劳玉军, 江思宇. New Progress in Study of Metallogenic Series at Tianshan Geological Era in Western Tianshan[J]. 2015, (4): 24-28. DOI: 10.16056/j.1005-7676.2015.04.007.
西天山成矿带天山期成矿阶段矿床成矿系列研究进展
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
2
57 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。
Abstract
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.