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首页> 外文期刊>Resource Geology >Ar-40/Ar-39 Geochronology of Volcanic and Intrusive Rocks in the Papandayan Metallic Prospect Area, West Java, Indonesia
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Ar-40/Ar-39 Geochronology of Volcanic and Intrusive Rocks in the Papandayan Metallic Prospect Area, West Java, Indonesia

机译:AR-40 / AR-39在印度尼西亚西爪哇省的巴巴扬扬金属前景区火山和侵入性岩石的地理学

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摘要

This study presents new Ar-40/Ar-39 ages on the volcanic and intrusive rocks from the Papandayan metallic district in West Java, Indonesia. The vein system in the Arinem area, one of the prospective areas in the district, has been considered as an epithermal gold-silver-base metal deposit, however, no published age results are available for the host volcanic rocks in the district. The ages of these rocks are critical in terms of their association with mineralization and are important to understand the evolution of volcanism in the region, which has implications for mineral exploration in the district. Ar-40/Ar-39 plateau ages of two typical basalt and one andesite samples of the Jampang Formation volcanic rocks yielded ages of 11.65 +/- 0.52Ma, 18.15 +/- 0.46Ma and 7.69 +/- 0.05Ma, respectively. Ar-40/Ar-39 ages of three intrusive rock samples from Gunung Halang diorite, Gunung Lingga diorite, and Gunung Buligir fine-grained quartz diorite yielded ages of 12.98 +/- 0.20Ma, 10.81 +/- 0.15Ma, and 7.37 +/- 0.05Ma, respectively. The age of the youngest fine-grained diorite (Gunung Wayang dike) is 3.95 +/- 0.03Ma. An Ar-40/Ar-39 age obtained from adularia in the Arinem mineralized vein (18.30 +/- 0.20Ma) is older than the age of altered basalt sample of this study (11.65 +/- 0.52Ma) and the K-Ar illite ages of the Arinem vein (9.4 +/- 0.3Ma and 8.8 +/- 0.3Ma) which resulted from a previous study. The age results suggest that the Papandayan district may have experienced multiple hydrothermal and mineralization events. This study, therefore, provides crucial age data to support future mineral exploration in the district.
机译:本研究提出了来自印度尼西亚西爪哇省巴布纳金属区的火山和侵入式岩石上的新AR-40 / AR-39。该地区潜在地区之一的Arinem地区的静脉系统被认为是卵子金银基金金属矿床,但是,该区宿主火山岩没有公布的年龄结果。这些岩石的年龄在与矿化的关系方面至关重要,并且对于了解该地区的火山主义的演变非常重要,这对该地区的矿产勘探有影响。 AR-40 / AR-39两个典型玄武岩的高原和Jampang地层火山岩的一个安特氏型样品,分别为11.65 +/- 0.52mA,18.15 +/- 0.46mA和7.69 +/- 0.05mA。来自Gunung Halang Diorite,Gunung Lingga Diorite的三个侵入式侵入式岩石样品和Gunung Buligir细粒度石英二霰素,9.98 +/- 0.20mA,10.81 +/- 0.15mA,7.37 + / - 0.05mA分别。最小的细粒粒子(Gunung Wayang Dike)的年龄是3.95 +/- 0.03ma。从Arinem矿化静脉(18.30 +/- 0.20mA)的AR-40 / AR-39年龄比本研究的改变玄武岩样品(11.65 +/- 0.52mA)和K-AR的型玄武岩样本年龄较大Arinem vein(9.4 +/- 0.3mA和8.8 +/- 0.3mA)的灯座年龄,由之前的研究产生。年龄结果表明,巴布纳南区可能经历过多种水热和矿化事件。因此,本研究提供了关键的年龄数据,以支持该地区未来的矿物勘探。

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