大兴安岭南段黄岗矽卡岩型铁锡多金属矿床蚀变矿化特征及其成因

梅微; 吕新彪; 王祥东; 范谢均; 魏巍

doi:10.3799/dqkx.2020.298

Volume 45 Issue 12

Dec. 2020

Turn off MathJax

Article Contents

Article Navigation > Earth Science > 2020 > 45(12): 4428-4445

Mei Wei, Lü Xinbiao, Wang Xiangdong, Fan Xiejun, Wei Wei, 2020. Alteration, Mineralization and Genesis of Huanggang Skarn Iron-Tin Polymetallic Deposit, Southern Great Xing'an Range. Earth Science, 45(12): 4428-4445. doi: 10.3799/dqkx.2020.298

Citation:

Mei Wei, Lü Xinbiao, Wang Xiangdong, Fan Xiejun, Wei Wei, 2020. Alteration, Mineralization and Genesis of Huanggang Skarn Iron-Tin Polymetallic Deposit, Southern Great Xing'an Range. Earth Science, 45(12): 4428-4445. doi: 10.3799/dqkx.2020.298

Citation:

Mei Wei, Lü Xinbiao, Wang Xiangdong, Fan Xiejun, Wei Wei, 2020. Alteration, Mineralization and Genesis of Huanggang Skarn Iron-Tin Polymetallic Deposit, Southern Great Xing'an Range. Earth Science, 45(12): 4428-4445. doi: 10.3799/dqkx.2020.298

PDF( 13830 KB)

Alteration, Mineralization and Genesis of Huanggang Skarn Iron-Tin Polymetallic Deposit, Southern Great Xing'an Range

doi: 10.3799/dqkx.2020.298

Mei Wei^{1
,
,},
Lü Xinbiao^{1, 2},
Wang Xiangdong³,
Fan Xiejun²,
Wei Wei¹

1.
Institute of Geological Survey, China University of Geosciences, Wuhan 430074, China
2.
School of Earth Resources, China University of Geosciences, Wuhan 430074, China
3.
Wuhan Center of Geological Survey, CGS, Wuhan 430205, China

Received Date: 2020-07-20
Publish Date: 2020-12-15

Abstract

Abstract

The Huanggang iron-tin polymetallic deposit in the southern Great Xing'an Range is characterized by alteration-mineralization features, which is of great significance to study the ore-forming process of skarn deposit. In this paper, it makes the Electron Probe Micro-analysis (EPMA) on typical alteration minerals and metallic minerals. The results indicate that hydrothermal evolution in the study area has experienced four stages. The prograde skarn stage (Ⅰ): the minerals are mainly grossular (GrtⅡ) with the andradite (GrtⅠ) core and hedenbergite. The retrograde skarn stage (Ⅱ): the minerals are mainly Fe-rich garnet (GrtⅢ), disseminated magnetite and hydrated minerals. The oxide stage (Ⅲ): the minerals are represented by a large amount of magnetite, cassiterite, a small amount of andradite (GrtⅣ) and diopside. The sulfide stage (Ⅳ): the minerals are a small amount of magnetites which are replaced by later sulfides, developing arsenopyrite, pyrite, chalcopyrite, iron-rich sphalerite, light-colored sphalerite-chalcopyrite-isostannite solid solution, and antimony-bearing tetrahedrite. It makes clear that the source of main metallogenic stage from the Huanggang skarn iron polymetallic deposit is magmatic fluid, metasomatic fluid to mixing of meteoric water, fluid compositions change complex, fluid evolution is characterized by the temperature decreased, the water/rock ratio increases gradually, and reducing to oxidizing to reducing.
- southern Great Xing'an Range,
- Huanggang deposit,
- skarn-type,
- mineralogy,
- EPMA,
- ore genesis

FullText(HTML)

References(48)

References

Chen, L., Wang, J.B., Deng, X.H., et al., 2018.Geological and Geochemical Characteristics and Genesis of Xierqu Fe-Cu Deposit in the Kalatag District, Eastern Tianshan, NW China.Earth Science, 43(9):3065-3085(in Chinese with English abstract).

Dai, J.Z., Mao, J.W., Zhao, C.S., et al., 2009.New U-Pb and Re-Os Age Data and the Geodynamic Setting of the Xiaojiayingzi Mo (Fe) Deposit, Western Liaoning Province, Northeastern China.Ore Geology Reviews, 35(2):235-244. https://doi.org/10.1016/j.oregeorev.2008.10.001

Dupuis, C., Beaudoin, G., 2011.Discriminant Diagrams for Iron Oxide Trace Element Fingerprinting of Mineral Deposit Types.Mineralium Deposita, 46(4):319-335. https://doi.org/10.1007/s00126-011-0334-y

Hong, W., Zhang, Z.H., Jiang, Z.S., et al., 2012.Magnetite and Garnet Trace Element Characteristics from the Chagangnuoer Iron Deposit in the Western Tianshan Mountains, Xinjiang, NW China:Constrain for Ore Genesis.Acta Petrologica Sinica, 28(7):2089-2102(in Chinese with English abstract).

