Journal of Jilin University(Earth Science Edition) ›› 2019, Vol. 49 ›› Issue (6): 1591-1606.doi: 10.13278/j.cnki.jjuese.20190125

Previous Articles     Next Articles

Mineralogical Characteristics and Genetic Mechanism of Turquoise Deposit in Bijiashan Area in Anhui Province

Shen Chonghui1, Zhao Enquan2   

  1. 1. School of Earth Science and Resources, China University of Geosciences, Beijing 100083, China;
    2. Langfang Natural Resources Integrated Survey Center, China Geological Survey, Langfang 065000, Hebei, China
  • Received:2019-06-21 Published:2019-11-30
  • Supported by:
    Supported by National Natural Science Foundation of China (41872209)

Abstract: A typical turquoise mineralization belt is distributed in Ma'anshan City of Anhui Province. The genesis of these turquoise deposits remains controversial. In this study, a detailed field geological survey and indoor observation of the Bijiashan turquoise deposits were carried out. The mineralogy and petro-chemistry of the turquoise minerals were analyzed by using microscope, electron probe, SEM, ICP-MS and other methods. The main minerals of Bijiashan turquoise deposit consist of turquoise with a small amount of quartz, pyrite, feldspars, pyrophyllite, limonite and jarosite. Turquoise is microcrystalline aggregate with gelatinous structure. The SEM micromorphology shows that the platelike crystallite aggregates of turquoise are parallel or staggered. The symbiotic pyrites with turquoise are characterized by medium-low temperature hydrothermal cubes, pentagonal dodecahedron and polymorphic crystal. In the chart of Co-Ni content relationship, the samples mainly distributed in magma and hydrothermal area. The δ34S isotope ranges from 8.3‰ to 11.9 ‰, which indicates that the sulphur was derived from a deep magmatic and sedimentary source, and the ore-forming fluid was formed by mixed atmospheric precipitation and deep magmatic water. Combined with the mineral assemblage, mineral forming sequence, symbiotic pyrite mineralization, and ore-forming fluid, Bijiashan turquoise deposit is a medium-low temperature hydrothermally metasomatic deposit formed by volcanic eruption.

Key words: Bijiashan turquoise deposit, turquoise, mineralogy, isotope, hydrothermal alliteration, genesis of deposit

CLC Number: 

  • P619.2
[1] 魏道贵,管荣华. 马鞍山地区绿松石矿的分布、成因及标志[J].矿业快报, 2003(10):19-20. Wei Daogui, Guan Ronghua. Distribution, Genesis and Signs of Turquoise Deposits in Ma'anshan Area[J]. Express Information of Mining Industry, 2003(10):19-20.
[2] 岳德银. 安徽马鞍山地区假象绿松石的研究[J].岩石矿物学杂志,1995,14(1):79-83. Yue Deyin. A Study of Pseudomorphic Turquoise from Maanshan Area, Auhui Province[J]. Acta Petrologica et Mineralogical,1995,14(1):79-83.
[3] 王华田,章纯荪,贺菊瑞. 宁芜、卢枞火山岩地区几种表生磷酸盐矿物特征及形成机理[J].矿物学报,1990,10(1):58-65. Wang Huatian, Zhang Chunsun, He Jurui. Mineralogical Features and Genetic Mechanism of Some Hypergene Phosphates in Nanjing-Wuhu and Lujiang-Zongyang Volcanic Areas[J]. Acta Mineralogical Sinica,1990,10(1):58-65.
[4] 张青,戴慧,阳珊,等. 安徽马鞍山假象绿松石、磷铝石成因探讨[J].安徽地质,2016, 26(2):153-157. Zhang Qing, Dai Hui, Yang Shan, et al. On the Origin of Pseudomorphic Turquoise and Variscite in Ma'anshan,Anhui[J]. Geology of Anhui,2016, 26(2):153-157.
[5] 杨晓勇,王奎仁,刘向华.马鞍山地区不同类型绿松石稀土元素地球化学研究[J].稀土,1997,18(4):1-3,29. Yang Xiaoyong, Wang Kuiren, Liu Xianghua. Rare Earth Element Geochemistry of the Different Types of Turquoise from Ma'anshan Area[J]. Chinese Rare Earths, 1997,18(4):1-3,29.
