40Ar/39Ar Geochronology of Volcanic and Intrusive Rocks in the Papandayan Metallic Prospect Area, West Java, Indonesia

IF 1.1 4区 地球科学 Q3 GEOLOGY Resource Geology Pub Date : 2017-01-01 DOI:10.1111/rge.12118
A. D. Titisari, D. Phillips, Prayatna, E. P. Setyaraharja
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引用次数: 1

Abstract

This study presents new 40Ar/39Ar 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. 40Ar/39Ar plateau ages of two typical basalt and one andesite samples of the Jampang Formation volcanic rocks yielded ages of 11.65 ± 0.52 Ma, 18.15 ± 0.46 Ma and 7.69 ± 0.05 Ma, respectively. 40Ar/39Ar 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 ± 0.20 Ma, 10.81 ± 0.15 Ma, and 7.37 ± 0.05 Ma, respectively. The age of the youngest fine‐grained diorite (Gunung Wayang dike) is 3.95 ± 0.03 Ma. An 40Ar/39Ar age obtained from adularia in the Arinem mineralized vein (18.30 ± 0.20 Ma) is older than the age of altered basalt sample of this study (11.65 ± 0.52 Ma) and the K–Ar illite ages of the Arinem vein (9.4 ± 0.3 Ma and 8.8 ± 0.3 Ma) 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.
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印度尼西亚西爪哇帕潘达延金属探区火山岩和侵入岩的40Ar/39Ar年代学
本文对印度尼西亚西爪哇省帕潘达扬金属区火山岩和侵入岩进行了40Ar/39Ar年龄的研究。Arinem地区脉系是该区找矿远景区之一,被认为是浅成低温热液型金银基金属矿床,但本区寄主火山岩年龄尚未公布。这些岩石的年龄对其与矿化的关系至关重要,对了解该地区火山作用的演化具有重要意义,这对该地区的矿产勘探具有重要意义。2个典型玄武岩样品和1个安山岩样品的40Ar/39Ar高原年龄分别为11.65±0.52 Ma、18.15±0.46 Ma和7.69±0.05 Ma。古农哈朗闪长岩、古农灵嘎闪长岩和古农布利格尔细粒石英闪长岩3个侵入岩样品的ar年龄分别为12.98±0.20 Ma、10.81±0.15 Ma和7.37±0.05 Ma。最年轻的细粒闪长岩(古农大阳岩脉)年龄为3.95±0.03 Ma。Arinem矿化脉的40Ar/39Ar年龄(18.30±0.20 Ma)高于本研究蚀变玄武岩样品的年龄(11.65±0.52 Ma)和Arinem脉的K-Ar伊利石年龄(9.4±0.3 Ma和8.8±0.3 Ma)。年龄结果表明,巴潘达延地区可能经历了多次热液成矿事件。因此,该研究为该区今后的矿产勘探提供了重要的年龄资料。
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来源期刊
Resource Geology
Resource Geology 地学-地质学
CiteScore
2.30
自引率
14.30%
发文量
18
审稿时长
12 months
期刊介绍: Resource Geology is an international journal focusing on economic geology, geochemistry and environmental geology. Its purpose is to contribute to the promotion of earth sciences related to metallic and non-metallic mineral deposits mainly in Asia, Oceania and the Circum-Pacific region, although other parts of the world are also considered. Launched in 1998 by the Society for Resource Geology, the journal is published quarterly in English, making it more accessible to the international geological community. The journal publishes high quality papers of interest to those engaged in research and exploration of mineral deposits.
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