广西寒武系地层建造边缘铅锌矿床成矿构造岩相特征及其找矿意义

P612%P618.4; 广西寒武系地层建造边缘铅锌矿床主要分布于沉积不整合面之上古风化壳或碳酸盐岩建造中,呈浅成中-低温热液类型,具有多阶段成矿及围岩蚀变分带特征.通过成矿构造岩相特征分析,认为矿床成矿建造以碳酸盐岩地层有利岩性、层间滑脱面或层间破碎带叠加区域大断裂为主,控制着层状矿体空间分布,古风化壳层、区域大断裂伴生的次级断裂次之,控制着脉状矿体的空间分布.成矿物质主要来源于生物碎屑岩中的元素迁移.矿床围岩蚀变可划分为强蚀变岩带和弱蚀变岩带,强蚀变岩带蚀变以黄铁矿化、毒砂矿化、硅化、白云岩化、方解石化为主,偶见重晶石化、绢云母化、铅锌矿化.弱蚀变岩带蚀变以黄铁矿化、毒砂化、方解石化为主,...

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Published in地质与勘探 Vol. 59; no. 5; pp. 946 - 960
Main Authors 周国发, 梁标志, 周伟金, 吕古贤, 韦安伟, 张培才, 王磊, 陈彪, 陆济璞, 肖昌浩
Format Journal Article
LanguageChinese
Published 广西地质矿产勘查开发局,广西南宁 530023%广西地质调查院,广西南宁 530023%中国地质科学院地质力学研究所动力成岩成矿实验室,北京 100081 01.09.2023
Subjects
prospecting indicators
浅成中-低温热液矿床
找矿标志
tectonic lithofacies
wall rock alteration
Guangxi
Cambrian stratigraphic formation
广西
hypabyssal medium-low temperature hydrothermal deposit
构造岩相
寒武系地层建造
围岩蚀变
Online AccessGet full text
ISSN0495-5331
DOI10.12134/j.dzykt.2023.05.003

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Abstract P612%P618.4; 广西寒武系地层建造边缘铅锌矿床主要分布于沉积不整合面之上古风化壳或碳酸盐岩建造中,呈浅成中-低温热液类型,具有多阶段成矿及围岩蚀变分带特征.通过成矿构造岩相特征分析,认为矿床成矿建造以碳酸盐岩地层有利岩性、层间滑脱面或层间破碎带叠加区域大断裂为主,控制着层状矿体空间分布,古风化壳层、区域大断裂伴生的次级断裂次之,控制着脉状矿体的空间分布.成矿物质主要来源于生物碎屑岩中的元素迁移.矿床围岩蚀变可划分为强蚀变岩带和弱蚀变岩带,强蚀变岩带蚀变以黄铁矿化、毒砂矿化、硅化、白云岩化、方解石化为主,偶见重晶石化、绢云母化、铅锌矿化.弱蚀变岩带蚀变以黄铁矿化、毒砂化、方解石化为主,偶见重晶石化.地质找矿标志为方解石脉、重晶石脉、蚀变岩带及古风化壳与断裂构造交汇部位.地球化学找矿标志为Pb、Zn、Cd、Hg、As、Ba等元素异常的出现.
AbstractList P612%P618.4; 广西寒武系地层建造边缘铅锌矿床主要分布于沉积不整合面之上古风化壳或碳酸盐岩建造中,呈浅成中-低温热液类型,具有多阶段成矿及围岩蚀变分带特征.通过成矿构造岩相特征分析,认为矿床成矿建造以碳酸盐岩地层有利岩性、层间滑脱面或层间破碎带叠加区域大断裂为主,控制着层状矿体空间分布,古风化壳层、区域大断裂伴生的次级断裂次之,控制着脉状矿体的空间分布.成矿物质主要来源于生物碎屑岩中的元素迁移.矿床围岩蚀变可划分为强蚀变岩带和弱蚀变岩带,强蚀变岩带蚀变以黄铁矿化、毒砂矿化、硅化、白云岩化、方解石化为主,偶见重晶石化、绢云母化、铅锌矿化.弱蚀变岩带蚀变以黄铁矿化、毒砂化、方解石化为主,偶见重晶石化.地质找矿标志为方解石脉、重晶石脉、蚀变岩带及古风化壳与断裂构造交汇部位.地球化学找矿标志为Pb、Zn、Cd、Hg、As、Ba等元素异常的出现.
Author 陈彪
王磊
吕古贤
梁标志
张培才
陆济璞
韦安伟
周国发
肖昌浩
周伟金
AuthorAffiliation 广西地质矿产勘查开发局,广西南宁 530023%广西地质调查院,广西南宁 530023%中国地质科学院地质力学研究所动力成岩成矿实验室,北京 100081
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Author_FL LIANG Biaozhi
LU Jipu
XIAO Changhao
WEI Anwei
ZHOU Guofa
Lü Guxian
ZHOU Weijin
ZHANG Peicai
WANG Lei
CHEN Biao
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DocumentTitle_FL Characteristics of Metallogenic Tectonic Lithofacies of Lead-Zinc Deposits on the Edge of Cambrian Stratigraphic Formation in Guangxi and Their Prospecting Significance
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Issue 5
Keywords prospecting indicators
浅成中-低温热液矿床
找矿标志
tectonic lithofacies
wall rock alteration
Guangxi
Cambrian stratigraphic formation
广西
hypabyssal medium-low temperature hydrothermal deposit
构造岩相
寒武系地层建造
围岩蚀变
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PublicationTitle 地质与勘探
PublicationTitle_FL Geology and Exploration
PublicationYear 2023
Publisher 广西地质矿产勘查开发局,广西南宁 530023%广西地质调查院,广西南宁 530023%中国地质科学院地质力学研究所动力成岩成矿实验室,北京 100081
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Snippet P612%P618.4; 广西寒武系地层建造边缘铅锌矿床主要分布于沉积不整合面之上古风化壳或碳酸盐岩建造中,呈浅成中-低温热液类型,具有多阶段成矿及围岩蚀变分带特征.通过成矿构...
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StartPage 946
Title 广西寒武系地层建造边缘铅锌矿床成矿构造岩相特征及其找矿意义
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