[6] 施德兰,邱泳昱,孔维斌.安徽省马鞍山市大黄山绿松石、自然铜矿初步调查研究报告[R].马鞍山:安徽省地质矿产局情报中心,1998:1-19. Shi Delan, Qiu Yongyu, Kong Weibin.Preliminary Investigation Report on Turquoise and Natural Copper Deposits in Dahuang Mountain, Ma'anshan City[R]. Ma'anshan:Information Center of Geology and Mineral Resources Bureau of Anhui Provinces, 1998:1-19.
[7] 陈全莉,张琰. 具磷灰石假象绿松石的宝石矿物学特征[J].宝石和宝石学杂志, 2005,7(4):13-16. Chen Quanli, Zhang Yan. Features of Gem-Mineralogy of Apatite-Pseudomorphic Turquoise[J]. Journal of Gems and Gemmology, 2005,7(4):13-16.
[8] 陈全莉,亓利剑. 马鞍山绿松石中水的振动光谱表征及其意义[J].矿物岩石, 2007,27(1):30-35. Chen Quanli,Qi Lijian. Study of the Vibrational Spectra Characters of Water in Turquoise from Maanshan[J].Journal of Mineralogy and Petrology, 2007,27(1):30-35.
[9] 陈全莉,亓利剑,袁心强,等. 具磷灰石假象绿松石的热性能[J].地球科学:中国地质大学学报, 2007,33(3):416-422. Chen Quanli, Qi Lijian, Yuan Xinqiang, et al. Thermal Property of the Apatite Pseudomorphic Turquoise[J]. Earth Science:Journal of China University of Geosciences, 2007,33(3):416-422.
[10] 佘玲珠,秦颍,冯敏,等.绿松石显微拉曼光谱及产地意义初步分析[J].光谱学与光谱分析, 2008,28(9):2107-2110. She Lingzhu, Qin Ying, Feng Min,et al. A Primary Raman Microscopic Study of the Turquoise and Its Role in Provenance-Tracking[J].Spectroscopy and Spectral Analysis, 2008,28(9):2107-2110.
[11] 周彦,亓利剑,戴慧,等. 安徽殿庵山绿松石的宝石学特征研究[J].宝石和宝石学杂志, 2013,15(4):37-45. Zhou Yan, Qi Lijian, Dai Hui, et al. Study on Gemmological Characteristics of Turquoise from Diananshan, Anhui Province[J].Journal of Gems & Gemmology, 2013,15(4):37-45.
[12] 杨力乙. 安徽笔架山绿松石谱学特征及呈色机制研究[D].武汉:中国地质大学, 2013. Yang Liyi. Spectrum Characteristics and Color-Forming Mechanism of Bijiashan Turquoise in Anhui Province[D].Wuhan:China University of Geosciences, 2013.
[13] 王金云,施德兰,钱统丁,等. 安徽省马鞍山市笔架山外围绿松石矿详查地质报告[R].马鞍山:安徽省地质矿产勘查局322地质队, 2011:1-25. Wang Jinyun, Shi Delan, Qian Tongding, et al. Detailed Geological Report of Turquoise Deposits in the Periphery of Bijia Mountain Ma'anshan City, Anhui Province[R]. Ma'anshan:No 322 Geological Team,Bureau of Geology and Mineral Reasources of Anhui Province,2011:1-25.
[14] 张惠芬,林传易,马中玮,等. 绿松石的某些磁性、光谱特性和颜色的研究[J].矿物学报,1982,2(4):254-261. Zhang Huifen, Lin Chuanyi, Ma Zhongwei, et al.Magentic Properties, Characteristic Spectra and Colour of Turquoise[J].Acta Mineralogica Sinica,1982,2(4):254-261.
[15] 宁芜研究项目编写小组. 宁芜玢岩铁矿[M].北京:地质出版社,1978. Ningwu Research Project Writing Group. Iron Ore Deposits Associated with Porphyrites[M]. Beijing:Geological Publishing House,1978.
