矿床地质:2020,Vol.>>Issue(1):19-41

斑岩型矿床容矿裂隙成因的几种概念模型及其意义
云南地矿国际矿业股份有限公司, 云南 昆明 650051;云南省地质矿产勘查院, 云南 昆明 650051,北京师范大学信息科学与技术学院, 北京 100875,云南省国土资源厅, 云南 昆明 650224,云南地矿国际矿业股份有限公司, 云南 昆明 650051,云南地矿国际矿业股份有限公司, 云南 昆明 650051,云南省地质科学研究所, 云南 昆明 650051,云南国土资源职业学院, 云南 昆明 652501,云南地矿国际矿业股份有限公司, 云南 昆明 650051,云南地矿国际矿业股份有限公司, 云南 昆明 650051,云南地矿国际矿业股份有限公司, 云南 昆明 650051,香格里拉市宝峰矿业有限责任公司, 云南 香格里拉 674400
Conceptual model for genesis of mineralized fissures in porphyry deposits and its geological significance
ZHAO MaoChun,YU XianChuan,ZHANG YiFei,WANG YaWei,HE Yun,SU TaiMin,YAO JinChang,TANG Qiong,LIU ShiJun,ZHAO SiChuan,LI ShiLei
(Yunnan Geology and Mining International Mining Industry Co., Ltd., Kunming 650051, Yunnan, China;Yunnan Exploration Institute of Geology&Mineral Resources, Kunming 650051, Yunnan, China;College of Information Science and Technology, Beijing Normal University, Beijing 100875, China;Department of Land and Resources of Yunnan Province, Kunming 650224, Yunnan, China;Yunnan Institute of Geological Science, Kunming 650051, Yunnan, China;Yunnan Land and Resources Vocational College, Kunming 652501, Yunnan, China;Shangri-la Baofeng Mining Co., Ltd., Shangri-la 674400, Yunnan, China)
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投稿时间:2018-12-13   修订日期:2019-07-16      网络发布日期:2020-02-26
中文摘要:斑岩型矿床对成矿的围岩没有选择性,但斑岩型矿床的网状裂隙系统控制了矿体的分布、矿石的品位和组构变化、矿化蚀变等特征,因此对容矿裂隙的形成机制、控制因素、裂隙分布规律等开展研究有着重要意义。文章探讨了斑岩在侵位、冷却、结晶演化过程中,在岩体及其围岩中形成网状裂隙系统的相关机制及其制约因素,将斑岩型矿床容矿裂隙的成因归纳为岩浆结晶冷缩、侵入挤压、水岩分离和区域应力叠加等4种主要成因类型,并构建了它们的概念模型。这些裂隙成因概念模型较好地反映了不同成因的裂隙系统与斑岩侵入体的空间依存关系、裂隙的分布特征及裂隙率的变化规律,以及它们之间的差异;较好地解释了斑岩型矿床的成矿作用特点及其共性特征。在分析典型斑岩型矿床容矿裂隙成因的基础上,提出了将概念模型应用于斑岩型矿床勘查找矿的思路。
Abstract:Porphyry deposits do not choose their mineralized host rocks, but the distribution of the orebody, the grade and composition of the ore, and the mineralization-alteration characteristics are controlled by the extensively developed reticular fracturing system of the porphyry deposit. Therefore, the study of the formation mechanism, controlling factors and fractures distribution of the ore-bearing fractures is of great importance. In this paper, the mechanism concerning the reticular fracturing system formation in the porphyry rock mass and its surrounding rocks during the emplacement, cooling and crystallization evolution of porphyry rock mass is discussed. Further more, the genesis of the fracturing is divided into four main types:magma crystallization shrinkage, magmatic intrusion extrusion, water-rock separation, and regional stress superposition, and their conceptual models are constructed. These conceptual models for fracturing genesis can better reflect the spatial dependence of different genetic fractures and porphyry intrusions, the distribution characteristics and the variation of fracture rates of fractures, and the differences between them; in addition, they can better explain the distinct porphyry mineralization characteristics and common characteristics of ore deposits. Based on an analysis of the genesis of the ore-bearing fractures in typical porphyry deposits, the authors put forward the idea of applying the conceptual model to the exploration of porphyry deposits.
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基金项目:本文得到国家自然科学基金(编号:41672323)、国土资源部公益基金(编号:201511079-02)和中国地质调查局发展研究中心公益基金(编号:DD20190166-04)共同资助
引用文本:
赵茂春,余先川,张翼飞,王亚伟,何云,苏泰民,姚金昌,唐琼,刘仕军,赵思传,李石磊.2020.斑岩型矿床容矿裂隙成因的几种概念模型及其意义[J].矿床地质,39(1):19~41
ZHAO MaoChun,YU XianChuan,ZHANG YiFei,WANG YaWei,HE Yun,SU TaiMin,YAO JinChang,TANG Qiong,LIU ShiJun,ZHAO SiChuan,LI ShiLei.2020.Conceptual model for genesis of mineralized fissures in porphyry deposits and its geological significance[J].Mineral Deposits39(1):19~41
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