地球
地毬
지구
EARTH
2013年
9期
31-33
,共3页
雷阳艾%陈梁%杨枝斌%Wu Daopeng%Wei Ronghua
雷暘艾%陳樑%楊枝斌%Wu Daopeng%Wei Ronghua
뢰양애%진량%양지빈%Wu Daopeng%Wei Ronghua
锡(钨)矿床%地质特征%找矿远景%云南大理云龙
錫(鎢)礦床%地質特徵%找礦遠景%雲南大理雲龍
석(오)광상%지질특정%조광원경%운남대리운룡
tin (tungsten) deposit,geological characteristics%prospecting%Yunnan Dali Yun Long
云龙锡矿带位于青藏滇缅"歹"字型构造收缩部位的澜沧江变质带中，属于东南亚锡矿带东支一滇泰锡矿带的北延部份。矿带北起泸水县石缸河，南至云龙县铁厂，长约30公里，宽5至15公里。文章对带内锡矿床的地质特征、地球化学特征、矿体富集规律、控矿因素等进行分析和探讨，预测了带上的找矿远景区。
雲龍錫礦帶位于青藏滇緬"歹"字型構造收縮部位的瀾滄江變質帶中，屬于東南亞錫礦帶東支一滇泰錫礦帶的北延部份。礦帶北起瀘水縣石缸河，南至雲龍縣鐵廠，長約30公裏，寬5至15公裏。文章對帶內錫礦床的地質特徵、地毬化學特徵、礦體富集規律、控礦因素等進行分析和探討，預測瞭帶上的找礦遠景區。
운룡석광대위우청장전면"알"자형구조수축부위적란창강변질대중，속우동남아석광대동지일전태석광대적북연부빈。광대북기로수현석항하，남지운룡현철엄，장약30공리，관5지15공리。문장대대내석광상적지질특정、지구화학특정、광체부집규률、공광인소등진행분석화탐토，예측료대상적조광원경구。
the Yunlong tin deposit belt of Lancang Rivermetamorphism is located in the Qinghai Tibet Burma "bad" fontstructure shrinkage parts of the belt, which belongs to theSoutheast Asian tin belt east branch Yidian Thai tin ore belt ofNorth Extension section.Ore belt north of Lushui CountyShiganghe,ironworks south to Yunlong County, about 30 km long,wide 5 to 15 kilometer. The geological characteristics,theband tin deposit,geochemical characteristics, the enrichment regularity of ore body,ore controlling factors are analyzed anddiscussed,prediction with prospecting area.
