THE ORE STRUCTURAL FEATURES AND THE ORE-FORMING MATERIAL SOURCE OF THE SHADONGGOU MERCURY ANTIMONY DEPOSIT IN XUNYANG, SHAANXI

ZHAO Xin-ke; CAO Lin-jie; SHEN Yu-ke; LI Wei-song; MA Yun-feng; LIU Ya-li; WANG Xiao-hu; SUN Jian; LIU Li-min

2016 Vol. 22, No. 2

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ZHAO Xin-ke, CAO Lin-jie, SHEN Yu-ke, LI Wei-song, MA Yun-feng, LIU Ya-li, WANG Xiao-hu, SUN Jian, LIU Li-min. THE ORE STRUCTURAL FEATURES AND THE ORE-FORMING MATERIAL SOURCE OF THE SHADONGGOU MERCURY ANTIMONY DEPOSIT IN XUNYANG, SHAANXI[J]. Journal of Geomechanics, 2016, 22(2): 199-211.

Citation:

THE ORE STRUCTURAL FEATURES AND THE ORE-FORMING MATERIAL SOURCE OF THE SHADONGGOU MERCURY ANTIMONY DEPOSIT IN XUNYANG, SHAANXI

1.
The No.1 Geological Team, Bureau of Geology and Mineral Resources of Shaanxi, Ankang 725000, Shaanxi, China
2.
Shaanxi Key Laboratory of Exploration and Comprehensive Utilization of Mineral Resources, Xi'an 710054, China
3.
Institute of Geomechanis, CAGS, Beijing 100081, China

Received Date: 27 October 2015

Publish Date: 25 June 2016

Abstract

Abstract

The mercury antimony ore body of the Shadonggou ore field in Xunyang, Shaanxi is controlled jointly by the fold structure (anticline) and fracture structure. Through studying the ore controlling structures, the tectonic sequence of the ore-rich space and the combination characteristics of structural plane, the metallogenic model of "anticline+one knife" has been established and completed. The ore-forming fluid and rare earth analysis show that the metallogenic material may be from the deep crust. The existing exploration engineering and prospecting results show that this ore concentration area has great prospecting potential.
- the ore structure characteristics /
- metallogenic model /
- structure assemblage /
- the Shadonggou mercury antimony deposit