Kamvong, T., Zaw, K., 2009.The Origin and Evolution of Skarn-Forming Fluids from the Phu Lon Deposit, Northern Loei Fold Belt, Thailand:Evidence from Fluid Inclusion and Sulfur Isotope Studies.Journal of Asian Earth Sciences, 34(5):624-633. https://doi.org/10.1016/j.jseaes.2008.09.004

Liu, C.H., Bagas, L., Wang, F.X., 2016.Isotopic Analysis of the Super-Large Shuangjianzishan Pb-Zn-Ag Deposit in Inner Mongolia, China:Constraints on Magmatism, Metallogenesis, and Tectonic Setting.Ore Geology Reviews, 75:252-267. https://doi.org/10.1016/j.oregeorev.2015.12.019

Liu, J.M., Ye, J., Li, Y.B., et al., 2001.A Preliminary Study on Exhalative Mineralization in Permian Basins, the Southern Segment of the Da Hinggan Mountains, China:Case Studies of the Huanggang and Dajing Deposits.Resource Geology, 51(4):345-358. https://doi.org/10.1111/j.1751-3928.2001.tb00107.x

Liu, J.M., Zhang, R., Zhang, Q.Z., 2004.The Regional Metallogeny of Da Hinggan Ling, China.Earth Science Frontiers, 11(1):269-277(in Chinese with English abstract). http://www.researchgate.net/publication/287652723_The_regional_metallogeny_of_Dahingganling_China

Mei, W., 2014.Mesozoic Magmatism and Mineralization in Northern Chifeng, Inner Mongolia (Dissertation).China University of Geosciences, Wuhan(in Chinese with English abstract).

Mei, W., Lü, X.B., Cao, X.F., et al., 2015.Ore Genesis and Hydrothermal Evolution of the Huanggang Skarn Iron-Tin Polymetallic Deposit, Southern Great Xing'an Range:Evidence from Fluid Inclusions and Isotope Analyses.Ore Geology Reviews, 64(1):239-252. https://doi.org/10.1016/j.oregeorev.2014.07.015

Mei, W., Lü, X.B., Wang, X.D., et al., 2018.Geochemistry of Magnetite from the Huanggang Skarn Iron-Tin Polymetallic Deposit in the Southern Great Xing'an Range, NE China.Geological Journal, 53(3):1200-1214. https://doi.org/10.1002/gj.2951

Meinert, L.D., Dipple, G.M., Nicolescu, S., 2005.World Skarn Deposits.One Hundredth Anniversary Volume.Society of Economic Geologists, McLean, Va, 299-336. https://doi.org/10.5382/av100.11

Ouyang, H.G., Mao, J.W., Zhou, Z.H., et al., 2015.Late Mesozoic Metallogeny and Intracontinental Magmatism, Southern Great Xing'an Range, Northeastern China.Gondwana Research, 27(3):1153-1172. https://doi.org/10.1016/j.gr.2014.08.010

Shao, H., Chen, M., Ji, M., et al., 2020.Micro-Textures and Chemistry of Magnetite from the Tonglushan Skarn Cu-Fe Deposit and Its Implications for Ore-Forming Processes.Earth Science, 45(1):118-130(in Chinese with English abstract).

Smith, M.P., Henderson, P., Jeffries, T.E.R., et al., 2004.The Rare Earth Elements and Uranium in Garnets from the Beinn an Dubhaich Aureole, Skye, Scotland, UK:Constraints on Processes in a Dynamic Hydrothermal System.Journal of Petrology, 45(3):457-484. https://doi.org/10.1093/petrology/egg087

Somarin, A.K., Moayyed, M., 2002.Granite-and Gabbrodiorite-Associated Skarn Deposits of NW Iran.Ore Geology Reviews, 20(3-4):127-138. https://doi.org/10.1016/s0169-1368(02)00068-9

Tang, P., Tang, J.X., Zheng, W.B., et al., 2017.Progress in Study of Mineral Chemistry of Magmatic and Hydrothermal Biotites.Mineral Deposits, 36(4):935-950(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-KCDZ201704010.htm

Tang, R.K., Lü, X.B., Cao, X.F., et al., 2014.Mineralogy and Metallogenic Mechanism of Weilasituo and Bairendaba Deposits, Inner Mongolia, China.Earth Science, 39(6):671-686(in Chinese with English abstract). http://www.researchgate.net/publication/287841153_Mineralogy_and_metallogenic_mechanism_of_Weilasituo_and_Bairendaba_deposits_Inner_Mongolia_China

Wang, C., Shao, Y.J., Zhang, X., et al., 2018.Trace Element Geochemistry of Magnetite:Implications for Ore Genesis of the Huanggangliang Sn-Fe Deposit, Inner Mongolia, Northeastern China.Minerals, 8(5):195.

