山东招远市谢家沟-石城夼构造岩浆带金成矿系统研究
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摘要
胶东金矿集中区是我国重要的黄金生产基地。谢家沟金矿则是新发现的大型金矿床,与产在大型断裂带上著名的焦家金矿、玲珑金矿不同,谢家沟金矿位于焦家断裂带与招平断裂带之间。因此,谢家沟金矿的发现即为该区地质找矿的新突破,并带来新的找矿思路。
本文重点解剖谢家沟金矿床。谢家沟金矿产于蚀变的玲珑花岗岩内,并受脆-韧性剪切带构造控制,单矿物及全岩的K-Ar 法测年获得主成矿年龄115~125Ma,矿化类型分为同剪切带蚀变岩型和石英硫化物脉型两种,三个热液成矿阶段形成黄铁绢英岩型、黄铁矿-黄铜矿绢英岩型和多金属硫化物绢英岩(石英脉)等不同矿物组合的矿石类型。围岩蚀变主要有绢英岩化、硅化、黄铁矿化、钾化、碳酸盐化和绿泥石化等,且蚀变具有较明显的分带性,认为其原因与不同蚀变作用的叠加有关。
根据地表宏观特征,谢家沟金矿及其外围的小宋家、白鹤顶、北冯家和山陈家等矿化点均受统一脆-韧性剪切带控制。另外,磁异常资料显示,该剪切带深部发育隐伏郭家岭花岗岩,因此,作者称之为谢家沟-石城夼构造岩浆带。CSAMT测深表明,该构造岩浆带具有低阻高导的特点,并在倾向上最深可达-300m 中段,走向上延伸稳定。根据岩石变形、蚀变和矿化程度,谢家沟-石城夼构造岩浆带由白鹤顶剪切带、谢家沟剪切带和北冯家剪切带组成,它们近平行产出,并受统一构造应力场控制。
综合研究谢家沟金矿和四个矿化点,探讨成矿系统的基本要素,初步建立了谢家沟-石城夼构造岩浆带金成矿系统。成矿的区域地质背景是各种地质作用的耦合,太平洋板块俯冲是构造作用及岩浆活动的主要原动力,构造体制转换为成矿提供了有利的地质条件;成矿物质主要来自胶东群等老地层;成矿流体主要是岩浆热液,同时含有大量幔源的流体,含矿流体的沸腾是促使金沉淀成矿的直接因素;隐伏的郭家岭花岗岩为金成矿提供了大量的能量;脆-韧性剪切带既是含矿流体的运移通道,也是最重要的储矿构造。
本文利用黄铁矿标型特征、地球化学原生晕分带模型等方法探讨矿床形成后的剥蚀与保存,认为构造岩浆带的浅部矿体已被剥蚀,但深部还有很好的资源潜力。成矿期后断裂构造活动及脉岩贯入没有改变矿床的本质特征。
Jiaodong gold deposit cluster in Shandong Province is the most important gold production base in China. Different from two famous gold deposit “Jiaojia deposit”and “Linglong deposit”, Xiejiagou gold deposit, a large scale deposit found in 2002, was not located on the fault belt, but between Jiaojia fault belt and Zhaoping fault belt. Therefore, the investigation of Xiejiagou deposit is greatly advance on geological research and will enlarge our knowledge on exploration.
Our study focused on Xiejiagou gold deposit. Xiejiagou deposit occurred in alteration granite and was controlled by brittle-ductility shearing belt. The age of main mineralization was from 115 Ma to 125 Ma. Mineralization type was divided into synshearing alteration type and sulfide quartz vein. Three kinds of ores, pyritization-pyrilic-phyllic alteration, multi-sulfide quartz vein and chalcopyritization-pyritization-pyrilic-phyllic alteration, formed in different mineralization periods. The alterations of wall rock related to mineralization were pyrilic phyllic, silicification, pyritization and so on. And the reason for alteration zoning was superposition of different kind of alteration.
Several mineralization points have been founded in the surroundings of Xiejiagou gold deposit, such as Xiaosongjia, Baiheding, Beifengjia and Shanchenjia (still under investigation). According to macro-features on surface, it is believed that the deposit and all mineralization points were controlled by the same brittle-ductility shearing belt. Besides, magnetic anomaly research indicates that there occurred blind Guojialing type granite at the area. So we call it as Xiejiagou-Shichengkuang structure-magma belt. The study by CSAMT shows that the structure-magma belt was a low resistance geological body which was on large scale. According to deformation degree, alteration and mineralization forms of rock, Xiejiagou-Shichengkuang structure-magma belt is made up of Baiheding shearing belt, Xiejiagou shearing belt and Beifengjia shearing belt which were output parallel and controlled by the same stress field.
