An Experimental Study of the Formation of Talc through CaMg(CO3)(2)-SiO2-H2O Interaction at 100-200 degrees C and Vapor-Saturation Pressures
文献类型：期刊论文
| 作者 | Wan, Ye4; Wang, Xiaolin2,3,4; Chou, I-Ming1 ; Hu, Wenxuan(Nanjing Univ, Sch Earth Sci & Engn, State Key Lab Mineral Deposits Res, Nanjing 210023, Jiangsu, Peoples R China); Wang, Xiaolin(Nanjing Univ, Sch Earth Sci & Engn, State Key Lab Mineral Deposits Res, Nanjing 210023, Jiangsu, Peoples R China); Wang, Xiaoyu4; Zhang, Yang4; Hu, Wenxuan3,4
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| 刊名 | GEOFLUIDS
 |
| 出版日期 | 2017 |
| DOI | 10.1155/2017/3942826 |
| 产权排序 | 第1完成单位 ; 第2完成单位 ; 第3完成单位 ; 第4完成单位 |
| 文献子类 | Article |
| 英文摘要 | The metamorphic interaction between carbonate and silica-rich fluid is common in geological environments. The formation of talc from dolomite and silica-rich fluid occurs at low temperatures in the metamorphism of the CaO-MgO-SiO2-CO2-H2O system and plays important roles in the formation of economically viable talc deposits, the modification of dolomite reservoirs, and other geological processes. However, disagreement remains over the conditions of talc formation at low temperatures. In this study, in situ Raman spectroscopy, quenched scanning electron microscopy, micro-X-ray diffraction, and thermodynamic calculations were used to explore the interplay between dolomite and silica-rich fluids at relatively low temperatures in fused silica tubes. Results showed that talc formed at <= 200 degrees C and low CO2 partial pressures (PCO2). The reaction rate increased with increasing temperature and decreased with increasing PCO2. The major contributions of this study are as follows: (1) we confirmed the formation mechanism of Mg-carbonate-hosted talc deposits and proved that talc can form at <= 200 degrees C; (2) the presence of talc in carbonate reservoirs can indicate the activity of silica-rich hydrothermal fluids; and (3) the reactivity and solubility of silica require further consideration, when a fused silica tube is used as the reactor in high P-T experiments. |
| URL标识 | 查看原文 |
| WOS关键词 | SAN-ANDREAS FAULT ; RAMAN-SPECTROSCOPIC CHARACTERIZATION ; THERMOCHEMICAL SULFATE REDUCTION ; AMORPHOUS SILICA SOLUBILITIES ; FLUID INCLUSIONS ; DEGREES-C ; HYDROTHERMAL ALTERATION ; ISOTOPE GEOCHEMISTRY ; AQUEOUS-SOLUTIONS ; CARBONATE RESERVOIRS |
| 语种 | 英语 |
| WOS记录号 | WOS:000405781300001 |
| 源URL | [http://ir.idsse.ac.cn/handle/183446/3959]  |
| 专题 | 深海科学研究部_深海极端环境模拟研究实验室 |
| 通讯作者 | Wang, Xiaolin; Hu, Wenxuan(Nanjing Univ, Sch Earth Sci & Engn, State Key Lab Mineral Deposits Res, Nanjing 210023, Jiangsu, Peoples R China); Wang, Xiaolin(Nanjing Univ, Sch Earth Sci & Engn, State Key Lab Mineral Deposits Res, Nanjing 210023, Jiangsu, Peoples R China); Hu, Wenxuan |
| 作者单位 | 1.Chinese Acad Sci, Inst Deep Sea Sci & Engn, Lab Expt Study Deep Sea Extreme Condit, Sanya 572000, Hainan, Peoples R China 2.Shandong Univ Sci & Technol, Shandong Prov Key Lab Deposit Mineralizat & Sedim, Qingdao 266510, Shandong, Peoples R China 3.Nanjing Univ, Inst Energy Sci, Nanjing 210023, Jiangsu, Peoples R China 4.Nanjing Univ, Sch Earth Sci & Engn, State Key Lab Mineral Deposits Res, Nanjing 210023, Jiangsu, Peoples R China |
| 推荐引用方式 GB/T 7714 | Wan, Ye,Wang, Xiaolin,Chou, I-Ming,et al. An Experimental Study of the Formation of Talc through CaMg(CO3)(2)-SiO2-H2O Interaction at 100-200 degrees C and Vapor-Saturation Pressures[J]. GEOFLUIDS,2017. |
| APA | Wan, Ye.,Wang, Xiaolin.,Chou, I-Ming.,Hu, Wenxuan.,Wang, Xiaolin.,...&Hu, Wenxuan.(2017).An Experimental Study of the Formation of Talc through CaMg(CO3)(2)-SiO2-H2O Interaction at 100-200 degrees C and Vapor-Saturation Pressures.GEOFLUIDS. |
| MLA | Wan, Ye,et al."An Experimental Study of the Formation of Talc through CaMg(CO3)(2)-SiO2-H2O Interaction at 100-200 degrees C and Vapor-Saturation Pressures".GEOFLUIDS (2017). |
入库方式： OAI收割
来源：深海科学与工程研究所
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