摘要
天山位于我国西部新疆地区,西邻国界线,塔里木盆地与准噶尔盆地之间。西天山以金属矿产众多,不乏出产大矿而出名。天山期主要发生在中泥盆世-早二叠世（386~257 Ma）,在此时期主要发育有铅、赤铁矿、菱铁矿、煤、铝、硫等沉积矿床;此外,与岩浆有关的矿床以及铅锌多金属层控型矿床,其内生成矿作用较为强烈。西天山是我国重要的成矿带,此区产出的大量铜、铅、锌、金、钼等矿,这些矿床在其成因上多多少少存在着联系,运用矿床成矿系列理论对这些矿床进行分类、对比,分析其内在联系与成因关系对指导找矿提供重要理论依据。
Tianshan is located in China＇s western region of Xinjiang, neighboring west line, between Tarim Basin and Junggar basin. In the West Tianshan metal mineral is numerous, many famous large mine production. Tianshan period mainly occurred in the Middle Devonian to early Permian（386-257 Ma）, in this period mainly development lead, hematite, siderite,coal, aluminum, sulfur and other sedimentary deposit and magma and related deposits and lead-zinc polymetallic layer control type deposit, the generated ore more strongly. West Tianshan is China＇s important metallogenic belt, the output in this area has a large number of copper, lead, zinc, gold, molybdenum and other, these deposits in the cause of more or less there is a link, use the theory of metallogenic series of ore deposits of these deposits are classified, contrast, analysis the intrinsic relation and the reason.To analyze its inner link and genetic relationship to guide prospecting provide important theoretical basis.
出处
《能源研究与管理》
2015年第4期24-28,共5页
Energy Research and Management
关键词
西天山
天山成矿阶段
成矿系列
多金属矿床
Western Tianshan
Tianshan geological era
metallogenic series
polymetallic deposit
作者简介
劳玉军（1989-），男，广西崇左人，硕士研究生在读，地质资源与地质工程专业，主要研究方向：矿产普查与勘探。
