Examination of chloritization of biotite as a tool for reconstructing the physicochemical parameters of mineralization and associated alteration in the Zafarghand porphyry copper system, Ardestan, Central Iran: mineral-chemistry and stable isotope analyses
文献类型:期刊论文
作者 | Yamini, Maryam Aminroayaei1; Tutti, Faramarz1; Yamini, Mohammad Reza Aminoroayaei2; Ahmadian, Jamshid3; Wan, Bo4,5 |
刊名 | MINERALOGY AND PETROLOGY
![]() |
出版日期 | 2017-10-01 |
卷号 | 111期号:5页码:747-759 |
关键词 | Porphyry copper Chloritized biotite Stable isotopes Zafarghand, Iran |
ISSN号 | 0930-0708 |
DOI | 10.1007/s00710-016-0486-7 |
文献子类 | Article |
英文摘要 | The chloritization of biotite and stable isotopes of silicate have been studied for the Zafarghand porphyry copper deposit, Ardestan, Iran. The studied area, in the central part of the Urumieh-Dokhtar magmatic belt, contains porphyry-style Cu mineralization and associated hydrothermal alteration within the Miocene (19-26 Ma, Zircon U-Pb age) granodioritc stock and adjacent andesitic to rhyodacitic volcanic rocks (ca. 56 Ma, zircon U-Pb age). The primary and secondary biotite that formed during potassic alteration in this porphyry and these volcanic host rocks are variably chloritized. Chloritization of biotite pseudomorphically is characterized by an increase in MgO, FeOt, and MnO, with decreasing in SiO2, K2O, and TiO2. Based on the Ti-in-biotite geothermometer of Henry et al. (Am Mineral 90:316-328, 2005) and Al-in-chlorite geothermometer of Cathelineau (Clay Miner 23:417-485, 1988), crystallization temperatures of primary biotite representative of magmatic conditions and later chloritization temperature range from 617A degrees to 675 A degrees C +/- 24 A degrees C and 177A degrees to 346 A degrees C, respectively. Calculated isotopic compositions of fluids that chloritized primary and secondary biotite display isotopic compositions of 1.1 to 1.7 per mil for delta O-18 and -19.9 to -20.5 per mil for delta D consistent with meteoric water. Sericite, barren, and A-type-quartz veins from phyllic alteration were produced by mixed magmatic and meteoric water with delta O-18 values from -2.8 to 2.5 and delta D values of similar to -23 per mil; the narrow range of delta D values of the propylitic epidote may be due to a meteoric water with delta O-18 values from 0.8 to 1.6 and delta D values from -14.6 to -16.9 per mil. |
WOS关键词 | POTASSIUM-SILICATE PROTORE ; HYDROGEN ISOTOPE ; HYDROTHERMAL ALTERATION ; FLUID INCLUSIONS ; GRANITIC-ROCKS ; KERMAN REGION ; OROGENIC BELT ; MASS-TRANSFER ; DEPOSIT ; WATER |
WOS研究方向 | Geochemistry & Geophysics ; Mineralogy |
语种 | 英语 |
WOS记录号 | WOS:000410742800006 |
出版者 | SPRINGER WIEN |
资助机构 | Strategic Priority Research Program (B) of the Chinese Academy of Sciences(XDB03010801) ; NSFC(41672085) ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences(XDB03010801) ; NSFC(41672085) ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences(XDB03010801) ; NSFC(41672085) ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences(XDB03010801) ; NSFC(41672085) |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/61918] ![]() |
专题 | 地质与地球物理研究所_岩石圈演化国家重点实验室 |
通讯作者 | Yamini, Maryam Aminroayaei |
作者单位 | 1.Univ Tehran, Sch Geol, Tehran, Iran 2.Isfahan Univ Technol, Min Dept, Esfahan, Iran 3.Payame Noor Univ, Dept Geol, Tehran, Iran 4.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China 5.Chinese Acad Sci, Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China |
推荐引用方式 GB/T 7714 | Yamini, Maryam Aminroayaei,Tutti, Faramarz,Yamini, Mohammad Reza Aminoroayaei,et al. Examination of chloritization of biotite as a tool for reconstructing the physicochemical parameters of mineralization and associated alteration in the Zafarghand porphyry copper system, Ardestan, Central Iran: mineral-chemistry and stable isotope analyses[J]. MINERALOGY AND PETROLOGY,2017,111(5):747-759. |
APA | Yamini, Maryam Aminroayaei,Tutti, Faramarz,Yamini, Mohammad Reza Aminoroayaei,Ahmadian, Jamshid,&Wan, Bo.(2017).Examination of chloritization of biotite as a tool for reconstructing the physicochemical parameters of mineralization and associated alteration in the Zafarghand porphyry copper system, Ardestan, Central Iran: mineral-chemistry and stable isotope analyses.MINERALOGY AND PETROLOGY,111(5),747-759. |
MLA | Yamini, Maryam Aminroayaei,et al."Examination of chloritization of biotite as a tool for reconstructing the physicochemical parameters of mineralization and associated alteration in the Zafarghand porphyry copper system, Ardestan, Central Iran: mineral-chemistry and stable isotope analyses".MINERALOGY AND PETROLOGY 111.5(2017):747-759. |
入库方式: OAI收割
来源:地质与地球物理研究所
浏览0
下载0
收藏0
其他版本
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。