山西辛庄金矿床地质地球化学特征及成因研究
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摘要
山西辛庄金矿床位于华北克拉通中间带北部,山西陆台五台隆起西北侧与燕山沉降带西南缘两大构造单元相互嵌接的中生代构造岩浆活动带上,是中生代构造岩浆岩活化地区。本文系统总结了辛庄金矿床的区域成矿背景、矿床地质特征、矿床地球化学特征以及成矿流体特征,在此基础上,以金矿床成因理论为依据,开展了辛庄金矿床成矿期次、成矿地质条件、控矿因素、矿化标志、成矿规律以及矿床成因等方面的研究,取得的成果和创新点主要有以下几点：
(1)依据野外宏观地质特征和显微镜下矿物微观特征,分析了矿物共生组合规律,划分了辛庄金矿床的成矿期次。
(2)首次通过系统研究成矿岩体的地质地球化学特征,探讨了本区岩浆来源、成岩环境以及成岩机制,得出岩石属典型S型花岗岩,具明显富硅富钾富碱的特征；岩浆起源于地壳物质的重熔,形成环境为造山带环境,在岩体形成过程中岩浆演化经历了部分熔融和较强的分离结晶作用。
(3)运用电子探针测试手段,对金属硫化物矿物标型特征进行了研究,认为本区金属硫化物为岩浆热液成因。
(4)通过同位素以及流体包裹体特征分析,探讨了成矿物质及成矿流体来源,指出成矿物质主要来源于燕山期岩浆：成矿流体主要为岩浆水,后期有大气降水的加入,为中高温、中低盐度、中等密度流体。
(5)在综合分析矿床地质特征及矿床地球化学特征的基础上,分析其矿床成因属与燕山期岩浆侵入活动有关的中温热液石英脉型金矿床,并建立了成矿模式。
(6)系统分析了地层、构造和岩浆岩与成矿的关系,总结了关键控矿因素,总结了矿化富集标志和成矿定位规律。
Xinzhuang gold deposit is located in the northern part of the North China Craton intermediate belt, and in a Mesozoic tectonic-magma activation area which is embedded by the two tectonic units-the northwestern Wutai uplifts of Shanxi platform and the southwestern Yanshanian subsidence belt. The regional metallogenic background, geological characteristics of ore deposits, geochemical characteristics and ore-forming fluid features of the Xinzhuang Gold Deposit were systematically summarized. Based on these and according to for the theory of gold deposit genesis, the minerlization stages, ore-forming geological conditions, ore-controlling factors, mineralization mark, metallogenic controls and metallogeny of Xinzhuang Gold Deposit were researched. The main achievements are as follows:
(1) Mineral assemblage regularity was analyzed based on the microscopic characteristics of the minerals under the microscope and field macro-geological characteristics. And mineralization stages were divided of Xinzhuang gold deposit.
(2) The geological and geochemical characteristics were studied for the first time, based on the geological characteristics of ore-forming rock body, petrological characteristics and geochemical characteristics. The results are show that the rock is typical S type granite with obvious silica-rich potassium rich alkali-rich characteristics, magma originated from the remelting crustal material and the environment is orogenic environment, magma evolution experienced partial melting and fractional crystallization during the rock formation process.
(3) The causes of metal sulfides were studied for the first time based on the metal sulfides chemical composition by EPMA. The results are showed that metal sulfides are hydrothermal origin.
(4) The ore-forming material source and ore-forming fluid source were studied for the first time based on isotope characteristics and fluid inclusion characteristics. The results are showed that ore-forming material originated from Yanshanian magmatic activity, ore-forming fluid is mainly magmatic water and later joined the meteoric water, with medium-high temperature, medium-low salinity and medium density.
(5) Ore genesis was analyzed on the basis of geological characteristics and geochemical characteristics of the ore deposi. The ore genesis of Xinzhuang Gold Deposit is Mesothermal quartz vein type, related to the Yanshanian mediosilicicacid magma intrusion activities. The metallogenic model was established for the first time of Xinzhuang gold deposit, based on summarizing ore-forming geological elements.
