辽北地区块状硫化物矿床的成矿物质来源及成因  

SOURCE OF CONSTITUENTS AND GENESIS OF MASSIVE SULFIDE DEPOSITS IN NORTHERN LIAONING PROVINCE

作　　者：彭晓亮[1] 沈保丰[1] 

机构地区：[1]地矿部天津地质矿产研究所

出　　处：《地质找矿论丛》1992年第4期43-49,共7页Contributions to Geology and Mineral Resources Research

摘　　要：辽北地区块状硫化物矿床矿石的稳定同位素及容矿岩系的稀土元素地球化学特征表明,其成矿物质来源和清原绿岩带的火山作用密切相关.矿床的形成是绿岩带火山-喷气热液沉淀和构造富集双重作用的结果.The massive sulfide deposits in northern Liaoning province occur in the felsic volcanic-sedimentary rock series of Qinyuan greenstone belt. Shapes of the deposits are variable and they run from discordant to concordant with surrounding rocks. some are broadly lensoid and have a stratiform appearance while others are irregular-shaped.Geochemical feature of ore stable isotope and the REE of host rocks show that the sources of ore constituents of the deposits closely relate to the volcanism of the greenstone belt, especially to the felsic volcanism. The sulfur isotopic composition implies that the sulfur are mantle-derived, being of magmatic-hydrothermal origin with characters very close to that of the Noranda district in Candian Shield. According to the lead isotopic composition, the source of the metals of deposits are mainly from the host rocks. The forming-time of the deposits are same as the host rock. The REE patterns of the felsicvolcanic rocks related to the deposits are similar to that of the deposits in Canadian Shield. The LREE have a slight enrichement, Eu shows a strong depletion. The extent of the HREE depletion directly represents the mineralized degree.In brief, the massive sulfide deposits are products of the precipitation of volcanic-emanated hydrotbermal solution of the greenstone belt and the enrichement by tectonism.

关 键 词：硫化物矿床 成矿物质 来源 成因 

分 类 号：P612[天文地球—矿床学]