A study of the ore-forming age of the Hutouya deposit and its geological significance:Geochemistry and U-Pb zircon ages of biotite monzonitic granite in Qimantag, East Kunlun Mountains

SHI Chao; LI Rongshe; HE Shiping; JI Wenhua; GU Pingyang; CHEN Shoujian; ZHANG Haidi

Geological Bulletin of China > 2017 > 36(6): 977-986.

SHI Chao, LI Rongshe, HE Shiping, JI Wenhua, GU Pingyang, CHEN Shoujian, ZHANG Haidi. 2017: A study of the ore-forming age of the Hutouya deposit and its geological significance:Geochemistry and U-Pb zircon ages of biotite monzonitic granite in Qimantag, East Kunlun Mountains. Geological Bulletin of China, 36(6): 977-986.

Citation:

PDF (7744 KB)

A study of the ore-forming age of the Hutouya deposit and its geological significance:Geochemistry and U-Pb zircon ages of biotite monzonitic granite in Qimantag, East Kunlun Mountains

SHI Chao^{1, 2,},
LI Rongshe^{1, 2, ,},
HE Shiping^{1, 2},
JI Wenhua^{1, 2},
GU Pingyang^{1, 2},
CHEN Shoujian¹,
ZHANG Haidi^{1, 2}

1.
MLR Key Laboratory for the Study of Focused Magmatism and Giant Ore Deposits, Xi'an Center of Geological Survey, CGS, Xi'an 710054, Shaanxi, China
2.
Research Center for Orogenic Geology, Xi'an Center of Geological Survey, CGS, Xi'an 710054, Shaanxi, China

More Information

Received Date: February 01, 2016
Revised Date: May 22, 2016
Available Online: August 15, 2023

Graphical Abstract

Abstract

Abstract

The Hutouya Pb-Zn polymetallic ore deposit is located in Qimantag, East Kunlun Mountains.Intermediate-acid intru-sive rocks occur widely in this area, and are closely related to iron polymetallic mineralization.The ²⁰⁶Pb/²³⁸U weighted average age is 234.2±1.5 Ma, which was obtained by in-situ LA-ICP-MS zircon dating of biotite monzonitic granite that was closely related to mineralization and skarn.The results of geochemical analysis show that the biotite monzonitic granite is characterized by high Al₂O₃, K₂O and low TiO₂, Na₂O.The I-type granites are characterized by rich LREE, Rb, Th and some of HFSE, but poor Nb, Sr and Zr, and clear separation of LREE from HREE.In diagram of(Y+Nb)-Rb, all samples fall into post-collision granite area, and in R1-R2 diagram, all samples fall into the superimpositon of post-collision granite area and collision granite area, indicating that the gran-ites probably formed in a collision-post-collision structural phase.The Ⅵ belt of the Hutouya Pb-Zn polymetallic ore deposit expe-riended strong skarnization.The authors hold that the deposit has characteristics of skarn deposit, as shown by its ore fabric, gangue minerals, wall rock alteration, and it was formed at 234.2±1.5 Ma (Middle-Late Triassic).

FullText(HTML)

References (50)

References

李荣社, 计文化, 潘晓萍, 等. 1:100万昆仑山及邻区地质图及说明书[M].北京:地质出版社, 2009.

张爱奎, 莫宣学, 李云平, 等.青海西部祁漫塔格成矿带找矿新进展及其意义[J].地质通报, 2010, 29(7):1062-1074. http://dzhtb.cgs.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20100713&journal_id=gbc

刘云华, 莫宣学, 张雪亭, 等.东昆仑野马泉地区矽卡岩矿床地质特征及控矿条件[J].华南地质与矿产, 2005, (3):18-23. http://www.cnki.com.cn/Article/CJFDTOTAL-HNKC200503003.htm

张爱奎, 李云平, 刘光莲, 等.虎头崖铜铅锌矿床类型新认识及其意义[J].青海国土经略, 2008, (4):25-27. http://www.cnki.com.cn/Article/CJFDTOTAL-GTJL200804013.htm

胡杏花, 朱谷昌, 刘欢, 等.祁漫塔格矿带虎头崖多金属矿矿床特征和成矿作用分析[J].地质与勘探, 2011, 47(2):216-221. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKT201102012.htm

古凤宝, 吴向农, 姜常义.东昆仑华力西期-印支期花岗岩组合及构造环境[J].青海地质, 1996, 5(1):18-26. http://www.cnki.com.cn/Article/CJFDTOTAL-GTJL199601001.htm

袁万明, 莫宣学, 喻学惠, 等.东昆仑印支期区域构造背景的花岗岩记录[J].地质论评, 2000, 46(2):203-221. http://www.cnki.com.cn/Article/CJFDTOTAL-DZLP200002012.htm

