摘要
成矿物质来源是矿床研究的重要内容。本文通过里伍铜矿含矿岩石中的石英流体包裹体的温度、成分和盐度测试分析,以及矿床地球化学特征研究,结合区域地质演化历史,揭示其成矿物质来源、成矿物质的运移和浓集机制,为解释里伍铜矿的成矿环境和成因提供依据。
The approaches to the sources of ore-forming matter are considered as an important aspect for the research of ore deposits. The exploration of temperatures, compositions and salinity of the quartz inclusions from the ore-bearing rocks, and geochemical signatures of the Liwu copper deposit, Jiulong, Sichuan has disclosed the sources, migration and enrichment of the ore-forming matter, thus help establish a basis for the interpretation of the genesis and mineralization conditions of the Liwu copper deposit.
出处
《沉积与特提斯地质》
CAS
CSCD
2008年第2期1-11,共11页
Sedimentary Geology and Tethyan Geology
关键词
里伍铜矿
包裹体
成矿流体
Liwu copper deposit
inclusion
mineralizing fluid