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References

[1]	白洪生, 朱经祥. 陕西省旬阳县公馆汞锑矿床地质研究报告[R]. 北京: 中国地质大学, 1984: 1~66. Google Scholar BAI Hong-sheng, ZHU Jing-xiang. Study report for the geology of mercury-antimony deposits in Gongguan area, Xunyan, Shaanxi[R]. Beijing: China University of Geosciences, 1984: 1~66. Google Scholar
[2]	丁抗. 陕西公馆地区汞锑矿床地球化学研究[D]. 贵阳: 中国科学院地球化学研究所, 1986: 1~126. Google Scholar DING Kang. Study on geochemistry of mercury-antimony deposits in Gongguan area, Shaanxi[D]. Guiyang: Institute of Geochemistry, Chinese Academy of Sciences, 1986: 1~126. Google Scholar
[3]	李勇, 周宗桂.陕西镇安—旬阳地区汞锑、铅锌、金矿床成因及演化规律浅析[J].地质与资源, 2003, 12(1): 19~35. Google Scholar LI Yong, ZHOU Zong-gui. A brief study on the genesis and evolvement rules of the Hg-Sb, Pb-Zn and Au deposits in Zhenan-Xunyang area, Shaanxi Province[J]. Geology and Resources, 2003, 12(1): 19~35. Google Scholar
[4]	庞庆邦, 贾伟光, 韩仲文, 等.陕西省旬阳地区汞锑金矿成矿条件[J].地质与资源, 2001, 10(2): 91~101. Google Scholar PANG Qing-bang, JIA Wei-guang, HAN Zhong-wen, et al. The minerogenetic conditions for the Hg-Sb-Au deposits in Xunyang district, Shaanxi Province[J]. Geology and Resources, 2001, 10(2): 91~101. Google Scholar
[5]	彭大明.旬阳锑汞矿田成矿研探[J].有色金属矿产与勘查, 1998, 7(5): 289~293. Google Scholar PENG Da-ming. Geology of the Xunyang Sb-Hg ore field[J]. Geological Exploration for Non-ferrous Metals, 1998, 7(5): 289~293. Google Scholar
[6]	屈开硕.陕南公馆—回龙地区汞锑矿床地质特征[J].地质论评, 1981, 27(1): 186~192. Google Scholar QU Kai-shuo. On the geological features of the mercury-antimony deposits in Gongguan-huilong area, Southern Shanxi[J]. Geological Review, 1981, 27(1): 186~192. Google Scholar
[7]	杨志华.边缘转换盆地的构造岩相与成矿[M].北京:科学出版社, 1991: 1~228. Google Scholar YANG Zhi-hua. Tectono-lithofacie and ore-forming of marginal transition basin[M]. Beijing: Science Press, 1991: 1~228. Google Scholar
[8]	杨志华.陕西旬阳公馆汞锑矿床地质特征及形成机制[J].西北地质, 1980, (4): 236~242. Google Scholar YANG Zhi-hua. Geological characteristics and formation mechanism of Gongguan mercury-antimony deposit in Xunyang, Shaanxi Province[J]. Northwestern Geology, 1980, (4): 236~242. Google Scholar
[9]	齐文, 赵新科, 唐明锋.南秦岭汞锑成矿带控矿地质标志类型及勘查模式初探[J].陕西地质, 2010, 28(2): 47~51. Google Scholar QI Wen, ZHAO Xin-ke, TANG Ming-feng. Summary of geological criteria and prospecting model of mercury-antimony metallogenic belt in South Qinling orogeny[J]. Shaanxi Geology, 2010, 28(2): 47~51. Google Scholar
[10]	张国伟, 张宗清, 董云鹏.秦岭造山带主要构造岩石地层单元的构造性质及其大地构造意义[J].岩石学报, 1995, 11(2): 101~114. Google Scholar ZHANG Guo-wei, ZHANG Zong-qing, DONG Yun-peng. Nature of main tectono-lithostratigraphic units of the Qinling orogen: Implications for the tectonic evolution[J]. Acta Petrologica Sinica, 1995, 11(2): 101~114. Google Scholar
[11]	陕西省地质局第一地质队综合研究组.陕南公馆—迥龙地区汞锑矿床地质特征[J].地质论评, 1981, 27(1): 15~23. Google Scholar First Geologic Brigate, Shaanxi Bureau of Geology. On the geological features of the mercury-antimony deposits in Gongguan-Huilong area, Southern Shanxi[J]. Geological Review, 1981, 27(1): 15~23. Google Scholar
[12]	王晓虎, 申玉科, 赵新科, 等.陕西省镇旬地区汞锑矿床地球化学特征及成矿年龄[J].地质论评, 2013, 59(4): 365~366. Google Scholar WANG Xiao-hu, SHEN Yu-ke, ZHAO Xin-ke, et al. Geochemistry and ore-forming age of mercury-antimony deposits in the area of Zhenxun, Shaanxi Province[J]. Geological Review, 2013, 59(4): 365~366. Google Scholar
[13]	何立贤, 韩至钧, 安树仁, 等.汞矿地质与普查勘探[M].北京:地质出版社, 1996: 1~129. Google Scholar HE Li-xian, HAN Zhi-jun, AN Shu-ren, et al. Geology and prospecting of mercury deposit[M]. Beijing: Geological Publishing House, 1996: 1~129. Google Scholar
[14]	彭大明.秦岭地槽汞锑资源成矿探讨[J].地质找矿论丛, 2000, 15(1): 64~71. Google Scholar PENG Da-ming. Research on Hg, Sb mineralization in Qinling geosyncline, China[J]. Contributions to Geology and Mineral Resources Research, 2000, 15(1): 64~71. Google Scholar
[15]	涂光炽.中国层控矿床地球化学[M].北京:科学出版社, 1984: 189~214. Google Scholar TU Guang-zhi. Geochemistry of stratabound ore deposit in China[M]. Beijing: Science Press, 1984: 189~214. Google Scholar
[16]	胡受奚.交代蚀变岩岩相学[M].北京:地质出版社, 1980. Google Scholar HU Shou-xi. Petrography of metasomatic alterated rock[M]. Beijing: Geological Publishing House, 1980. Google Scholar
[17]	Cullers R L, Graf J L, 李文达.热液体系中的稀土元素[J].国外火山地质, 1987, (3): 20~23. Cullers R L, Graf J L, LI Wen-da. Rare earth elements in hydrothermal system[J]. Volcanic Geology in Foreign Countries, 1987, (3): 20~23. Google Scholar
[18]	韩吟文, 马振东, 张宏飞, 等.地球化学[M].北京:地质出版社, 2003.1~369. Google Scholar HAN Yin-wen, MA Zhen-dong, ZHANG Hong-fei, et al. Geochemistry[M]. Beijing: Geological Publishing House, 2003: 1~369. Google Scholar
[19]	Chi G X, Ni P. Equation of NaCl/(NaCl+CaCl₂) rations and salinities from hydrohalite-melting and ice-melting temperatures in the H₂O-NaCl-CaCl₂ system[J]. Acta Petrologica Sinica, 2007, 23: 33~37. Google Scholar
[20]	刘建明, 刘家军, 顾雪祥.沉积盆地中的流体活动及其成矿作用[J].岩石矿物学杂志, 1997, 16(4): 341~352. Google Scholar LIU Jian-ming, LIU Jia-jun, GU Xue-xiang. Basin fluids and their related ore deposits[J]. Acta Petrologica Et Mineralogica, 1997, 16(4): 341~352. Google Scholar
[21]	卢焕章, 范宏瑞, 倪培, 等.流体包裹体[M].北京:科学出版社, 2004: 1~487. Google Scholar LU Huan-zhang, FAN Hong-rui, NI Pei, et al. Fluid inclusions[M]. Beijing: Science Press, 2004: 1~487. Google Scholar
[22]	邵洁涟.金矿找矿矿物学[M].武汉:中国地质大学出版社, 1988: 38~45. Google Scholar ShAO Jie-lian. Mineralogy for gold ore prospecting[M]. Wuhan: China University of Geosciences Press, 1988: 38~45. Google Scholar
[23]	福尔G.同位素地质学原理[M].北京:科学出版社, 1983: 1~351. Google Scholar Faure G. Geology principle of isotopes[M]. Beijing: Science Press, 1983: 1~351. Google Scholar
[24]	孙景贵, 胡受奚, 沈昆, 等.胶东金矿区矿田体系中基性—中酸性脉岩的碳氧同位素地球化学研究[J].岩石矿物学杂志, 2001, 20(1): 47~56. Google Scholar SUN Jing-gui, HU Shou-xi, SHEN Kun, et al. Research on C, O isotopic geochemistry of intermediate_basic and intermediate_acid dykes in goldfields of Jiaodong Peninsula[J]. Acta Petrologica et Mineralogica, 2001, 20(1): 47~56. Google Scholar