Based on the integrated study on Xiejiagou gold deposit and other mineralization points, the Xiejiagou-Shichengkuang structure-magma belt was set up preliminarily in the paper after discussion on the basic elements of mineralization system. It was regarded that the coupling of different geological process was the key on regional setting for mineralization. The subduction of pacific plate was the main dynamic for tectonism and magmatism. The transfer of tectonic system provided benefic geological conditions for mineralization especially. Most of gold was from
本文重点解剖谢家沟金矿床。谢家沟金矿产于蚀变的玲珑花岗岩内,并受脆-韧性剪切带构造控制,单矿物及全岩的K-Ar 法测年获得主成矿年龄115~125Ma,矿化类型分为同剪切带蚀变岩型和石英硫化物脉型两种,三个热液成矿阶段形成黄铁绢英岩型、黄铁矿-黄铜矿绢英岩型和多金属硫化物绢英岩(石英脉)等不同矿物组合的矿石类型。围岩蚀变主要有绢英岩化、硅化、黄铁矿化、钾化、碳酸盐化和绿泥石化等,且蚀变具有较明显的分带性,认为其原因与不同蚀变作用的叠加有关。
根据地表宏观特征,谢家沟金矿及其外围的小宋家、白鹤顶、北冯家和山陈家等矿化点均受统一脆-韧性剪切带控制。另外,磁异常资料显示,该剪切带深部发育隐伏郭家岭花岗岩,因此,作者称之为谢家沟-石城夼构造岩浆带。CSAMT测深表明,该构造岩浆带具有低阻高导的特点,并在倾向上最深可达-300m 中段,走向上延伸稳定。根据岩石变形、蚀变和矿化程度,谢家沟-石城夼构造岩浆带由白鹤顶剪切带、谢家沟剪切带和北冯家剪切带组成,它们近平行产出,并受统一构造应力场控制。
综合研究谢家沟金矿和四个矿化点,探讨成矿系统的基本要素,初步建立了谢家沟-石城夼构造岩浆带金成矿系统。成矿的区域地质背景是各种地质作用的耦合,太平洋板块俯冲是构造作用及岩浆活动的主要原动力,构造体制转换为成矿提供了有利的地质条件;成矿物质主要来自胶东群等老地层;成矿流体主要是岩浆热液,同时含有大量幔源的流体,含矿流体的沸腾是促使金沉淀成矿的直接因素;隐伏的郭家岭花岗岩为金成矿提供了大量的能量;脆-韧性剪切带既是含矿流体的运移通道,也是最重要的储矿构造。
本文利用黄铁矿标型特征、地球化学原生晕分带模型等方法探讨矿床形成后的剥蚀与保存,认为构造岩浆带的浅部矿体已被剥蚀,但深部还有很好的资源潜力。成矿期后断裂构造活动及脉岩贯入没有改变矿床的本质特征。
Jiaodong gold deposit cluster in Shandong Province is the most important gold production base in China. Different from two famous gold deposit “Jiaojia deposit”and “Linglong deposit”, Xiejiagou gold deposit, a large scale deposit found in 2002, was not located on the fault belt, but between Jiaojia fault belt and Zhaoping fault belt. Therefore, the investigation of Xiejiagou deposit is greatly advance on geological research and will enlarge our knowledge on exploration.
Our study focused on Xiejiagou gold deposit. Xiejiagou deposit occurred in alteration granite and was controlled by brittle-ductility shearing belt. The age of main mineralization was from 115 Ma to 125 Ma. Mineralization type was divided into synshearing alteration type and sulfide quartz vein. Three kinds of ores, pyritization-pyrilic-phyllic alteration, multi-sulfide quartz vein and chalcopyritization-pyritization-pyrilic-phyllic alteration, formed in different mineralization periods. The alterations of wall rock related to mineralization were pyrilic phyllic, silicification, pyritization and so on. And the reason for alteration zoning was superposition of different kind of alteration.
Several mineralization points have been founded in the surroundings of Xiejiagou gold deposit, such as Xiaosongjia, Baiheding, Beifengjia and Shanchenjia (still under investigation). According to macro-features on surface, it is believed that the deposit and all mineralization points were controlled by the same brittle-ductility shearing belt. Besides, magnetic anomaly research indicates that there occurred blind Guojialing type granite at the area. So we call it as Xiejiagou-Shichengkuang structure-magma belt. The study by CSAMT shows that the structure-magma belt was a low resistance geological body which was on large scale. According to deformation degree, alteration and mineralization forms of rock, Xiejiagou-Shichengkuang structure-magma belt is made up of Baiheding shearing belt, Xiejiagou shearing belt and Beifengjia shearing belt which were output parallel and controlled by the same stress field.
Based on the integrated study on Xiejiagou gold deposit and other mineralization points, the Xiejiagou-Shichengkuang structure-magma belt was set up preliminarily in the paper after discussion on the basic elements of mineralization system. It was regarded that the coupling of different geological process was the key on regional setting for mineralization. The subduction of pacific plate was the main dynamic for tectonism and magmatism. The transfer of tectonic system provided benefic geological conditions for mineralization especially. Most of gold was from
引文
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