摘要
刁泉大型银铜矿床产于由黑云母石英二长岩、花岗斑岩、石英斑岩等组成的复式岩体的夕卡岩带中,矿化呈环带状展布。矿体严格受火山口构造控制。由银铜矿的地质特征、矿物组成、微量元素、稳定同位素、包裹体地球化学特征等研究表明刁泉银铜矿是与次火山岩体有关的夕卡岩型银铜矿床。
The Diaoquan silver
copper deposit,a large sized deposit recently discovered in northeastern Shanxi,occurs in the
skarn zone around a neck facies complex rock body.Orebodies in zonal distribution are strictly
controlled by crater structure.Composed of quartz porphyry,granite porphyry,biotite quartz
monzonite and gabbro,the complex rock body intruded into Middle and Upper Cambrian and
Lower and Middle Ordovician carbonate strata which contain relatively high minor elements
such as Ag,Au,Pb and Zn.The Cu,Ag,Au,Pb,Zn,As and Mo contents of granite porphyry and
quartz porphyry are 4~9 times higher than their Vinogradov's values in acid rocks,and their
whole rock Rb Sr isotopic isochron age is 130 9×10 6,indicating products of Yanshanian
period.The initial ratio of strontium isotopes( 87 Sr/ 86 Sr) 0 is 0 7061,suggesting that
the rock body is of mixed crust mantle type.The lead isotopic characteristics of rocks give the
same conclusion. The orebodies have complicated mineral composition,with 47 metallic
minerals already observed.The formation of minerals might be divided into two metallogenic
periods and four ore forming stages.Sulfur isotopic composition( δ 34 S) of minerals is
between 0 5‰ and 5 7‰,showing hydrothermal characteristics of magma.The lead isotopic
composition of Diaoquan ores and the characteritic values of the source area are similar to
those of biotite quartz monzonite and granite porphyry.δ 18 O H 2O of ore forming fluids
is 3 66‰,and δ D is -91‰,exhibiting characteritstics of initial magmatic water.Meteoric
water entered the ore forming fluids at the late ore forming stage.When the ore fomring
temperature of fluids was 120~400℃ and 120~220℃,the salinity of fluids was 3 5% ̄3
8%NaCl;when the ore forming temperature was 325 ̄400℃,the salinity of fluids was 40% ̄
46%NaCl.The Diaoquan silver copper deposit was a skarn type silver copper deposit related to
the subvolcanic rock body.Copper and gold mineralization took place relatively early,but the
principal ore forming process occurred somewhat later and was related to volcanic epithermal
mesothermal solution.
出处
《矿床地质》
CAS
CSCD
北大核心
1999年第1期11-21,共11页
Mineral Deposits
基金
国家白银基金
关键词
银矿床
铜矿床
地质特征
成因机制
Skarn type silver copper deposit,metallogenic characteristics,
Diaoquan orefield in Shanxi Province