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安徽芜湖黄浒膨润土矿床地质特征及其成因分析

方翔宇 杨傲 张奥 潘祯 李军如 曹达旺

安徽地质2024,Vol.34Issue(2):111-114,4.
安徽地质2024,Vol.34Issue(2):111-114,4.

安徽芜湖黄浒膨润土矿床地质特征及其成因分析

Geological characteristics and genetic analysis of the Huanghu bentonite deposit in Wuhu,Anhui

方翔宇 1杨傲 1张奥 1潘祯 1李军如 1曹达旺1

作者信息

  • 1. 安徽省核工业勘查技术总院,安徽芜湖 241002
  • 折叠

摘要

Abstract

Focusing on the ore body I of the Huanghu bentonite deposit,this paper has conducted geological surveying,drilling,chemical testing and software simulation to analyze the ore-controlling geological conditions and their characteristics.The results indicate that this is a volcanic sedimentary bentonite deposit formed by low-temperature hydrothermal alteration and supergene oxidation on the basis of the primary rocks of andesitic brecciated tuff and andesitic brecciated lava of the Cretaceous Kedoushan Formation.This study provides a train of thought and experience for search of volcanic sedimentary bentonite deposits in the future.

关键词

黄浒膨润土矿/地质特征/矿床成因/火山沉积型

Key words

the Huanghu bentonite deposit/geological characteristics/genesis of ore deposit/volcanic sedimentary type

分类

天文与地球科学

引用本文复制引用

方翔宇,杨傲,张奥,潘祯,李军如,曹达旺..安徽芜湖黄浒膨润土矿床地质特征及其成因分析[J].安徽地质,2024,34(2):111-114,4.

安徽地质

1005-6157

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