李光明, 沈远超.东昆仑祁漫塔格地区华力西期花岗岩地质地球化学特征[J].地质与勘探, 2001, (1):73-78. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKT200101016.htm

罗照华, 柯珊, 曹永清, 等.东昆仑印支晚期幔源岩浆活动[J].地质通报, 2002, 21(6):292-297. http://dzhtb.cgs.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20020677&journal_id=gbc

王松, 丰成友, 李世金, 等.青海祁曼塔格卡尔却卡铜多金属矿区花岗闪长岩锆石SHRIMP U-Pb测年及其地质意义[J].中国地质, 2009, 36(1):74-84. http://www.cnki.com.cn/Article/CJFDTOTAL-DIZI200901008.htm

李侃, 高永宝, 钱兵, 等.东昆仑祁漫塔格虎头崖铅锌多金属矿区花岗岩年代学、地球化学及Hf同位素特征[J].中国地质, 2015, 42(3):630-645. http://www.cnki.com.cn/Article/CJFDTOTAL-DIZI201503017.htm

Gao S, Liu X M, Yuan H L, et al. Analysis of forty-two major and trace elements of USGS and NIST SRM Glasses by LA-ICPMS[J]. Geostand Newsl., 2002, 22:181-195. https://www.researchgate.net/publication/252188504_Analysis_of_forty-two_major_and_trace_elements_in_USGS_and_NIST_SRM_glasses_by_LA-ICPMS

刘小明, 高山, 袁洪林, 等. 193nm LA-ICPMS对国际地质标准参考物中42种主元素和微量元素的分析[J].岩石学报, 2002, 18(3):408-418. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=ysxb200203016&dbname=CJFD&dbcode=CJFQ

袁洪林, 吴福元, 高山, 等.东北地区新生代侵入体的锆石激光探针U-Pb年龄测定与稀土元素成分分析[J].科学通报, 2003, 48(14):1511-1520. doi: 10.3321/j.issn:0023-074X.2003.14.008

Anderson T. Correction of common lead in U-Pb analyses that do not report 204 Pb[J]. Chemical Geology, 2002, 192:59-79. doi: 10.1016/S0009-2541(02)00195-X

Ludwig K R. 3.0-A geochronology cal toolkit for Micro-soft Excel[J]. Berkeley Geochronology Center, Special Publication, 2003, (4):1-70.

Hoskin P W O, Black L P. Metamorphic zircon formation by solid-state recrystallization of protolith igneous zircon[J]. Journal of Metamorphic Geology, 2000, 18:423-439. https://www.researchgate.net/publication/229968849_Metamorphic_zircon_formation_by_solid-state_recrystallization_of_protolith_igneous_zircon

Turner S P, Foden J D, Morrison R S. Derivation of some A-type magmas by fractionation of basaltic agama:an example from the Padthaway Ridge, South Australia[J]. Lithos, 1992, 28:151-179. doi: 10.1016/0024-4937(92)90029-X

Chappell B W, White A J R. Two contrasting granite types[J]. Pacific Geology, 1974, 8:173-174. http://geoscienceworld.org/georef/1975-030452

Maniar P D, Piccoli P M. Tectonic discrimination of granitoids[J]. GSA Bull., 1989, 101(5):635-643. doi: 10.1130/0016-7606(1989)101<0635:TDOG>2.3.CO;2

Richwood P C. Boundary lines within petrologic diagrams which use oxides of major and minor elements[J]. Lithos, 1989, 22(4):247-263. doi: 10.1016/0024-4937(89)90028-5

Sun S S, Mc Donoungh W F. Chemical and isotopic systematics of oceanic basalt:implication for mantle composition and processes[C]//Saunders A D, Norry M J. Magmatism in the Ocean Basins. Geol. Soc. London Spec. Pub., 1989, 42:313-345.

Pearce J A. Sources and setting of granitic rocks[J]. Episodes, 1996, 19(4):120-125. https://www.researchgate.net/publication/262099137_Sources_and_Settings_of_Granitic_Rocks

Harris N B W, Pearce J A, Tindle A G. Geochemical characteristics of collision-zone magmatism[J]. Geological Society of London, Special Publication, 1986, 19:67-81. doi: 10.1144/GSL.SP.1986.019.01.04

Williamson B J, Shaw A, Downes H, et al. Geochemical constraints on the genesis of Hercynian two-micaleucogranites from the Massive Central[J]. Chemical Geology, 1996, 127:25-42. doi: 10.1016/0009-2541(95)00105-0

Pitcher W S. Granite type and tectonic environment[M]. Mountain Building Processes, London:Academic Press, 1983:19-40.