(6) The relationship with mineralization between Stratigraphy, structure and magmatic rock were analyzed, and the ore-forming geological conditions were summarized. The ore-forming location rule and mineralization enrichment markers were summarized.
(1)依据野外宏观地质特征和显微镜下矿物微观特征,分析了矿物共生组合规律,划分了辛庄金矿床的成矿期次。
(2)首次通过系统研究成矿岩体的地质地球化学特征,探讨了本区岩浆来源、成岩环境以及成岩机制,得出岩石属典型S型花岗岩,具明显富硅富钾富碱的特征；岩浆起源于地壳物质的重熔,形成环境为造山带环境,在岩体形成过程中岩浆演化经历了部分熔融和较强的分离结晶作用。
(3)运用电子探针测试手段,对金属硫化物矿物标型特征进行了研究,认为本区金属硫化物为岩浆热液成因。
(4)通过同位素以及流体包裹体特征分析,探讨了成矿物质及成矿流体来源,指出成矿物质主要来源于燕山期岩浆：成矿流体主要为岩浆水,后期有大气降水的加入,为中高温、中低盐度、中等密度流体。
(5)在综合分析矿床地质特征及矿床地球化学特征的基础上,分析其矿床成因属与燕山期岩浆侵入活动有关的中温热液石英脉型金矿床,并建立了成矿模式。
(6)系统分析了地层、构造和岩浆岩与成矿的关系,总结了关键控矿因素,总结了矿化富集标志和成矿定位规律。
Xinzhuang gold deposit is located in the northern part of the North China Craton intermediate belt, and in a Mesozoic tectonic-magma activation area which is embedded by the two tectonic units-the northwestern Wutai uplifts of Shanxi platform and the southwestern Yanshanian subsidence belt. The regional metallogenic background, geological characteristics of ore deposits, geochemical characteristics and ore-forming fluid features of the Xinzhuang Gold Deposit were systematically summarized. Based on these and according to for the theory of gold deposit genesis, the minerlization stages, ore-forming geological conditions, ore-controlling factors, mineralization mark, metallogenic controls and metallogeny of Xinzhuang Gold Deposit were researched. The main achievements are as follows:
(1) Mineral assemblage regularity was analyzed based on the microscopic characteristics of the minerals under the microscope and field macro-geological characteristics. And mineralization stages were divided of Xinzhuang gold deposit.
(2) The geological and geochemical characteristics were studied for the first time, based on the geological characteristics of ore-forming rock body, petrological characteristics and geochemical characteristics. The results are show that the rock is typical S type granite with obvious silica-rich potassium rich alkali-rich characteristics, magma originated from the remelting crustal material and the environment is orogenic environment, magma evolution experienced partial melting and fractional crystallization during the rock formation process.
(3) The causes of metal sulfides were studied for the first time based on the metal sulfides chemical composition by EPMA. The results are showed that metal sulfides are hydrothermal origin.
(4) The ore-forming material source and ore-forming fluid source were studied for the first time based on isotope characteristics and fluid inclusion characteristics. The results are showed that ore-forming material originated from Yanshanian magmatic activity, ore-forming fluid is mainly magmatic water and later joined the meteoric water, with medium-high temperature, medium-low salinity and medium density.
(5) Ore genesis was analyzed on the basis of geological characteristics and geochemical characteristics of the ore deposi. The ore genesis of Xinzhuang Gold Deposit is Mesothermal quartz vein type, related to the Yanshanian mediosilicicacid magma intrusion activities. The metallogenic model was established for the first time of Xinzhuang gold deposit, based on summarizing ore-forming geological elements.
(6) The relationship with mineralization between Stratigraphy, structure and magmatic rock were analyzed, and the ore-forming geological conditions were summarized. The ore-forming location rule and mineralization enrichment markers were summarized.
引文
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