[16] 赵玉琛. 宁芜马山式黄铁矿床的地质特征和成因探讨[J].化工矿产地质,1993,15(3):169-177. Zhao Yuchen. Geological Characteristic and Genetic Exploration of Mashan Type Pyrite Ore Deposit in Ningwu Area[J]. Geology of Chemical Minerals, 1993,15(3):169-177.
[17] 赵玉琛. 宁芜向山式黄铁矿床的地质特征和成因[J].化工矿产地质,1995,17(3):182-190. Zhao Yuchen. Geological Characteristics and Origination of Xiangshan-Type Pyrite Deposits Across Nanjing-Wuhu Region[J].Geology of Chemical Minerals,1995,17(3):182-190.
[18] 朱立新. 凹山铁矿床黄铁矿的赋存状态及成因机理[J].现代矿业,2002(20):5-6. Zhu Lixin. Occurrence State and Formation Mechanism of Pyrite in Washan Iron Deposit[J]. Express Information of Mining Industry, 2002(20):5-6.
[19] 李荫清,魏家秀,周兴汉,等. 某玢岩铁矿床中气液包裹体特征和成矿温度[J].地质学报,1979,53(1):53-96. Li Yinqing, Wei Jiaxiu,Zhou Xinghan, et al. Some Features of the Fluid Inclusions and the Ore-Forming Temperature of a Certain Porphyrite-Type Iron Deposit[J]. Acta Geological Sinica, 1979,53(1):53-96.
[20] 万宏. 凹山矿田铁硫矿床黄铁矿标型特征探讨[J].化工矿产地质,1983,5(2):32-39. Wan Hong. Discussion on the Typomorphic Characteristics of Pyrite in the Iron Ore Deposit, Washan Ore Field[J]. Geology of Chemical Minerals,1983,5(2):32-39.
[21] 熊先孝,姚超美. 向山地区铁、硫矿床中黄铁矿矿物学研究[J].岩石矿物学杂志,2000,19(2):185-192. Xiong Xianxiao, Yao Chaomei. Mineralogy of Pyrites from the Xiangshan Iron and Pyrite Deposits, Anhui Province[J]. Acta Petrologica et Mineralogica, 2000,19(2):185-192.
[22] 童潜明. 黄铁矿的钴、镍比值对矿床成因意义的讨论[J].矿产与地质,1986(3):8-11. Tong Qianming. Discussion on the Significance of Cobalt and Nickel Ratio of Pyrite to the Genesis of Deposits[J]. Mineral Resources and Geology, 1986(3):8-11.
[23] Bajwah Z U, Seccombe P K, Offler R. Trace Element Distribution, Co:Ni Ratios and Genesis of the Big Cadia Iron-Copper Deposit, New South Wales, Australia[J].Mineralium Deposita,1987,22(4):292-300.
[24] 盛继福,李岩,范书义.大兴安岭中段铜多金属矿床矿物微量元素研究[J].矿床地质,1999,18(2):153-160. Sheng Jifu, Li Yan, Fan Shuyi. A Study of Minor Elements in Minerals from Polymetallic Deposits in the Central Part of the Da Hinggan Mountains[J]. Mineral Deposits, 1999,18(2):153-160.
[25] Ohmoto H. Systematics of Sulfur and Carbon Isotopes in Hydrothermal Ore Deposits[J]. Economic Geology,1972,67(5):551-578.
[26] 代军治, 高菊生, 钱壮志,等. 小秦岭镰子沟金矿床地质特征、黄铁矿原位硫同位素组成及成因意义[J].吉林大学学报(地球科学版), 2018, 48(6):63-76. Dai Junzhi, Gao Jusheng, Qian Zhuangzhi, et al. Geological Characteristics and S Isotopic Compositions of Pyrite from Lianzigou Gold Deposit in Xiaoqinling Area, and It's Genetic Significance[J].Journal of Jilin University (Earth Science Edition), 2018, 48(6):63-76.
[27] 郝立波, 赵昕, 赵玉岩. 辽宁白云金矿床稳定同位素地球化学特征及矿床成因[J]. 吉林大学学报(地球科学版), 2017,47(2):442-451. Hao Libo, Zhao Xin, Zhao Yuyan. Stable Isotope Characteristics and Ore Genesis of the Baiyun Gold Deposit, Liaoning Province[J]. Journal of Jilin University (Earth Science Edition), 2017, 47(2):442-451.
