|Table of Contents|

Characteristics and Metallogeny of Triassic Polymetallic Mineralization in Xicheng and Fengtai Ore Cluster Zones, West Qinling, China and Their Implications for Prospecting Targets(PDF)

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

Issue:
2021年第03期
Page:
409-435
Research Field:
院士专稿
Publishing date:

Info

Title:
Characteristics and Metallogeny of Triassic Polymetallic Mineralization in Xicheng and Fengtai Ore Cluster Zones, West Qinling, China and Their Implications for Prospecting Targets
Author(s):
WANG Yi-tian*;  MAO Jing-wen**;  HU Qiao-qing;  WEI Ran;  CHEN Shao-cong
(MNR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China)
Keywords:
Triassic;  polymetallic mineralization;  ore-forming regularity;  prospecting target;  Xicheng ore cluster zone;  Fengtai ore cluster zone;  West Qinling
PACS:
P612; P617
DOI:
10.19814/j.jese.2021.02014
Abstract:
In recent a dozen years, the mineral exploration, research on mineralization and precise measurement of isotopic age have been carried out continuously in West Qinling, which have achieved a lot of new discoveries in exploration and some new understandings of metallogeny. Especially, a quantity of high accuracy isotopic age data of igneous rocks and polymetallic mineralization, have gradually uncovered the veil of Triassic polymetallic mineralization in West Qinling, showing the universality and diversity of Triassic mineralization, and indicating the huge metallogenic potential. Xicheng and Fengtai ore cluster zones, located in the eastern part of West Qinling, where the predominant Triassic minerals of Pb-Zn, Au, Ag and Cu are well developed with lesser minerals of W, Mo and Fe; and Pb-Zn and Au are the superior mineral resources in the ore cluster zones. The latest research achivements show that the ages of the polymetallic deposits in the area range from 231 Ma to 197 Ma, concentrated in 220-200 Ma; the ages of magmatic rocks range from 248 Ma to 195 Ma, concentrated in 230-200 Ma. The polymetallic mineralization and magmatic activity are temporal coupling with the peak of 220-210 Ma. The main types of polymetallic deposits include the hydrothermal filling and replacing ore deposits related to the magmatic activity and metamorphism, the porphyry, skarn and greisen ore deposits associated with magmatic-hydrothermal mineralization system. The tectonic activity and its product are the dominant ore-controlling factors of polymetallic mineralization, and the structures of the various types and different scales directly control the occurrence, form, attitude and size of the orebodies. The polymetallic mineralization in the area developes in the post-collision stage of Indosinian orogenic process in Qinling orogeny, which is the product of the extensive and intense coupling process of deformation and metamorphism, magmatic activity and fluid flow in Late Triassic. Based on the metallogenic geological conditions, mineralization characteristics, ore genesis, ore-controlling factors and ore-forming regularities, some further prospecting targets are suggested preliminarily to promote the prospecting and exploration works at depth in this area to make new achievements.

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Last Update: 2021-05-01