Forster H J, Tischendorf G, Gottesmann B, et al. Late-collisional granites in the Variscan Erzgebirge[J]. Journal of Petrology, 1999, 40:1613-1645. doi: 10.1093/petroj/40.11.1613

Kalsbeek F, J epsen H, Nutman A. From source migmatitesto to plutons:tracking the origin of ca. 435 Ma S-type granites in the East Greenland Caledonian orogen[J]. Lithos, 2001, 57:1-21. doi: 10.1016/S0024-4937(00)00071-2

肖庆辉, 邓晋福, 马大诠, 等.花岗岩研究思维与方法[M].北京:地质出版社, 2002.

Liegeois G P, Navez J, Hertongen J, et al. Contrasting origin of post-collisional high-K calc-alkaline and shoshonitic versus alkaline and peralkaline granitoids:the use of sliding normalization[J]. Lithos, 1998, 45:1-28. doi: 10.1016/S0024-4937(98)00023-1

韩宝福.后碰撞花岗岩类的多样性及其构造环境判别的复杂性[J].地学前缘, 2007, 14(3):64-72. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200703007.htm

任继舜, 姜春发, 张正坤, 等.中国大地构造及其演化[M].北京:科学出版社, 1980:1-124.

殷鸿福, 张克信.中央造山带的演化及其特点[J].地球科学, 1998, 23(5):437-442. http://www.cnki.com.cn/Article/CJFDTOTAL-DQKX805.000.htm

袁万明, 莫宣学, 喻学惠, 等.东昆仑印支期区域构造背景的花岗岩记录[J].地质论评, 2000, 46(2):203-211. http://www.cnki.com.cn/Article/CJFDTOTAL-DZLP200002012.htm

莫宣学, 罗照华, 邓晋福, 等.东昆仑造山带花岗岩及地壳生长[J].高校地质学报, 2007, 13(3):403-414. http://www.cnki.com.cn/Article/CJFDTOTAL-GXDX200703005.htm

校培喜, 高晓峰, 胡云绪, 等.阿尔金-东昆仑西段成矿带地质背景研究[M].北京:地质出版社, 2014:1-261.

罗照华, 邓晋福, 曹永清, 等.青海省东昆仑地区晚古生代-早中生代火山活动与区域构造演化[J].现代地质, 1999, 13(1):51-56. http://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ901.007.htm

Pearce J A, Harris N B W, Tindle A G. Trace element discrimination diagrams for the tectonic interpretation of granitic rocks[J]. Petrol, 1984, 25(4):956-983. doi: 10.1093/petrology/25.4.956

Batchelor R A, Bowden P. Petrogentic interpretation of granitoid rocks series using multicationic[J]. Chemical Geology, 1985, 48:43-45. doi: 10.1016/0009-2541(85)90034-8

Zhao X X, Coe R S, Gilder S A, et al. Palaeomagnetic constraints on the palaeogeography of China:implications for Gondwanaland[J]. Australian Journal of Earth Sciences, 1996, 43(6):643-672. doi: 10.1080/08120099608728285

Liegeois J P, Navez J, Hertogen J, et al. Contrasting origin of postcollisional high-K calc-alkaline and shoshonitic versus alkaline and per alkaline granitoids[J]. Lithos, 1998, 45(1):1-28. https://www.researchgate.net/publication/222483323_Contrasting_origin_of_post-collisional_high-K_calc-alkaline_and_shoshonitic_versus_alkaline_and_peralkaline_granitoids_The_use_of_sliding_normalization

刘成东, 张文秦, 莫宣学, 等.东昆仑约格鲁岩体暗色微粒包体特征及成因[J].地质通报, 2002, 21(11):739-744. doi: 10.3969/j.issn.1671-2552.2002.11.009

佘宏全, 张德全, 景向阳, 等.青海省乌兰乌珠尔斑岩铜矿床地质特征与成因[J].中国地质, 2007, 34(2):306-314. http://www.cnki.com.cn/Article/CJFDTOTAL-DIZI200702013.htm

李世金, 孙丰月, 丰成友, 等.青海东昆仑鸭子沟多金属矿的成矿年代学研究[J].地质学报, 2008, 82(7):949-955. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200807015.htm

吴祥珂, 孟繁聪, 许虹, 等.青海祁漫塔格玛兴大坂晚三叠世花岗岩年代学、地球化学及Nd-Hf同位素组成[J].岩石学报, 2011, 27(11):3380-3394. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201111018.htm

高永宝, 李文渊, 马晓光, 等.东昆仑尕林格铁矿床成因年代学及Hf同位素制约[J].兰州大学学报(自然科学版), 2012, 48(2):36-47. http://www.cnki.com.cn/Article/CJFDTOTAL-LDZK201202008.htm

高永宝, 李文渊, 钱兵, 等.东昆仑野马泉铁矿相关花岗质岩体年代学、地球化学及Hf同位素特征[J].岩石学报, 2014, 30(6):1647-1665. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201406009.htm