Wang, C.M., Zhang, S.T., Deng, J., et al., 2007.The Exhalative Genesis of the Stratabound Skarn in the Huanggangliang Sn-Fe Polymetallic Deposit of Inner Mongolia.Acta Petrologica et Mineralogica, 26(5):409-417(in Chinese with English abstract). http://www.zhangqiaokeyan.com/academic-journal-cn_acta-petrologica-mineralogica_thesis/0201254451841.html

Wang, L.J., Shimazaki, H., Shiga, Y., 2001a.Skarns and Genesis of the Huanggang Fe-Sn Deposit, Inner Mongolia, China.Resource Geology, 51(4):359-376. https://doi.org/10.1111/j.1751-3928.2001.tb00108.x

Wang, L.J., Shimazaki, H., Wang, J.B., et al., 2001b.Ore-Forming Fluid and Metallization of the Huanggangliang Skarn Fe-Sn Deposit, Inner Mongolia.Science in China (Series D), 44(8):735-747. https://doi.org/10.1007/bf02907203

Wang, L.J., Wang, J.B., Wang, Y.W., et al., 2001c.Fluid-Melt Inclusions in Fluorite of the Huanggangliang Skarn Iron-Tin Deposit and Their Significance to Mineralization.Acta Geologica Sinica, 75(2):204-211. https://doi.org/10.1111/j.1755-6724.2001.tb00522.x

Wang, W., Wang, M.F., Guo, X.N., et al., 2015.Geochemical Characteristics of Magnetite Elements in the Tieshan Iron Deposit in Southeastern Hubei Province and Geological Implications.Geology and Exploration, 51(3):451-465(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZKT201503006.htm

Wu, F.Y., Sun, D.Y., Ge, W.C., et al., 2011.Geochronology of the Phanerozoic Granitoids in Northeastern China.Journal of Asian Earth Sciences, 41(1):1-30. https://doi.org/10.1016/j.jseaes.2010.11.014

Xiao, W.J., Windley, B.F., Hao, J., et al., 2003.Accretion Leading to Collision and the Permian Solonker Suture, Inner Mongolia, China:Termination of the Central Asian Orogenic Belt.Tectonics, 22(6):1069. https://doi.org/10.1029/2002tc001484

Xu, Z.B., Shao, Y.J., Yang, Z.A., et al., 2017.LA-ICP-MS Analysis of Trace Elements in Sphalerite from the Huanggangliang Fe-Sn Deposit, Inner Mongolia, and Its Implications.Acta Petrologica et Mineralogica, 36(3):360-370(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSKW201703006.htm

Ying, L.J., Wang, D.H., Liang, T., et al., 2006.Chemical Composition and Typomorphic Characteristics of Magnetite and Its Geological Significance in Qiaoxiahala Iron-Copper-Gold Deposit of Altai, Xinjiang.Acta Mineralogica Sinica, 26(1):59-68(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-KWXB200601010.htm

Zaw, K., Singoyi, B., 2000.Formation of Magnetite-Scheelite Skarn Mineralization at Kara, Northwestern Tasmania:Evidence from Mineral Chemistry and Stable Isotopes.Economic Geology, 95(6):1215-1230. https://doi.org/10.2113/gsecongeo.95.6.1215

Zeng, Q.D., Liu, J.M., Yu, C.M., et al., 2011.Metal Deposits in the Da Hinggan Mountains, NE China:Styles, Characteristics, and Exploration Potential.International Geology Review, 53(7):846-878. https://doi.org/10.1080/00206810903211492

Zhai, D.G., Liu, J.J., Zhang, H.Y., et al., 2014.S-Pb Isotopic Geochemistry, U-Pb and Re-Os Geochronology of the Huanggangliang Fe-Sn Deposit, Inner Mongolia, NE China.Ore Geology Reviews, 59:109-122. https://doi.org/10.1016/j.oregeorev.2013.12.005

Zhang, Z.Y., Du, Y.S., Zhang, J., 2013.Alteration, Mineralization, and Genesis of the Zoned Tongshan Skarn-Type Copper Deposit, Anhui, China.Ore Geology Reviews, 53:489-503. https://doi.org/10.1016/j.oregeorev.2013.02.009

Zhao, Y.M., Feng, C.Y., Li, D.X., 2017.New Progress in Prospecting for Skarn Deposits and Spatial-Teporal Distribution of Skarn Deposits in China.Mineral Deposits, 36(3):519-543(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-KCDZ201703001.htm

Zhou, Z.H., Liu, H.W., Chang, G.X., et al., 2011.Mineralogical Characteristics of Skarns in the Huanggang Sn-Fe Deposit of Inner Mongolia and Their Metallogenic Indicating Significance.Acta Petrologica et Mineralogica, 30(1):97-112(in Chinese with English abstract).

