陕西省凤太矿集区柴蚂金矿床碳酸盐矿物的Sm-Nd同位素测年及意义
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摘要
柴蚂金矿床位于陕西省凤太矿集区西北部,八卦庙超大型金矿床西侧约0.5km处,二者在成矿地质背景和控矿条件等方面均较为相似。该矿床共划分出5个含矿带,其产出位置受地层和构造联合控制。矿石类型有石英脉型和蚀变岩型,以石英脉型为主。成矿过程可划分为早期石英-碳酸盐阶段、主成矿期石英-碳酸盐-硫化物阶段和晚期石英阶段。本次工作对主成矿阶段的白云石、方解石等碳酸盐矿物进行了Sm-Nd同位素测年研究,获得等时线年龄为203.2±1.6Ma,表明矿床形成于晚三叠世。结合前人对区内金矿、岩浆岩和构造活动的研究认为,柴蚂金矿床是印支末期后碰撞过程中形成的造山型金矿床。
The Chaima gold deposit is located on the northwest of the Fengtai ore concentration area in Shaanxi Province and 0. 5km west to the super-large Baguamiao gold deposit. They are similar in metallogenic geological environment and ore-control conditions. There are five ore-bearing zones in this deposit and their occurrence is controlled by lithology and tectonic. The ores are quartz-vein type and altered-rock type,in which the first is the main type. The gold mineralization of Chaima gold deposit could be divided into three stages: the early quartz-carbonate stage,the second and main quartz-carbonate-sulfide stage and the late quartz stage. In this paper,the Sm-Nd isotopic dating is carried out on the calcite and dolomite from the main stage,yielding an isochron age of 203. 2 ± 1. 6Ma,which shows that the deposit formed in Late Triassic. Combined with the previous research on the gold deposits,magmatite and tectonic movements of the area,we suggest that the Chaima gold deposit is an orogenic gold deposit formed after the collision of Qinling in Late Indosinian.
The Chaima gold deposit is located on the northwest of the Fengtai ore concentration area in Shaanxi Province and 0. 5km west to the super-large Baguamiao gold deposit. They are similar in metallogenic geological environment and ore-control conditions. There are five ore-bearing zones in this deposit and their occurrence is controlled by lithology and tectonic. The ores are quartz-vein type and altered-rock type,in which the first is the main type. The gold mineralization of Chaima gold deposit could be divided into three stages: the early quartz-carbonate stage,the second and main quartz-carbonate-sulfide stage and the late quartz stage. In this paper,the Sm-Nd isotopic dating is carried out on the calcite and dolomite from the main stage,yielding an isochron age of 203. 2 ± 1. 6Ma,which shows that the deposit formed in Late Triassic. Combined with the previous research on the gold deposits,magmatite and tectonic movements of the area,we suggest that the Chaima gold deposit is an orogenic gold deposit formed after the collision of Qinling in Late Indosinian.
引文
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