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山东蓬莱金矿黄铁矿成分环带的成因及成矿意义
引用本文:杨进辉, 马红梅, 周新华, 冯本智. 山东蓬莱金矿黄铁矿成分环带的成因及成矿意义[J]. 地质科学, 2000, 35(2): 168-174.
作者姓名:杨进辉  马红梅  周新华  冯本智
作者单位:1. 中国科学院地质研究所 北京 100029; 2. 北京敬业电工集团 北京 100800; 3. 长春科技大学 长春 130061
基金项目:国家科技部九五攀登预选项目!(编号 :95-预 -2 5)
摘    要:蓬莱金矿位于胶东半岛北部,是一个中型热液型脉状金矿。利用分析型高分辨电子显微镜(JEM-2000FX)并配以能谱仪(EDS)对主要的载金矿物黄铁矿进行微区分析,发现成矿阶段黄铁矿晶体内部Fe、S等成分呈环带状分布。本文从耗散结构理论出发,初步探讨黄铁矿内部成分环带的成因,并论述了它的成矿意义。

关 键 词:黄铁矿   成分环带   耗散结构   成矿意义   山东蓬莱金矿
收稿时间:1998-09-23
修稿时间:1998-09-23

GENESIS AND SIGNIFICANCE OF COMPONENT ZONES IN PYRITES FROM PENGLAI GOLD DEPOSIT, SHANDONG PROVINCE
Yang Jinhui, Ma Hongmei, Zhou Xinhua, Feng Benzhi. GENESIS AND SIGNIFICANCE OF COMPONENT ZONES IN PYRITES FROM PENGLAI GOLD DEPOSIT, SHANDONG PROVINCE[J]. Chinese Journal of Geology, 2000, 35(2): 168-174.
Authors:Yang Jinhui  Ma Hongmei  Zhou Xinhua  Feng Benzhi
Affiliation:1. Institute of Geology, Chinese Academy of Sciences, Beijing 100029; 2. Beijing Electric Engineering Group Corporation, Beijing 100800; 3. Changchun University of Science and Technology, Changchun 130061
Abstract:The Penglai gold deposit, located in the northern part of Jiaodong Penisula, is a middle, hydrothermal lode type deposit. It is along the outside contact zone of the Guojialing granodiorite. The Au carrying minerals are pyrite, quartz, chalcopyrite, galena, pyrrhotite and sphalerite, in which pyrite and quartz are the main Au carrying minerals. Microinformation of pyrites at different stages studied by electronic microscope(JEF 2000FX) equipped with spectrum(EDS) shows that there exit component zones in pyrites at syn gold mineralization stage stage. Based on dissipative structure, we discuss the dynamic genesis of component zones in pyrites at syn gold mineralization stage, and give a suggestion about the geological setting and the process of gold mineralization in Penglai gold deposit, Shandong.
Keywords:Pyrite   Component zones   Dissipative structure   Gold mineralization   Penglai gold deposit   Shandong Province
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