哈萨克斯坦阿克斗卡特大型斑岩铜矿床成矿时代与剥露历史研究  

Metallogenic Age of the Super-Large Aktogai Porphyry Copper Deposit, Kazakhstan, and Its Exhumation History

作　　者：李勇[1] 陈宣华[1] 董树文[1] 王志宏[2] 陈正乐[2] 韩淑琴[2] Eleonora SEITMURATOVA 杨屹 叶宝莹[5] 施炜[2] 陈文[6] 

机构地区：[1]中国地质科学院,北京100037 [2]中国地质科学院地质力学研究所,北京100081 [3]Laboratory of Geological Formations,K.Satpaev Institute of Geological Sciences [4]新疆维吾尔自治区地质矿产开发勘查局第一区调大队,乌鲁木齐830011 [5]中国地质大学(北京),北京100083 [6]中国地质科学院地质研究所,北京100037

出　　处：《地质学报》2012年第2期295-306,共12页Acta Geologica Sinica

基　　金：国家科技支撑计划重点项目暨国家"305"项目(编号2007BAB25B02)资助成果

摘　　要：哈萨克斯坦阿克斗卡特大型斑岩型铜矿床产在中亚成矿域巴尔喀什成矿带阿克斗卡矿田。本文根据花岗岩类岩石的锆石U-Pb、40Ar/39Ar和裂变径迹(FT)热年代学研究,结合前人研究成果,给出了阿克斗卡斑岩铜矿床从深成岩浆活动、成矿作用、区域冷却到剥露作用的全过程。阿克斗卡矿床及附近花岗岩类锆石SHRIMPU-Pb定年结果,给出科尔达尔岩体早期英云闪长岩的结晶年龄为335.7±1.3Ma;主成矿期的含矿二长花岗斑岩结晶年龄为327.5±1.9Ma,反映了阿克斗卡矿床斑岩型铜成矿作用的年龄。花岗岩类角闪石、黑云母、钾长石40Ar/39Ar热年代学分别给出矿物冷却年龄为310.6Ma、271.5Ma和274.9Ma,进一步限定了深成斑岩型铜成矿作用的时代和区域冷却的历史。磷灰石FT测年数据揭示,受区域构造作用的影响,阿克斗卡铜矿田在晚白垩世(91～68.0Ma)发生地块的差异隆升和剥露作用。The super-large Aktogai porphyry copper deposit is one of three porphyry copper deposits in the Aktogai ore field in the Balkhash metallogenic belt, Kazakhstan, Central Asia. In this study, zircon SHRIMP, 40Ar/39Ar and fission track （FT） dating, together with metallogenic data from previous studies, reveals the whole thermal history from the intrusion of plutons and porphyry copper metallogenesis, and regional cooling, to the exhumation of the deposits. Zircon SHRIMP dating of granitoids from the Aktogay ore field gives a crystallization age of 335.7±1.3 Ma for quartz diorite from the Cole-Dahl intrusion body, and of 327.5±1.9 Ma for the Cu-bearing porphyry granodiorite from the Aktogay deposit. These two ages represent the age of main ore-forming stage of the Aktogai porphyry Cu deposit. 40Ar/39Ar thermochronology of hornblende, biotite, and K-feldspar gives the mineral cooling ages of 310.6 Ma, 271.5 Ma, and 274.9 Ma, respectively, further constraining the porphyry Cu mineralization and regional cooling history. Apatite FT dating of granitoids yields low temperature cooling ages of 91 Ma and 68.0 Ma, suggesting that the Aktogai ore field had undergone the differential uplifting and exhumation resulting from regional tectonic activity during the Late Cretaceous.

关 键 词：成矿时代 SHRIMP U-PB 40AR/39AR 裂变径迹 阿克斗卡斑岩铜矿床 巴尔喀什成矿带 

分 类 号：P618.41[天文地球—矿床学]