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甘肃北贵多金属矿成矿地质特征及成因分析

王鹏祥

世界有色金属Issue(13):76-78,3.
世界有色金属Issue(13):76-78,3.

甘肃北贵多金属矿成矿地质特征及成因分析

Geological characteristics and genesis analysis of precious polymetallic deposits in northern Gansu Province

王鹏祥1

作者信息

  • 1. 甘肃煤田地质局一四九队,甘肃 兰州 730000
  • 折叠

摘要

Abstract

Through comprehensive geological surveys and data analysis,it is known that the ore-forming geological characteristics and genesis of polymetallic deposits in the northern Guizhou region of Gansu Province can provide reliable basis for mineral resource development.The mineral deposits in this area are mainly distributed in the Red Liuyuan Formation of the Middle Carboniferous and the late Variscan intrusive rocks,and are controlled by significant regional faults and their secondary faults.In addition,the formation of mineral deposits is closely related to magmatic activity and hydrothermal flow.This article further identifies a series of clear prospecting indicators,including surrounding rock types,structural features,magmatic rock features,geochemical anomalies,and alteration features,providing important scientific guidance for future exploration activities.

关键词

多金属矿/地质特征/成因

Key words

polymetallic ore/Geological features/origin

分类

天文与地球科学

引用本文复制引用

王鹏祥..甘肃北贵多金属矿成矿地质特征及成因分析[J].世界有色金属,2024,(13):76-78,3.

世界有色金属

1002-5065

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