中文摘要:小寺沟斑岩型铜钼矿产于华北板块北缘，其主体岩体类型为英云闪长 岩和二长花岗岩类，矿物组合为斜长石+角闪石+石英+钾长石±黑云母±辉石+不透明矿物， 岩性为钙碱性I型侵入岩。K_Ar法测得小寺沟岩体花岗斑岩年龄为（122.83±2.46）Ma。岩石主量元素具有高 SiO2、Al2O3、Na2O、Mg＃，低K2O、TiO2、MgO、CaO、P2O5特征。稀土元素具有负Eu异常不明显，低HREE和Y，轻、重稀土元素强烈分异特 征。研究认为，小寺沟岩体与埃达克岩相似，其初始岩浆主要为加厚下地壳的部分熔融产物，即小寺沟埃达克岩为C型埃达克岩，其初始岩浆中可能还有部分地幔物质。小寺沟大型斑岩型铜钼矿 的形成与埃达克岩的成矿专属性、华北板块北缘特殊构造环境密切相关。
Abstract:The Xiaosigou porphyry deposit occurs in the northern margin of North China crat on, which belongs to the East Circum-Pacific metallogenic domain. The Xiaosigou pluton is comprised of tonalite and monzonitic granite, which are both I-type granites, with the mineral assemblage being plagioclase+ amphibole+ quartz+ potass ium feldspar±biotite±pyroxene+some opaque minerals. K-Ar dating of unalter ed granite-porphyry yielded an age of （122.83±2.46）Ma. SiO2, Al2O3, Na2O and Mg＃ are high whereas K2O, TiO2, MgO, CaO and P2O5 are rel atively low. The Xiaosigou pluton is characterized by slightly negative to posit ive δEu anomalies, the lowness of HREE and Y, and the intense fractionation of LREE from HREE. These characteristics suggest that the Xiaosigou pluton is extremely similar to adakite. The primitive magma of the Xiaosigou pluton was derived from the partia lly melted lower crust as well as some mantle materials. The Xiaosigou large-size porphyry copper-molybdenum deposit is genetically in close connection with ada kite and the tectonic environment of the northern edge of North China craton.
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基金项目:科技部国家“十一五”科技支撑计划（2006BA01B07）和国家“973"计划前期研究专项（1007CB416608）
引用文本：
戴雪灵,彭省临,胡祥昭.2010.河北小寺沟铜钼矿埃达克岩: 年龄、地球化学特征及其地质意义[J].矿床地质,29(3):517~528.2010.Adakite in Xiaosigou porphyry copper-molybdenum deposit, Hebei Province: Age,geochemical characteristics and geological implications[J].Mineral Deposits29(3):517~528
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