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特提斯构造域西段晚白垩世以来Cu、Au矿床时空分布和成矿地质特征

刘金龙 周永恒 姜平 李伫民 贺俊庆 王卓 吴涛涛

地球学报2026,Vol.47Issue(3):507-526,20.
地球学报2026,Vol.47Issue(3):507-526,20.DOI:10.3975/cagsb.2026.031201

特提斯构造域西段晚白垩世以来Cu、Au矿床时空分布和成矿地质特征

Spatiotemporal Distribution and Metallogenic Characteristics of Cu and Au deposits in the Western Segment of the Tethyan Tectonic Domain since Late Cretaceous

刘金龙 1周永恒 1姜平 2李伫民 1贺俊庆 1王卓 1吴涛涛1

作者信息

  • 1. 中国地质调查局沈阳地质调查中心,辽宁 沈阳 110000
  • 2. 中国地质调查局哈尔滨自然资源综合调查中心,黑龙江 哈尔滨 150081
  • 折叠

摘要

Abstract

The complex tectonic evolutionary history of the western segment of the Tethyan Orogenic Belt(zone)has made it an important Cu and Au polymetallic mineralization belts.In-depth research on the mineralization process and summarizing the mineralization laws in this area is scientifically important for enhancing the level of basic regional geological research and guiding mineral exploration practices.Regional geological and mineral resource data were systematically collected and comprehensively analyzed,focusing on elucidating the metallogenic characteristics,resource endowment conditions,spatiotemporal distribution patterns of deposits,and their tectonic-magmatic metallogenic contexts.Since the Late Cretaceous,the study area has undergone multiple tectonic-magmatic events,including oceanic and continental subduction,orogeny,back-arc extension,slab rollback and tearing,and asthenospheric upwelling.These dynamic mechanisms collectively control large-scale regional Cu-Au mineralization.To date,the area has revealed 39 large to super-large Cu-Au deposits and 31 medium-sized deposits,with numerous small deposits and widely distributed mineral occurrences,demonstrating substantial metallogenic potential.The regional deposits exhibited distinct spatiotemporal patterns.Cu-Au mineralization can be classified into the Late Cretaceous Apuseni-Banat-Timok-Srednogorie Cu-Au Belt(93-72 Ma),Late Cretaceous-Paleocene East Pontides Cu-Au Belt(88-59 Ma),Late Cretaceous East Tauride Cu Belt(81-71 Ma),Eocene Southeastern Anatolian Cu-Au Belt(54-37 Ma),Eocene-Pliocene North Macedonia-Rhodope-North Aegean Au-Cu Belt(50-3 Ma),Oligocene Tunceli Cu-Au Zone(~26 Ma),and Miocene Carpathians-Alpine Cu-Au Zone(15-8 Ma).

关键词

地质背景/特提斯构造域西段/成矿规律/地质调查工程

Key words

geological setting/western segment of Tethyan tectonic domain/metallogenic regularity/geological survey project

分类

天文与地球科学

引用本文复制引用

刘金龙,周永恒,姜平,李伫民,贺俊庆,王卓,吴涛涛..特提斯构造域西段晚白垩世以来Cu、Au矿床时空分布和成矿地质特征[J].地球学报,2026,47(3):507-526,20.

基金项目

本文由中国地质调查局项目(编 号:DD202309008)和云南铜业股份有限公司"东北亚铜金矿项目优选与评价"项目(编号:YNTY-KSB-08-2025-035)联合资助. This study was supported by China Geological Survey(No.DDDD202309008),and Yunnan Copper Co.,Ltd.(No.YNTY-KSB-08-2025-035). (编 号:DD202309008)

地球学报

1006-3021

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