[28] 郑永飞. 矿物稳定同位素地球化学研究[J].地学前缘,2000,7(2):299-320. Zheng Yongfei. Geochemical Studies of Stable Isotopes in Minerals[J]. Earth Science Frontiers, 2000,7(2):299-320.
[29] 陕亮,郑有业,许荣科,等. 硫同位素示踪与热液成矿作用研究[J].地质与资源,2009,18(3):197-203. Shan Liang, Zheng Youye,Xu Rongke, et al. Review on Sulfur Isotopic Tracing and Hydrothermal Metallogenesis[J]. Geology and Resources, 2009,18(3):197-203.
[30] 修世荫.宁芜火山断陷盆地黄铁矿床成矿物质来源、成矿区划及找矿方向[J].化工矿产地质,1993,15(3):178-185. Xiu Shiyin. The Sources of Ore-Forming Material, Metallogenetic Subdivision and Ore-Prospecting Targets of the Pyrite Deposits in Ningwu Faulted Volcanic Basin[J]. Geology of Chemical Minerals, 1993,15(3):178-185.
[31] 张成.宁芜盆地梅山铁矿床地质地球化学特征及矿床成因研究[D].北京:中国地质大学(北京),2012. Zhang Cheng. Geological and Geochemical Characteristics and Genesis of Meishan Iron Deposit in Ningwu Basin[D]. Beijing:China University of Geosciences (Beijing),2012.
[32] 张荣华, 盛继福,陆成庆. 庐枞火山岩盆地的矿化蚀变与矿质来源[J].中国地质科学院矿床地质研究所所刊, 1982,4(2):51-64. Zhang Ronghua, Sheng Jifu, Lu Chengqing. The Mineralizing Alteration and the Source of Ore-Forming Materials at Luzong Volcanic Basin[J]. Bulletin of the Institute of Mineral Deposits Chinese Academy of Geological Sciences, 1982,4(2):51-64.
[33] 袁野,施光海. 江西上饶龙门高岭石-叶蜡石矿的矿物组成及稳定同位素特征[J].地球学报,2012, 33(2):176-184. Yuan Ye, Shi Guanghai. Mineral Components and Stable Isotope Compositions of the Longmen Kaolinite-Pyrophyllite Deposit in Shangrao, Jiangxi Province[J]. Acta Geoscientica Sinica, 2012,33(2):176-184.
[34] Anovitz L M, Perkins D, Essene E J. Metastability in Near-Surface Rocks of Minerals in the System Al2O3-SiO2-H2O[J]. Clay and Clay Minerals,1991,39(3):225-233.
[35] Hemley J J, Montoya J W, Marinenko J W, et al. Equilibria in the System Al2O3-SiO2-H2O and Some General Implications for Alteration/Mineralization Processes[J]. Economic Geology, 1980,75(2):210-228.
[1] Long Tianxiang, He Xiaohu, Liu Fei, Li Zongyong, Wang Yuchao, Zhao Jun, Li Yunfei, Wang Changbing, Cao Yuan. Zircon U-Pb Geochronology, Trace Element, Hf Isotope of Alkaline Rocks from Chang'an Gold Deposit and Its Geological Implication [J]. Journal of Jilin University(Earth Science Edition), 2019, 49(6): 1607-1627.
[2] Jia Yinggang, Zhao Jun, Jiang Lei, Guan Liwei, Wang Xiaoxuan, He Liang. Early Paleozoic Tectonic Evolution of Northern Yili Block: Evidence from Diorite in Wenquan, Xinjiang [J]. Journal of Jilin University(Earth Science Edition), 2019, 49(4): 1015-1038.
[3] Dong Jinkun, Yang Mei, Wu Zhiyuan, Qin Shan, Wang Yuwei. Systematic Mineralogy Data Characteristics and Database Construction [J]. Journal of Jilin University(Earth Science Edition), 2019, 49(3): 727-736.
[4] Su Xiaosi, Gao Ruimin, Yuan Wenzhen, Lu Shuai, Su Dong, Zhang Lihua, Meng Xiangfei, Zuo Ende. Research on River Recharge Based on Environmental Isotope Technology: A Case Study of Huangjia Riverside Well Field in Shenyang City [J]. Journal of Jilin University(Earth Science Edition), 2019, 49(3): 762-772.
