西拉木伦河北岸敖仑花斑岩型钼矿含矿岩体

杨永强; 定立; 翟德高; 王建平; 刘家军

doi:10.3799/dqkx.2012.137

Volume 37 Issue 6

Jun. 2012

Turn off MathJax

Article Contents

Article Navigation > Earth Science > 2012 > 37(6): 1291-1304

YANG Yong-qiang, DING Li, ZHAI De-gao, WANG Jian-ping, LIU Jia-jun, 2012. Metallogenic Granitoid of Aolunhua Mo Deposit at North Bank of Xilamulun River. Earth Science, 37(6): 1291-1304. doi: 10.3799/dqkx.2012.137

Citation:

YANG Yong-qiang, DING Li, ZHAI De-gao, WANG Jian-ping, LIU Jia-jun, 2012. Metallogenic Granitoid of Aolunhua Mo Deposit at North Bank of Xilamulun River. Earth Science, 37(6): 1291-1304. doi: 10.3799/dqkx.2012.137

Citation:

PDF( 3127 KB)

Metallogenic Granitoid of Aolunhua Mo Deposit at North Bank of Xilamulun River

doi: 10.3799/dqkx.2012.137

1.
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China
2.
School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China

Received Date: 2012-07-10
Available Online: 2021-11-09
Publish Date: 2012-06-15

Abstract

Abstract

The Aolunhua Mo deposit is a typical porphyry deposit,which is located in middle southern section of the Da Hinggan metallogenic belt. In order to determinate the petrogenetic ages of the deposit,we focus our study on granite zircons LA-ICP-MS. Combined with the trace element geochemistry in granites zircons,we discuss in-depth the ore-forming rock's material sources of the deposit. The granite zircons LA-ICP-MS analysis shows that the crystallization age of the granite is 135.0±1.0 Ma,indicating that the granite related with mineralization resulted from magmatism in Early Cretaceous period. The Th/U ratios of the ore-forming rock is greater than 0.1 with a significant positive Ce anomaly(Ce^*=1.72~188.71) and negative Eu anomalies (Eu^*=0.05~0.57). It can be concluded that crust-derived magmatic zircon is characterized by poor LREE,rich HREE,low La,Pr content and positive Ce anomaly. Combined with ore deposit geology and mineralization epoch as well as regional tectonic evolution,we draw a conclusion that formation of the Aolunhua Mo deposit is in the peak metallogenic epoch as 140 Ma in the Da Hinggan region. The tectonic settings of the deposit are in the transition period from lithosphere compression to extension. We think that the Tianshan-Linxi is a crustal type section,it has an important role for research this area. At the same time,we contrast some newly discovered Mo deposits along north bank of Xilamulun River,and find that Tianshan-Linxi is an important Mo ore-forming belt,which facilitates the understanding of regional controlling tectonics and prospecting of the ore deposits.
- porphyry type deposit,
- metallogenic granitoids,
- zircons,
- trace elements,
- Aolunhua Mo deposit,
- ore prospecting,
- ore deposits.

FullText(HTML)

References(75)

References

Andersen, T., 2002. Correction of common lead in U-Pb analyses that do not report ²⁰⁴Pb. Chemical Geology, 192(1-2): 59-79. doi: 10.1016/S009-2541(02)00195-X

Belousova, E.A., Griffin, W.L., Pearson, N.J., 1998. Trace element composition and cathodoluminescence properties of southern African kimberlitic zircons. Mineralogical Magazine, 62(3): 355-366. doi: 10.1180/002646198547747

Chakoumakos, B.C., Murakami, T., Lumpkin, G.R., et al., 1987. Alpha-decay induced fracturing in zircon: the transition from the crystalline to the metamict state. Science, 235(4808): 1556-1559. doi: 10.1126/science.236.4808.1556

Chen, B., Jahn, B.M., Tian, W., 2009. Evolution of the Solonker suture zone: constraints from zircon U-Pb ages, Hf isotopic ratios and whole-rock Nd-Sr isotope compositions of subduction and collision-related magmas and forearc sediments. Journal of Asian Earth Sciences, 34(3): 245-257. doi: 10.1016/j.jsease.2008.05.007

Chen, B., Zhao, G.C., Wilde, S., 2001. Subduction and collision related granitoids from southern Sonidzuoqi, Inner Mongolia: isotopic ages and tectonic implication. Geological Review, 47(4): 361-367(in Chinese with English abstract).

