中文摘要:家杖子金矿是赤峰南部地区新发现的隐爆角砾岩型金矿床，矿体呈脉状产于隐爆角砾岩筒内，角砾岩筒主要由隐爆含角砾岩屑晶屑凝灰岩组成。角砾岩筒蚀变强烈，并具一定的蚀变分带，金矿化主要与硅化和冰长石化有关，载金矿物主要为毒砂。含矿岩石的岩石化学特征为铝过饱和型，以w(K2O)＞＞w(Na2O)为特征，属于钙碱性系列I型花岗岩；稀土元素特征表现为轻稀土元素富集型，有Eu亏损；微量元素具有明显的Ti、Nb、Sr、Ba、Th、U亏损，K富集，与大陆边缘正常弧非成熟花岗岩的微量元素特征相符。石英内流体包裹体均一温度表明，金成矿作用主要发生在150～180℃、225～390℃温度段，估算成矿压力为72×105～158×105Pa（255～560 m）。矿石硫同位素组成稳定，δ34SV-CDT变化范围为5.3‰～9.4‰。矿石铅与含矿角砾岩的铅同位素组成相似，μ值分别为7.89～8.16及7.89～8.08，模式年龄为591～622 Ma和478～912 Ma；在Z-D演化模式图上，岩（矿）石铅投影于上地幔与下地壳演化线之间。含矿角砾岩和二长花岗斑岩脉的ISr为0.70820～0.70118，εSr (t)为50.64～106.8，143Nd/144Nd(t)为0.511819～0.512001，εNd(t)为-7.99～-11.62，具有大陆地壳特征。tCHUR及tDM值与该区晚中生代玄武岩、安山岩一致，而不同于印支期闪长岩及其下地壳麻粒岩包体。硫、铅、锶、钕同位素特征显示，成矿物质具壳幔混源特点。主要含矿角砾岩的Rb_Sr同位素等时线年龄为191 Ma，两期隐爆角砾岩之间侵入的二长花岗斑岩脉的等时线年龄为177 Ma。陈家杖子金矿应为与早燕山期隐爆角砾岩有关的浅成中_低温热液型金矿床。
Abstract:The Chenjiazhangzi gold deposit is a newly discovered ore deposit in Chifeng, whose veinlike gold orebodies occur in cryptoexplosive breccia pipes consisting of felsic cryptoexplosive breccia_bearing crystal fragments, lithic fragment tuff, and minor black cryptoexplosive breccia. In this paper, geological and geochemical characteristics of the ore deposit are studied in detail, and its genesis and material source are discussed on the basis of fluid inclusion and isotope studies of the gold ores and ore_bearing rocks. The breccia pipe has been intensely altered and shows apparent alteration zoning. Gold mineralization is closely related to silication and adularization. Electrum is the dominant gold mineral and mainly occurs in arsenopyrite, the dominant gold_carrier mineral. The major oxide of ore_bearing breccia belongs to aluminum supersaturated calc_alkaline I_type granite and is characterized by K2O＞＞Na2O. The primary mantle_normalized rare earth and trace element patterns of the breccia show the enrichment of LREE, K and the depletion of Eu, Ti, Sr, Ba, Th, U, which is in conformity with the features of non_mature normal arc granites on the continental margin. The homogenization temperatures of fluid inclusions in quartz suggest that gold mineralization mainly took place at temperatures of 150～180℃, 225～390℃, and that the estimated ore_forming pressures are about (72～158)×105 Pa（255～560 m）. The sulfur isotope composition of the gold ores is within the range of 5.3‰～9.4‰ δ34SV-CDT. The lead isotope composition of ores and that of ore_bearing breccia are similar to each other, their μ values are in the range of 7.89～8.16, 7.89～8.08, and the mode ages are 591～622 Ma and 478～912 Ma, respectively. The lead composition of ores is located at the area between upper mantle and crust evolution lines in the 207Pb/204Pb-206Pb/204Pb diagram. ISr,εSr(t),143Nd/144Nd(t),εNd(t) of the ore_bearing breccia and monzonitic granite porphyry are in the range of 0.7082～0.70118, 50.64～106.8, 0.511819～0.512001, and -7.99～-11.62, respectively, suggesting that they are derived from the continental crust. tCHUR,tDM values of the ores and ore-bearing breccia are similar to those of Late Mesozoic basalt and andesite, but different from the data of Early Mesozoic diorite and lower crust xenolith outside the ore deposit. Characteristics of S, Pb, Sr, Nd isotopes indicate that ore_forming materials are mainly derived from the crust, with some probably from the mantle. The Rb_Sr isochron age of early ore_bearing breccia is 191 Ma, and the age of monzonitic granite porphyry emplaced after the early breccia pipe is 177 Ma. The Chenjiazhangzi gold deposit is of the epithermal_mesothermal type formed in Early Yanshanian period.
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基金项目:地质调查项目（D002-028-05）
引用文本：
佘宏全，张桂兰，张德全，李大新，丰成友，王 忠，孟立军，王 启.2005.赤峰陈家杖子隐爆角砾岩型金矿床地质地球化学特征与成因[J].矿床地质,24(4):373~387.2005.Geological and geochemical characteristics and genesis of Chenjiazhangzi cryptoexplosive breccia pipe gold deposit, Chifeng, Inner Mongolia [J].Mineral Deposits24(4):373~387
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