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

Volume 22 Issue 2

Jun. 2016

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Article Navigation > Journal of Geomechanics > 2016 > 22(2): 199-211

ZHANG Zhi-guo, PENG Hua, MA Yin-sheng, et al., 2005. APPLICATION OF THE ULTRASONIC FLAWLESS DETECTOR IN THE PRESERVATION OF UNEARTHED STONY CULTURAL RELICS. Journal of Geomechanics, 11 (3): 278-285,244.

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ZHAO Xin-ke, CAO Lin-jie, SHEN Yu-ke, et al., 2016. THE ORE STRUCTURAL FEATURES AND THE ORE-FORMING MATERIAL SOURCE OF THE SHADONGGOU MERCURY ANTIMONY DEPOSIT IN XUNYANG, SHAANXI. Journal of Geomechanics, 22 (2): 199-211.

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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

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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. 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.
[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. 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.
[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. http://www.cnki.com.cn/Article/CJFDTOTAL-GJSD200301002.htm 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. http://www.cnki.com.cn/Article/CJFDTOTAL-GJSD200301002.htm
[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. http://www.cnki.com.cn/Article/CJFDTOTAL-GJSD200102004.htm 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. http://www.cnki.com.cn/Article/CJFDTOTAL-GJSD200102004.htm
[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. PENG Da-ming. Geology of the Xunyang Sb-Hg ore field[J]. Geological Exploration for Non-ferrous Metals, 1998, 7(5): 289~293.
[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. http://www.cnki.com.cn/Article/CJFDTOTAL-DZLP198101002.htm 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. http://www.cnki.com.cn/Article/CJFDTOTAL-DZLP198101002.htm
[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. YANG Zhi-hua. Tectono-lithofacie and ore-forming of marginal transition basin[M]. Beijing: Science Press, 1991: 1~228.
[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. http://www.cnki.com.cn/Article/CJFDTOTAL-XBDI198004002.htm YANG Zhi-hua. Geological characteristics and formation mechanism of Gongguan mercury-antimony deposit in Xunyang, Shaanxi Province[J]. Northwestern Geology, 1980, (4): 236~242. http://www.cnki.com.cn/Article/CJFDTOTAL-XBDI198004002.htm
[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. http://cpfd.cnki.com.cn/Article/CPFDTOTAL-DQHJ201010001089.htm 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. http://cpfd.cnki.com.cn/Article/CPFDTOTAL-DQHJ201010001089.htm
[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. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB199502000.htm 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. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB199502000.htm
[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. http://www.cnki.com.cn/Article/CJFDTOTAL-DZLP198101002.htm 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. http://www.cnki.com.cn/Article/CJFDTOTAL-DZLP198101002.htm
[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. http://cpfd.cnki.com.cn/Article/CPFDTOTAL-DXHD201304001160.htm 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. http://cpfd.cnki.com.cn/Article/CPFDTOTAL-DXHD201304001160.htm
[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. 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.
[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. http://www.cnki.com.cn/Article/CJFDTOTAL-DZZK200001008.htm 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. http://www.cnki.com.cn/Article/CJFDTOTAL-DZZK200001008.htm
[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. TU Guang-zhi. Geochemistry of stratabound ore deposit in China[M]. Beijing: Science Press, 1984: 189~214.
[16]	胡受奚.交代蚀变岩岩相学[M].北京:地质出版社, 1980. HU Shou-xi. Petrography of metasomatic alterated rock[M]. Beijing: Geological Publishing House, 1980.
[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. http://www.cnki.com.cn/Article/CJFDTOTAL-GWHD198701001.htm
[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. HAN Yin-wen, MA Zhen-dong, ZHANG Hong-fei, et al. Geochemistry[M]. Beijing: Geological Publishing House, 2003: 1~369.
[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.
[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. http://www.cnki.com.cn/Article/CJFDTOTAL-YSKW704.006.htm 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. http://www.cnki.com.cn/Article/CJFDTOTAL-YSKW704.006.htm
[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. LU Huan-zhang, FAN Hong-rui, NI Pei, et al. Fluid inclusions[M]. Beijing: Science Press, 2004: 1~487.
[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. ShAO Jie-lian. Mineralogy for gold ore prospecting[M]. Wuhan: China University of Geosciences Press, 1988: 38~45.
[23]	福尔G.同位素地质学原理[M].北京:科学出版社, 1983: 1~351. Faure G. Geology principle of isotopes[M]. Beijing: Science Press, 1983: 1~351.
[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. http://www.cnki.com.cn/Article/CJFDTOTAL-YSKW200101007.htm 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. http://www.cnki.com.cn/Article/CJFDTOTAL-YSKW200101007.htm