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矿床成矿系列——五论矿床的成矿系列问题
引用本文:陈毓川,裴荣富,王登红,黄凡.矿床成矿系列——五论矿床的成矿系列问题[J].地球学报,2016,37(5):519-527.
作者姓名:陈毓川  裴荣富  王登红  黄凡
作者单位:中国地质科学院,中国地质科学院矿产资源研究所 国土资源部成矿作用与资源评价重点实验室,中国地质科学院矿产资源研究所 国土资源部成矿作用与资源评价重点实验室,中国地质科学院矿产资源研究所 国土资源部成矿作用与资源评价重点实验室
基金项目:中国地质调查局中国矿产地质与成矿规律综合集成和服务(矿产地质志)项目(编号: DD20160346)
摘    要:矿床的成矿系列(简称成矿系列)是矿床学领域的一个理论性概念,由五级序次组成。矿床成矿系列是成矿系列的第二序次,是成矿系列的核心部分。矿床成矿系列的划分,以岩浆、沉积、变质、表生和流体(非岩浆-非变质成因流体)5种成矿作用为基本原则,以成矿地质环境为基础,结合成矿的时段与形成的矿床组合进行划分。本文对矿床成矿系列时空范围、时空组成结构、矿化强度与演化、成矿区带内不同矿床成矿系列之间的演化、叠加和复合作用及对指导找矿的意义进行了论述。

关 键 词:矿床成矿系列概念    划分原则    时空圈定    组成与演化    找矿意义

Minerogenetic Series for Mineral Deposits:Discussion on Minerogenetic Series (V)
CHEN Yu-chuan,PEI Rong-fu,WANG Deng-hong and HUANG Fan.Minerogenetic Series for Mineral Deposits:Discussion on Minerogenetic Series (V)[J].Acta Geoscientia Sinica,2016,37(5):519-527.
Authors:CHEN Yu-chuan  PEI Rong-fu  WANG Deng-hong and HUANG Fan
Institution:Chinese Academy of Geological Sciences,MLR Key Laboratory of Metallogeny and Mineral Resources Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences,MLR Key Laboratory of Metallogeny and Mineral Resources Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences and MLR Key Laboratory of Metallogeny and Mineral Resources Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences
Abstract:Minerogenetic series of mineral deposits (metallogenic series for short) is a theoretical concept in the field of mineral deposits, which can be divided into five orders by ore-forming sequence. As the second order, minergenetic series for mineral deposits serves as the core of the components of minerogenetic series. According to the mineralization of magma, sedimentation, metamorphism, supergene and non-magmatic and non-metamorphic ore forming fluid, minero-genetic series for mineral deposits can be divided based on metallogenic geological environment in combination with the ore-forming period and the existence of deposit combinations. In this paper, the spatial-temporal range, composition structure, mineralization intensity and evolution of minerogenetic series for mineral deposits as well as the evolution, superposition and recombination between different metallogenic series for mineral deposits and their significance for guiding prospecting are discussed.
Keywords:concept of minerogenetic series for mineral deposits  classification principles  spatial-temporal  delineation  composition and evolution  prospecting significance
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