Zhou, Z.H., Mao, J.W., Lyckberg, P., 2012.Geochronology and Isotopic Geochemistry of the A-Type Granites from the Huanggang Sn-Fe Deposit, Southern Great Hinggan Range, NE China:Implication for Their Origin and Tectonic Setting.Journal of Asian Earth Sciences, 49:272-286. https://doi.org/10.1016/j.jseaes.2012.01.015

陈磊, 王京彬, 邓小华, 等, 2018.东天山卡拉塔格西二区铁铜矿床地质地球化学特征及成因.地球科学, 43(9):3065-3085. doi: 10.3799/dqkx.2018.157

洪为, 张作衡, 蒋宗胜, 等, 2012.新疆西天山查岗诺尔铁矿床磁铁矿和石榴石微量元素特征及其对矿床成因的制约.岩石学报, 28(7):2089-2102. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201207012.htm

刘建明, 张锐, 张庆洲, 2004.大兴安岭地区的区域成矿特征.地学前缘, 11(1):269-277. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200401036.htm

梅微, 2014.内蒙古赤峰北部地区中生代岩浆作用与成矿研究(硕士学位论文).武汉: 中国地质大学.

邵辉, 陈觅, 纪敏, 等, 2020.磁铁矿显微结构及化学成分对铜绿山矽卡岩型铜铁矿床成矿过程的指示.地球科学, 45(1):118-130. doi: 10.3799/dqkx.2018.583

唐攀, 唐菊兴, 郑文宝, 等, 2017.岩浆黑云母和热液黑云母矿物化学研究进展.矿床地质, 36(4):935-950. https://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ201704010.htm

唐然坤, 吕新彪, 曹晓峰, 等, 2014.内蒙古维拉斯托-拜仁达坝矿床矿石特征及成矿机理.地球科学, 39(6):671-686. doi: 10.3799/dqkx.2014.063

王伟, 王敏芳, 郭晓南, 等, 2015.鄂东南矿集区铁山铁矿床中磁铁矿元素地球化学特征及其地质意义.地质与勘探, 51(3):451-465. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKT201503006.htm

王长明, 张寿庭, 邓军, 等, 2007.内蒙古黄岗梁锡铁多金属矿床层状夕卡岩的喷流沉积成因.岩石矿物学杂志, 26(5):409-417. https://www.cnki.com.cn/Article/CJFDTOTAL-YSKW200705004.htm

徐卓彬, 邵拥军, 杨自安, 等, 2017.内蒙古黄岗梁铁锡矿床闪锌矿LA-ICP-MS微量元素组成及其指示意义.岩石矿物学杂志, 36(3):360-370. https://www.cnki.com.cn/Article/CJFDTOTAL-YSKW201703006.htm

应立娟, 王登红, 梁婷, 等, 2006.新疆阿尔泰乔夏哈拉铁铜金矿床磁铁矿的化学成分标型特征和地质意义.矿物学报, 26(1):59-68. https://www.cnki.com.cn/Article/CJFDTOTAL-KWXB200601010.htm

赵一鸣, 丰成友, 李大新, 2017.中国矽卡岩矿床找矿新进展和时空分布规律.矿床地质, 36(3):519-543. https://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ201703001.htm

周振华, 刘宏伟, 常帼雄, 等, 2011.内蒙古黄岗锡铁矿床夕卡岩矿物学特征及其成矿指示意义.岩石矿物学杂志, 30(1):97-112. https://www.cnki.com.cn/Article/CJFDTOTAL-YSKW201101013.htm

Relative Articles

Supplements(0)

Cited By

Proportional views

Proportional views

通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

Figures(12)

Get Citation

PDF

XML

Article views (2095) PDF downloads(104)

Alteration, Mineralization and Genesis of Huanggang Skarn Iron-Tin Polymetallic Deposit, Southern Great Xing'an Range

doi: 10.3799/dqkx.2020.298

Abstract

References

Proportional views

Catalog

通讯作者: 陈斌, bchen63@163.com

Proportional views

Export File

Citation

Format

Content