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福建德化下坂斑岩金矿地质特征及成因探讨
引用本文:朱玉磷,刘永发,张金塔.福建德化下坂斑岩金矿地质特征及成因探讨[J].福建地质,2009,28(1):21-35.
作者姓名:朱玉磷  刘永发  张金塔
作者单位:中国冶金地质总局二局,福州,350001
摘    要:下坂金矿位于中国东南沿海中生代陆相火山岩带之中,是近年来勘查的金矿床。通过对矿床的地质学、矿床学、地球化学等特征的研究,该矿床成因上与流纹斑岩关系密切,具有广义斑岩型矿床特点。

关 键 词:斑岩金矿  地质特征  德化下坂

On the Geologic Characteristics and Genesis of the Xiaban Porphyritic Gold Mine in Dehua County,Fujian Province
Zhu Yulin,Liu Yongfa,Zhang Jinta.On the Geologic Characteristics and Genesis of the Xiaban Porphyritic Gold Mine in Dehua County,Fujian Province[J].Geology of Fujian,2009,28(1):21-35.
Authors:Zhu Yulin  Liu Yongfa  Zhang Jinta
Institution:Zhu Yulin Liu Yongfa Zhang Jinta(No.2 Bureau of China Metallurgical Geology Bureau,Fuzhou,350001)
Abstract:The Xiaban gold mine is situated at the Mesozoic volcanic zone of continental facies in the coast area of Southeast China and is one of gold deposits discovered in recent years in Fujian Province.Based on the characteristics of geology,mineral deposit and geochemistry for the Xiaban gold deposit,it is considered that the Xiaban gold deposit has a close relation with the rhyolite porphyry and is provided with the characteristics of generalized porphyritic type deposits.
Keywords:porphyry  gold mine  Dehua County  Fujian Province  
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