Geochemical studies on Permian manganese deposits in Guichi, eastern China: Implications for their origin and formative environments
文献类型:期刊论文
作者 | Xie, Jiancheng1,2; Sun, Weidong1; Du, Jianguo3; Xu, Wei3; Wu, Libing3; Yang, Xiaoyong4; Zhou, Taofa2 |
刊名 | JOURNAL OF ASIAN EARTH SCIENCES |
出版日期 | 2013-09-25 |
卷号 | 74期号:S1页码:155-166 |
ISSN号 | 1367-9120 |
关键词 | Permian manganese deposit Sedimentary environment Hydrothermal Source of manganese Guichi region |
英文摘要 | Permian manganese ore deposits are widely distributed in southwestern and eastern China. Guichi Permian manganese district in southern Anhui Province, central eastern China, is currently the most important manganese metal producers in eastern China. Manganese ores (MnO = 18.2-45.4 wt.%) in Guichi region occur in calcareous, argillaceous and siliceous Mn-bearing sequence of the Permian Gufeng Formation. In contrast to Mn-bearing rocks, the ores have higher Mn, Fe, P, Sr (more than 1500 ppm) and Ni contents (>480 ppm), higher Mn/Fe (>5) and La-n/Ce-n (>2) values, and lower Co/Ni (<0.05) ratios. The Guichi manganese deposits also have low Co/Ni (<1) and Co/Zn ratios, low in total REE contents (mostly < 100 ppm) with negative Eu (0.46-0.75) and Ce (0.42-0.76) anomalies. The mineralogy and geochemistry of manganese deposits in the Guichi region strongly indicate hydrothermal activities, which is supported by high paleotemperatures (49-71 degrees C) of Permian Mn-carbonate ore and Mn-bearing carbonate. The low Ce-anom. values (<-0.1) and high strontium contents indicate that the Guichi manganese deposits were formed in high-salinity and oxidative marine sedimentary environment. The Al2O3/TiO2 (9.23-48.2) and Y/Ho (25.9-44.4) ratios, REE patterns, delta C-13(V-PDB) (-10.2 parts per thousand to 5.00 parts per thousand) and delta O-18(SMOW) (20.7-28.0 parts per thousand characteristics of Permian manganese deposits reveal a mixed Mn source of volcanic, terrigenous and organic matter. (C) 2013 Elsevier Ltd. All rights reserved. |
WOS标题词 | Science & Technology ; Physical Sciences |
类目[WOS] | Geosciences, Multidisciplinary |
研究领域[WOS] | Geology |
关键词[WOS] | RARE-EARTH-ELEMENTS ; OXYGEN-ISOTOPE COMPOSITION ; YANGTZE-RIVER BELT ; RIDGE SUBDUCTION ; FERROMANGANESE DEPOSITS ; HYDROTHERMAL ORIGIN ; SHAANXI PROVINCE ; STABLE-ISOTOPE ; OXIDE DEPOSITS ; PACIFIC-OCEAN |
收录类别 | SCI |
语种 | 英语 |
WOS记录号 | WOS:000324663500013 |
公开日期 | 2014-10-14 |
源URL | [http://ir.gig.ac.cn:8080/handle/344008/19022] |
专题 | 中国科学院广州地球化学研究所 |
作者单位 | 1.Chinese Acad Sci, Guangzhou Inst Geochem, CAS Key Lab Mineral & Metallogeny, Guangzhou 510640, Guangdong, Peoples R China 2.Hefei Univ Technol, Sch Resource & Environm Sci, Hefei 230009, Peoples R China 3.Anhui Acad Geol Survey, Hefei 230001, Peoples R China 4.Univ Sci & Technol China, Sch Earth & Space Sci, CAS Key Lab Crust Mantle Mat & Environm, Hefei 230026, Peoples R China |
推荐引用方式 GB/T 7714 | Xie, Jiancheng,Sun, Weidong,Du, Jianguo,et al. Geochemical studies on Permian manganese deposits in Guichi, eastern China: Implications for their origin and formative environments[J]. JOURNAL OF ASIAN EARTH SCIENCES,2013,74(S1):155-166. |
APA | Xie, Jiancheng.,Sun, Weidong.,Du, Jianguo.,Xu, Wei.,Wu, Libing.,...&Zhou, Taofa.(2013).Geochemical studies on Permian manganese deposits in Guichi, eastern China: Implications for their origin and formative environments.JOURNAL OF ASIAN EARTH SCIENCES,74(S1),155-166. |
MLA | Xie, Jiancheng,et al."Geochemical studies on Permian manganese deposits in Guichi, eastern China: Implications for their origin and formative environments".JOURNAL OF ASIAN EARTH SCIENCES 74.S1(2013):155-166. |
入库方式: OAI收割
来源:广州地球化学研究所
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