The Age and Origin of the Ruwai Polymetallic Skarn Deposit, Indonesia: Evidence of Cretaceous Mineralization in the Central Borneo Metallogenic Belt
文献类型：期刊论文
| 作者 | Dana, Cendi D. P.12,13; Agangi, Andrea12; Idrus, Arifudin11; Chelle-Michou, Cyril10; Lai, Chun-Kit8,9; Ishida, Mizuki7; Guillong, Marcel10; Gonzalez-Alvarez, Ignacio5,6; Takahashi, Ryohei12; Yano, Moei3,4 |
| 刊名 | ECONOMIC GEOLOGY
 |
| 出版日期 | 2023-09-01 |
| 卷号 | 118期号:6页码:1341-1370 |
| ISSN号 | 0361-0128 |
| DOI | 10.5382/econgeo.5009 |
| 英文摘要 | The Ruwai skarn deposit is the largest polymetallic skarn deposit in Borneo and is located in the Schwaner Mountains. The skarns and massive orebodies are hosted in marble of the Jurassic Ketapang Complex, which was intruded by Cretaceous Sukadana granitoids. The prograde-stage garnet and retrograde-stage titanite yielded U-Pb ages of 97.0 +/- 1.8 to 94.2 +/- 10.3 Ma and 96.0 +/- 2.9 to 95.0 +/- 2.0 Ma, respectively. These ages are similar to Re-Os ages obtained on sulfides (96.0 +/- 2.3 Ma) and magnetite (99.3 +/- 3.6 Ma). The U-Pb zircon ages reveal that magmatism at Ruwai occurred in three phases, including the Early Cretaceous (ca. 145.7 and 106.7- 105.7 Ma; andesite-dacite), Late Cretaceous (ca. 99.7-97.1 Ma; diorite-granodiorite), and late Miocene (ca. 10.94-9.51 Ma; diorite-dolerite). Based on geochemical and stable isotopic data (C-O-S) the Ruwai skarn ores are interpreted to have formed from oxidized fluids at ca. 160 to 670 degrees C. The ore-forming fluids and metals were mostly magmatic in origin but with significant crustal input. Ruwai skarn mineralization occurred in the Late Cretaceous, associated with Paleo-Pacific subduction beneath Sundaland after the Southwest Borneo accretion. Ruwai is the first occurrence of Cretaceous mineralization recognized in the Central Borneo metallogenic belt. |
| WOS研究方向 | Geochemistry & Geophysics ; Mineralogy |
| 语种 | 英语 |
| WOS记录号 | WOS:001085009900002 |
| 源URL | [http://ir.gig.ac.cn/handle/344008/78705]  |
| 专题 | 同位素地球化学国家重点实验室 |
| 通讯作者 | Dana, Cendi D. P. |
| 作者单位 | 1.PT Kapuas Prima Coal Tbk, North Jakarta 14460, Indonesia 2.Chinese Acad Sci, Guangzhou Inst Geochem, State Key Lab Isotope Geochem, Guangzhou, Peoples R China 3.Univ Tokyo, Sch Engn, Frontier Res Ctr Energy & Resources, Tokyo 1138656, Japan 4.Chiba Inst Technol, Ocean Resources Res Ctr Next Generat, Chiba 2750016, Japan 5.Univ Western Australia, Ctr Explorat Targeting, Perth, WA 6009, Australia 6.CSIRO, Discovery Program, Mineral Resources, Perth, WA 6151, Australia 7.Univ Tokyo, Sch Engn, Dept Syst Innovat, Tokyo 1138656, Japan 8.Univ Brunei Darussalam, Fac Sci, BE-1410 Gadong, Brunei 9.Fortescue Met Grp Ltd, Global Project Generat & Targeting, East Perth, WA 6004, Australia 10.Swiss Fed Inst Technol, Dept Earth Sci, CH-8092 Zurich, Switzerland |
| 推荐引用方式 GB/T 7714 | Dana, Cendi D. P.,Agangi, Andrea,Idrus, Arifudin,et al. The Age and Origin of the Ruwai Polymetallic Skarn Deposit, Indonesia: Evidence of Cretaceous Mineralization in the Central Borneo Metallogenic Belt[J]. ECONOMIC GEOLOGY,2023,118(6):1341-1370. |
| APA | Dana, Cendi D. P..,Agangi, Andrea.,Idrus, Arifudin.,Chelle-Michou, Cyril.,Lai, Chun-Kit.,...&Xia, Xiao-Ping.(2023).The Age and Origin of the Ruwai Polymetallic Skarn Deposit, Indonesia: Evidence of Cretaceous Mineralization in the Central Borneo Metallogenic Belt.ECONOMIC GEOLOGY,118(6),1341-1370. |
| MLA | Dana, Cendi D. P.,et al."The Age and Origin of the Ruwai Polymetallic Skarn Deposit, Indonesia: Evidence of Cretaceous Mineralization in the Central Borneo Metallogenic Belt".ECONOMIC GEOLOGY 118.6(2023):1341-1370. |
入库方式： OAI收割
来源：广州地球化学研究所
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