地球
地毬
지구
EARTH
2013年
12期
295-296
,共2页
硫钼矿%矿床地质特征%矿体成因
硫鉬礦%礦床地質特徵%礦體成因
류목광%광상지질특정%광체성인
pyrites molybdenum deposit%Geological feature of the ore deposi%Genesis of ore bodies
通过介绍铁坑矿区地质背景以及硫钼矿体特征、围岩蚀变，说明矿体产出与二叠系下统地层和燕山期花岗闪长斑岩有关。矿源、构造、成矿时序是找矿的有利地段。
通過介紹鐵坑礦區地質揹景以及硫鉬礦體特徵、圍巖蝕變，說明礦體產齣與二疊繫下統地層和燕山期花崗閃長斑巖有關。礦源、構造、成礦時序是找礦的有利地段。
통과개소철갱광구지질배경이급류목광체특정、위암식변，설명광체산출여이첩계하통지층화연산기화강섬장반암유관。광원、구조、성광시서시조광적유리지단。
Through the introduction of Tiekeng mining area geological background, Pyrites and Molybdenum ore body characteristics, erodibility of wall rock, reveal the formation of the orebodies was associated with the lower permian strata and the activities of intermediate to acidic magma . Ore source, structure, metallogenic series are favourable places for deposit-seeking.
