Transactions of Nonferrous Metals Society of China The Chinese Journal of Nonferrous Metals

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中國有色金屬學報

ZHONGGUO YOUSEJINSHU XUEBAO

第22卷    第3期    總第156期    2012年3月

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文章編號:1004-0609(2012)03-0809-10
福建梅仙丁家山鉛鋅礦成礦系統(tǒng)分析
石得鳳1, 2,張術(shù)根1, 2,韓世禮1, 2,艾國梁1, 2

(1. 中南大學 有色金屬成礦預測教育部重點實驗室,長沙 410083;
2. 中南大學 地球科學與信息物理學院,長沙 410083
)

摘 要: 通過對丁家山鉛鋅礦成礦時代、成礦物質(zhì)來源、成礦流體通道、儲礦場等成礦系統(tǒng)要素的全面分析,明確了丁家山鉛鋅礦區(qū)成礦作用為燕山期花崗質(zhì)巖漿與經(jīng)加里東期區(qū)域變質(zhì)的新元古界馬面山群龍北溪組上段富鈣質(zhì)巖之間的接觸交代變質(zhì)作用。Pb和S等同位素研究及化探掃面結(jié)果顯示:礦區(qū)成礦物質(zhì)由燕山期花崗巖和馬面山群龍北溪組地層共同提供,H和O同位素研究證實:成礦流體由大氣降水和巖漿水共同組成;精細化礦物場填圖指示成礦流體主要通過北東向斷層運移,而礦區(qū)儲礦場由馬面山群龍北溪組上段、上侏羅統(tǒng)長林組和其間的角度不整合接觸界面構(gòu)成。丁家山鉛鋅礦屬擠壓構(gòu)造成礦系統(tǒng)(大類)下屬的與燕山期花崗質(zhì)巖漿有關(guān)的接觸交代成礦系統(tǒng)類。

 

關(guān)鍵字: 成礦系統(tǒng);成礦作用;接觸交代變質(zhì);丁家山鉛鋅礦

Metallogenic system analysis of
Dingjiashan Pb-Zn ore district in Meixian, Fujian Province
SHI De-feng1,2, ZHANG Shu-gen1,2, HAN Shi-li1,2, AI Guo-liang1,2

1. Key Laboratory of Metallogenic Prediction of Nonferrous Metals, Ministry of Education, Central South University,
Changsha 410083, China;
2. School of Geosciences and Info-Physics, Central South University, Changsha 410083, China

Abstract:Based on the systematic study of metallogenic system elements, such as metallogenic epoch, ore-forming materials source, pass way of ore-forming fluid and site of ore body, it is found that the metallogenesis of Dingjiashan Pb-Zn ore district is contact metasomatic metamorphism between Yanshanian granite and the regional metamorphism calcareous rock of Neoproterozoic Mamianshan Formation Longbeixi group upper. The research on isotope of Pb, S and geochemical exploration confirms that the ore-forming materials are supplied by Yanshanian granite and Mamianshan Formation Longbeixi group, and the research on isotope of H and O confirms that the ore-forming fluid is composed of magmatic water and atmospheric water. The mineral mapping indicates that the ore-forming fluid flows along NE fault. There are three sites of ore body, Neoproterozoic Mamianshan Formation Longbeixi group upper, Jurassic Changlin group and angular unconformity between them. Dingjiashan Pb-Zn ore district is contact metasomatic metamorphism metallogenic system related to Yanshanian granite, which belongs to compression structure metallogenic system.

 

Key words: metallogenic system; metallogenesis; contact metasomatic metamorphism; Dingjiashan Pb-Zn ore district

ISSN 1004-0609
CN 43-1238/TG
CODEN: ZYJXFK

ISSN 1003-6326
CN 43-1239/TG
CODEN: TNMCEW

主管:中國科學技術(shù)協(xié)會 主辦:中國有色金屬學會 承辦:中南大學
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