丰成友, 王松, 李国臣, 等.青海祁漫塔格中晚三叠世花岗岩:年代学、地球化学及成因意义[J].岩石学报, 2012, 28(2):665-678. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201202025.htm

高永宝, 李文渊, 李侃, 等.青海祁漫塔格虎头崖铅锌矿床流体包裹体、同位素地球化学及矿床成因[J].地质通报, 2013, 32(10):1631-1642. doi: 10.3969/j.issn.1671-2552.2013.10.015

马圣钞, 丰成友, 李国臣, 等.青海虎头崖铜铅锌多金属矿床硫、铅同位素组成及成因意义[J].地质与勘探, 2012, 48(2):321-331. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKT201202015.htm

Cited By

Get Citation

PDF

XML

Article views (2209) PDF downloads (324)

Turn off MathJax

Article Contents

Abstract

References

	WANG Hongjie, BAI Jianke, ZHAO Haibo, CHENG Long, ZHU Likuan, GUO Feng. 2024: Early Paleozoic Paleo-Asian Ocean subduction in the southern Beishan, Gansu: Evidence of zircon U−Pb age and geochemical records from Mingshujing adakitic pluton. Geological Bulletin of China, 43(2~3): 376-389. DOI: 10.12097/gbc.2022.02.028
	XU Wentan, ZHANG Xuehui, ZHANG Binbin, LYU Jinsong, SUN Jiandong, ZHANG Yong, WU Bin. 2022: Genesis of highly fractionated S-type granites: Evidence from zircon U-Pb age, Hf isotopes and geochemistry of Fuquanshan pluton, Northeastern Jiangxi Province. Geological Bulletin of China, 41(4): 577-589. DOI: 10.12097/j.issn.1671-2552.2022.04.005
	WANG Liling, ZHANG Shuming, XU Xun, ZHANG Xin, RUAN Xiaoyu, LAN Dechu, WU Zhichun, QI Jiawei. 2020: LA-ICP-MS zircon U-Pb dating and genetic types of uranium-bearing granite porphyry in northern Xiangshan orefield, Jiangxi Province. Geological Bulletin of China, 39(1): 62-79.
	LIU Shuai, WU Jianhua, DING Hui, HUANG Meihua. 2018: Zircon U-Pb age of the Caledonian volcanic rocks in Nanjing basin of southern Jiangxi Province and its geological significance. Geological Bulletin of China, 37(10): 1905-1919.
	SHI Meifeng, LIN Fangcheng, FAN Wenyu, WANG Hong, CONG Feng, ZHU Huaping. 2015: SHRIMP zircon U-Pb dating of the monzogranites in the Pilok tintungsten mining area, western Thailand, and its geological implications. Geological Bulletin of China, 34(4): 769-779.
	WU Jian-hua, XU Xun-sheng, LIU Shuai. 2012: SHRIMP zircon U-Pb dating of the early Late Cretaceous felsic volcanic rock in southern Jiangxi-northern Guangdong area and its geological significance. Geological Bulletin of China, 31(8): 1296-1305.
	LIU Wei, LI Fen-qi, YUAN Si-hua, ZHANG Wan-ping, WANG Bao-di, ZHUO Jie-wen, CHEN Lu, CHEN Li. 2011: Zircon LA-ICP-MS U-Pb age of Early Cretaceous ignimbrite in southern Nagqu, Tibet. Geological Bulletin of China, 30(7): 1043-1049.
	YANG Li-zhen, LIU Rong-tao, BAI Yan-ping. 2011: The Early-Middle Triassic volcanic event—the Taima porphyroclastic lava in the Qinzhou area, southern Guangxi, China. Geological Bulletin of China, 30(1): 95-100.
	2006: Characteristics and zircon SHRIMP U-Pb ages of the arc magmatic rocks in Mazar, southern Yecheng, West Kunlun Mountains. Geological Bulletin of China, 25(1): 124-132.
	ZHANG Jianxin, MENG Fancong, WAN Yusheng, YANG Jingsui, Tung KuoAn. 2003: Early Paleozoic tectono-thermal event of the Jinshuikou Group on the southern margin of Qaidam:Zircon U-Pb SHRIMP age evidence. Geological Bulletin of China, 22(6): 397-404.

A study of the ore-forming age of the Hutouya deposit and its geological significance:Geochemistry and U-Pb zircon ages of biotite monzonitic granite in Qimantag, East Kunlun Mountains

Abstract

References

Related Articles

Catalog

A study of the ore-forming age of the Hutouya deposit and its geological significance:Geochemistry and U-Pb zircon ages of biotite monzonitic granite in Qimantag, East Kunlun Mountains

Abstract

References

Related Articles

Catalog

Export File

Citation

Format

Content