西北地质
西北地質
서북지질
NORTHWESTERN GEOLOGY
2015年
2期
169-175
,共7页
李永勤%王瑞廷%孟德明%代军治%黄长青
李永勤%王瑞廷%孟德明%代軍治%黃長青
리영근%왕서정%맹덕명%대군치%황장청
凤太矿集区%太山庙铜矿%地质特征%找矿标志%找矿方向
鳳太礦集區%太山廟銅礦%地質特徵%找礦標誌%找礦方嚮
봉태광집구%태산묘동광%지질특정%조광표지%조광방향
Feng-Tai ore-concentrated area%Taishanmiao copper deposit%geological characteris-tics%indicatorfor prospecting%prospecting direction
凤县太山庙铜矿点位于凤(县)太(白)矿集区南部铅硐山苇子坪铜牌沟铜铅锌多金属成矿带之铁炉湾九子沟矿化区,区内从西到东矿化分带明显,成矿条件十分有利。太山庙铜矿赋存于中泥盆统古道岭组灰岩与星红铺组千枚岩接触界面及其附近,属沉积改造型矿床;背斜构造、中泥盆统古道岭组灰岩与上泥盆统星红铺千枚岩接触带和硅化、黄铁矿化等蚀变是其主要找矿标志。目前,在太山庙铜矿区已发现 K1、K2两条铜矿体,矿石类型以硅化灰岩型为主,其次为硅化千枚岩型、含铜石英方解石脉型及硅质岩型。通过与东部凤县九子沟铜矿床对比研究,认为二者处于同一含矿层位,区内找矿应关注背斜构造转折端及其翼部的古道岭组灰岩和星红铺组千枚岩接触界面这2个主要找矿标志,注意背斜南翼铁碳酸岩脉及平行背斜构造,结合化探异常和物探异常,进而优选靶位开展深部工程验证,按照这一指导思想和工作方法,在区内及太山庙铜矿点有望取得新的找矿突破。
鳳縣太山廟銅礦點位于鳳(縣)太(白)礦集區南部鉛硐山葦子坪銅牌溝銅鉛鋅多金屬成礦帶之鐵爐灣九子溝礦化區,區內從西到東礦化分帶明顯,成礦條件十分有利。太山廟銅礦賦存于中泥盆統古道嶺組灰巖與星紅鋪組韆枚巖接觸界麵及其附近,屬沉積改造型礦床;揹斜構造、中泥盆統古道嶺組灰巖與上泥盆統星紅鋪韆枚巖接觸帶和硅化、黃鐵礦化等蝕變是其主要找礦標誌。目前,在太山廟銅礦區已髮現 K1、K2兩條銅礦體,礦石類型以硅化灰巖型為主,其次為硅化韆枚巖型、含銅石英方解石脈型及硅質巖型。通過與東部鳳縣九子溝銅礦床對比研究,認為二者處于同一含礦層位,區內找礦應關註揹斜構造轉摺耑及其翼部的古道嶺組灰巖和星紅鋪組韆枚巖接觸界麵這2箇主要找礦標誌,註意揹斜南翼鐵碳痠巖脈及平行揹斜構造,結閤化探異常和物探異常,進而優選靶位開展深部工程驗證,按照這一指導思想和工作方法,在區內及太山廟銅礦點有望取得新的找礦突破。
봉현태산묘동광점위우봉(현)태(백)광집구남부연동산위자평동패구동연자다금속성광대지철로만구자구광화구,구내종서도동광화분대명현,성광조건십분유리。태산묘동광부존우중니분통고도령조회암여성홍포조천매암접촉계면급기부근,속침적개조형광상;배사구조、중니분통고도령조회암여상니분통성홍포천매암접촉대화규화、황철광화등식변시기주요조광표지。목전,재태산묘동광구이발현 K1、K2량조동광체,광석류형이규화회암형위주,기차위규화천매암형、함동석영방해석맥형급규질암형。통과여동부봉현구자구동광상대비연구,인위이자처우동일함광층위,구내조광응관주배사구조전절단급기익부적고도령조회암화성홍포조천매암접촉계면저2개주요조광표지,주의배사남익철탄산암맥급평행배사구조,결합화탐이상화물탐이상,진이우선파위개전심부공정험증,안조저일지도사상화공작방법,재구내급태산묘동광점유망취득신적조광돌파。
The Taishanmiao copper deposit of Fengxian County is located in Tieluwan-Jiuzigou mineralized district of Qiandongshan-Weiziping-Tongpaigou Cu-Pb-Zn polymetallic mineraliza-tionbelt,south of Fengxian-Taibai ore-concentrated area.Mineralization zoning is clear from east to west of this area and metallogenetic conditions are favorable.Ore body occurs at the contact zone or nearby of Middle Devonian Gudaoling formation limestone and Upper Devonian Xinghong-pu formation phyllite,belonging to sedimentary-reformation deposit.Anticline,contact zone of limestone and phyllite,silication and pyritization are the main indicators for prospecting.Ore bodies including K1 and K2 are found in this deposit,in which silicified limestone is the main ore type,followed by silicified phyllite type,copper-bearing quartz-calcite vein type and siliceous rock type.Comparing with Jiuzigou copper deposit in the east of Fengxian county,they are in thesame ore-bearing position,prospecting should thus be based on transition and two wing twists of anticline and contact of limestone and phyllite,attention also should be paid to iron-carbonate veins of southern anticline and parallel to it.Combined with geophysical and geochemical anoma-ly,we can define optimal target and conductin-depth engineering test.Based on this exploration method and procedure,new prospecting break through is expected tobe madein Taishanmiao cop-per deposit.