[5] Lu Qian, Sun Jinggui, An Jiuhai, Han Jilong, Chu Xiaolei. Petrogenesis and Forming Environment of Mesozoic Porphyritic Granite in Songjianghe Region of Dunhua,Jilin Province: Evidences from Element Geochemistry,Hf Isotope and U-Pb [J]. Journal of Jilin University(Earth Science Edition), 2019, 49(3): 673-689.
[6] Wu Xichang, Chu Fengyou, Wang Wei, Li Zhenggang, Chen Ling, Bi Dongwei, Wang Jianqiang. Recognition of Subduction Melt and Fluid Component in Lau and Manus Basins: Sr-Nd-Pb Isotope Ratios and Independent Component Analysis [J]. Journal of Jilin University(Earth Science Edition), 2019, 49(2): 414-424.
[7] Wu Yongtao, Han Runsheng. C, O, Sr Isotope and REE Geochemistry of Maozu Pb-Zn Deposit in Northeastern Yunnan Mineral Concentration Area [J]. Journal of Jilin University(Earth Science Edition), 2019, 49(2): 400-413.
[8] Wang Taoli, Wang Qingtao, Liu Wenping, Lu Hong, Liu Dayong. Quantitative Method of Crushed Gas in Shale and Its Geological Significance [J]. Journal of Jilin University(Earth Science Edition), 2018, 48(6): 1645-1653.
[9] Zhang Peng, Kou Linlin, Zhao Yan, Bi Zhongwei. Zircon U-Pb Age and Hf Isotopic Composition of the Biotite Plagioclase Hornblende Gneiss of Shujigou Cu-Zn Deposit, Liaoning Province [J]. Journal of Jilin University(Earth Science Edition), 2018, 48(5): 1365-1377.
[10] Wu Meng, Li Yixin, Liu Guixiang. Characteristics of Ore-Forming Fluid and Genesis of Laozuoshan Gold Deposit, Heilongjiang [J]. Journal of Jilin University(Earth Science Edition), 2018, 48(5): 1353-1364.
[11] Dai Jiaqi, Li Guangrong, Guo Fusheng, Wang Chao, Wang Zhe, Zhang Wanliang, Yu Yushuai. Chemical Components and Boron Isotopic Composition of Tourmaline of Uranium Bearing Porphyroclastic Lava in Xiangshan, Jiangxi [J]. Journal of Jilin University(Earth Science Edition), 2018, 48(5): 1378-1393.
[12] Zhang Qiang, Ding Qingfeng, Song Kai, Cheng Long. Detrital Zircon U-Pb Geochronology and Hf Isotope of Phyllite of Langyashan Formation in Hongshuihe Iron Ore District of Eastern Kunlun and Their Geological Significance [J]. Journal of Jilin University(Earth Science Edition), 2018, 48(4): 1085-1104.
[13] He Xiaolong, Zhang Da, Chen Guohua, Di Yongjun, Huo Hailong, Li Ning, Zhang Zhihui, Rao Jianfeng, Wei Jin, Ouyang Yongpeng. Genesis of Zhuxi Copper-Tungsten Deposit in Jiangxi Province: Insights from Mineralogy and Chronology [J]. Journal of Jilin University(Earth Science Edition), 2018, 48(4): 1050-1070.
[14] Qi Fanyu, Zhang Zhi, Zhu Xinyou, Li Yongsheng, Zhen Shimin, Gong Fanying, Gong Xiaodong. Mineral Characteristics and Geological Significance of the Baoshan Cu-Pb-Zn Polymetallic Deposit in Hunan Province [J]. Journal of Jilin University(Earth Science Edition), 2018, 48(3): 754-768.
[15] Chen Ruili, Chen Zhengle, Wu Junjie, Liang Zhilu, Han Fengbin, Wang Yong, Xiao Changhao, Wei Liangxi, Shen Tao. Fluid Inclusions and S-Pb Isotopes in Zaozigou Gold Deposit, Hezuo in Gansu Province [J]. Journal of Jilin University(Earth Science Edition), 2018, 48(1): 87-104.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
No Suggested Reading articles found!