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巴塘纳交系铅锌矿床地质特征及成矿机理
引用本文:付畅德.巴塘纳交系铅锌矿床地质特征及成矿机理[J].四川地质学报,1993(3).
作者姓名:付畅德
作者单位:四川省地矿局402队
基金项目:地矿部“七五”重点科技攻关项目86010—6—3
摘    要:本文在前人工作基础上研究认为:纳交系铅锌矿床赋存在上寒武统额顶组碳酸盐岩层中,成矿物质主要来自围岩和下伏地层,矿床就位于印支复背斜与多向断裂转折复合部位,受层位、岩性和构造的明显控制,具同生与后生成矿特点,属沉积-改造型层控矿床。

关 键 词:纳交系  铅锌矿  沉积—改造型  层控矿床

GEOLOGICAL CHARACTERISTICS AND ORE-FORMING MECHANISM OF NAJIAOXI Pb-Zn DEPOSIT IN BATANG, SICHUAN
Fu Changde.GEOLOGICAL CHARACTERISTICS AND ORE-FORMING MECHANISM OF NAJIAOXI Pb-Zn DEPOSIT IN BATANG, SICHUAN[J].Acta Geologica Sichuan,1993(3).
Authors:Fu Changde
Abstract:From the previous data and this study it is concluded that Najiaoxi Pb-Zn deposit is confined to the carbonate rock of the Eding Formation of the Upper Cambrian. Ore-forming material was derived from the wall rocks and the underlying strata. The Pb-Zn deposit was emplaced in an Indo-Sinian anti-clinorium and hinge and combinatim of various fractures and are under the control of stratigraphic horizon, lithological character and structure. Being of both syngenetic and epigenetic metallization, the Pb-Zn deposit is a sedimentary-reformation type stratabound deposit.
Keywords:Najiaoxi Pb-Zn deposit  sedimentary-reformation type  stratabound deposit    
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