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2014年
17期
15-17
,共3页
地质特征%成矿条件%找矿方向%武定县铅锌矿
地質特徵%成礦條件%找礦方嚮%武定縣鉛鋅礦
지질특정%성광조건%조광방향%무정현연자광
geological characteristics%metallogenic condition%prospecting direction%lead and zinc ore of Wuding County
武定地区区域矿产资源极丰富,矿区经过40多年的勘查,共发现各类矿点百余个,综合研究表明,武定县平地耀左所铜矿床类型以“东川式”铜矿最重要,分布在金钟罩、鸡冠山、油基田、周家箐、走马地、黄龙河、牛德庄等地;次为稀矿山式,主要在蒿枝地,走马地等地。“东川式”铜矿:落雪组底部过渡层,“稀矿山式”铁铜矿:因民组下部,同生断裂旁侧,古火山机构中的火山洼地,火山旋回的中上部,富含Na2O的细碧角斑岩系,硅质岩、萤石岩、钠长岩等喷流岩以及黑云母、绿泥石火山凝灰岩的分布区。
武定地區區域礦產資源極豐富,礦區經過40多年的勘查,共髮現各類礦點百餘箇,綜閤研究錶明,武定縣平地耀左所銅礦床類型以“東川式”銅礦最重要,分佈在金鐘罩、鷄冠山、油基田、週傢箐、走馬地、黃龍河、牛德莊等地;次為稀礦山式,主要在蒿枝地,走馬地等地。“東川式”銅礦:落雪組底部過渡層,“稀礦山式”鐵銅礦:因民組下部,同生斷裂徬側,古火山機構中的火山窪地,火山鏇迴的中上部,富含Na2O的細碧角斑巖繫,硅質巖、螢石巖、鈉長巖等噴流巖以及黑雲母、綠泥石火山凝灰巖的分佈區。
무정지구구역광산자원겁봉부,광구경과40다년적감사,공발현각류광점백여개,종합연구표명,무정현평지요좌소동광상류형이“동천식”동광최중요,분포재금종조、계관산、유기전、주가정、주마지、황룡하、우덕장등지;차위희광산식,주요재호지지,주마지등지。“동천식”동광:락설조저부과도층,“희광산식”철동광:인민조하부,동생단렬방측,고화산궤구중적화산와지,화산선회적중상부,부함Na2O적세벽각반암계,규질암、형석암、납장암등분류암이급흑운모、록니석화산응회암적분포구。
Regional mineral resources of Wuding region are extremely rich, after 40 years of mining exploration, all kinds of hundred mines were found. Comprehensive studies show that, "Dongchuan style" copper mine is the most important mine in Wuding Pingdi-Zuosuo copper deposits, which located in Jinzhongzhao, Jiguanshan, oil-based fields, Zhoujiaqing, Zoumadi, Huanglong River, Niudezhuang etc.;Dilute mine type is the second important, mainly in Artemisia sticks, Zoumadi and other places. "Dongchuan style" copper mine: bottom snow group buffer layer; "dilute mine type" iron-copper: due to the lower part of the public group, contemporaneous faults flanking the ancient volcano volcanic depressions institutions, volcanic cycles in the upper rich Na2O of spilite porphyry system, chert, fluorite rock, rock and other jet albite rock and biotite, chlorite volcanic tuff distribution.