3. 青海省柴达木综合地质矿产勘查院,青海 格尔木 816099)

Author(s):

PAN Tong¹; 2;  JIA Jian-tuan²; 3*;  LI Dong-sheng²; 3;  GUO Ting-feng¹;  LI Xiao-long³;  HAN Guang²; 3;  ZHANG Xiao-dong²; 3;  ZHANG Shao-dong¹;  LIU Jiu-bo²; 3;  WANG Qin

(1. Bureau of Geological Exploration & Development of Qinghai Province, Xining 810008, Qinghai, China; 2. Qinghai Provincial Key Laboratory of Exploration and Research of Salt Lake Resources in Qaidam Basin, Golmud 816099, Qinghai, China; 3. Qaidam Integrated Geological Exploration Institute of Qinghai Province, Golmud 816099, Qinghai, China)

关键词:

成矿系列;  找矿方向;  盐类矿产;  地下水;  成矿单元;  矿床类型;  矿产分布;  柴达木盆地

Keywords:

mineralization series;  prospecting direction;  salt mineral;  groundwater;  metallogenic unit;  deposit type;  mineral distribution;  Qaidam Basin

分类号:

P612

DOI:

10.19814/j.jese.2023.10007

文献标志码:

A

摘要:

新生代以来,柴达木盆地形成了复杂的构造体系及一系列相对独立的构造、成矿单元。柴达木盆地不同的构造单元因沉积环境与成矿条件的差异,在第四系浅层盐湖区、更新统冲洪积扇区、古近系—新近系圈闭构造区等特定的时空范围形成了赋存状态、矿物组合等相对独特的矿产。对柴达木盆地盐类及地下水资源时空分布特征、成矿作用及成矿地质背景进行了归纳研究,划分了盆地盐类及地下水矿床成矿系列。以成矿系列理论为指导,结合柴达木盆地最新的勘查研究成果,对盆地演化、盐类成矿单元、矿产时空分布及成矿类型等进行梳理,将柴达木盆地盐类及地下水矿床划分为3个成矿系列、6个成矿亚系列、15个矿床式。根据矿床自然分类及矿床成矿系列“全位成矿、缺位找矿”的预测思维,提出了柴达木盆地盐类及地下水矿产的找矿方向。

Abstract:

Since the Cenozoic, Qaidam Basin has developed a complex tectonic system and a series of relatively independent tectonic and metallogenic units. Within specific spatiotemporal ranges including the shallow salt lake area in Quaternary, the alluvial-proluvial fan area in Pleistocene, and the trap structural area of Paleogene-Neogene, the different tectonic units in Qaidam Basin have brought minerals with relatively unique occurrence statuses and mineral compositions because of variations in the sedimentary environment and metallogenic conditions. The inductive research on the spatiotemporal distribution characteristics, mineralization, and metallogenic geological background of basin salts and groundwater resources, along with the classification of metallogenic series for basin salt and groundwater mineral deposits, holds great significance in guiding future exploration, ore prospecting, and resource development and utilization, as well as ensuring the smooth construction of a world-class salt lake industrial base. Guided by the metallogenic series theory, the basin evolution, salt metallogenic units, spatiotemporal distribution of mineral resources, and metallogenic types are systematically collated based on the latest exploration and research findings on Qaidam Basin. As a result, the salt and groundwater mineral deposits in Qaidam Basin are classified into three metallogenic series, six metallogenic sub-series, and fifteen ore deposit types. Moreover, utilizing the natural classification of deposits and the predictive mindset of inevitable mineralization in certain spatiotemporal dimensions and prospecting/research of unexplored or unpredicted deposits, the effective prospecting directions for salt and groundwater mineral deposits in Qaidam Basin are presented.

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备注/Memo

备注/Memo:

收稿日期:2023-10-09; 修回日期:2023-12-29投稿网址:http:∥jese.chd.edu.cn/
基金项目:国家重点研发计划项目(2022YFC2904301); 青海省“昆仑英才·高端创新创业人才”计划项目
作者简介:潘 彤(1966-),男,青海乐都人,青海省地质矿产勘查开发局教授级高级工程师,博士研究生导师,理学博士,E-mail:pant66@163.com。
*通信作者:贾建团(1983-),男,甘肃通渭人,青海省柴达木综合地质矿产勘察院高级工程师,E-mail:czy@qhczy.cn。

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