Corfu, F., Hanchar, J.M., Hoskin, P.W.O., et al., 2003. Altas of zircon textures. Reviews in Mineralogy and Geochemistry, 53(1): 469-500. doi: 10.2113/0530469

Guo, L.J., Xie, Y.L., Hou, Z.Q., et al., 2009. Geology and ore fluid characteristics of the Bairendaba silver polymetallic deposit in Inner Mongolia. Acta Petrologica et Mineralogica, 28(1): 26-36(in Chinese with English abstract).

Hoskin, P.W.O., Black, L.P., 2000. Metamorphic zircon formation by solid-state recrystallization of protolith igneous zircon. J. Metamorphic Geol., 18(4): 423-439. doi: 10.1046/j.1525-1314.2000.00266.x

Hoskin, P.W.O., Schaltegger, U., 2003. The composition of zircon and igneous and metamorphic petrogenesis. Reviews in Mineralogy and Geochemistry, 53(1): 27-62. doi: 10.2113/0530027

Li, J.Y., 1998. Some new ideas on tectonics of NE China and its neighboring areas. Geological Review, 44(4): 339-347 (in Chinese with English abstract).

Li, J.Y., Gao, L.M., Sun, G.H., et al., 2007. Shuangjingzi Middle Triassic syn-collisional crust-derived granite in the east Inner Mongolia and its constraint on the timing of collision between Silberian and Sino-Korean paleo-plates. Acta Petrologica Sinica, 23(3): 565-582(in Chinese with English abstract). http://www.researchgate.net/publication/279908280_Shuangjingzi_middle_Triassic_syn-collisional_crust-derived_granite_in_the_east_Inner_Mongolia_and_its_constraint_on_the_timing_of_collision_between_Siberian_and_Sino-Korean_paleo-plates?ev=auth_pub

Li, X.H., Liang, X.R., Sun, M., et al., 2000. Geochronology and geochemistry of single-grain zircons: simultaneous in-situ analysis of U-Pb age and trace elements by LAM-ICP-MS. Eur. J. Mineral., 12(5): 1015-1024. doi: 10.1127/0935-1221/2000/0012-1015

Liu, J.J., Xing, Y.L., Wang, J.P., et al., 2010. Discovery of falkmanite from the Bairendaba superlarge Ag-Pb-Zn polymetallic deposit, Inner Mongolia and its origin significance. Journal of Jilin University (Earth Science Edition), 40(3): 565-572(in Chinese with English abstract). http://d.wanfangdata.com.cn/Periodical/cckjdxxb201003012

Liu, J.M., Zhang, R., Zhang, Q.Z., 2004. The regional metallogeny of Da Hingganling, China. Earth Science Frontiers, 11(1): 269-277(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DXQY200401036.htm

Lv, Z.C., Duan, G.Z., Liu, C.Q., et al., 2000. Silver deposit type, metallogenic series and metallogenic geochemical characteristics in Da Hingganling area. Bulletin of Mineralogy, Petrology and Geochemistry, 19(4): 305-309(in Chinese).

Ma, X.H., Chen, B., Lai, Y., et al., 2009. Petrogenesis and mineralization chronology study on the Aolunhua porphyry Mo deposit, Inner Mongolia, and its geological implications. Acta Petrologica Sinica, 25(11): 2939-2950(in Chinese with English abstract).

Mao, J.W., Wang, Y.T., Zhang, Z.H., et al., 2003. Geodynamic settings of Mesozoic large-scale mineralization in North China and adjacent areas. Science in China (Series D), 46(8): 838-851. doi: 10.1007/BF02879527

McInnes, B.A., Evans, N.J., Fu, F.Q., et al., 2005. Application of thermochronology to hydrothermal ore deposits. Reviews in Mineralogy & Geochemistry, 58(1): 467-498. doi: 10.2138/rmg.2005.58.18

Nie, F.J., Zhang, W.Y., Du, A.D., et al., 2007. Re-Os isotopic dating on molybdenite separates from the Xiaodonggou porphyry Mo deposit, Hexigten Qi, Inner Mongolia. Acta Geogolical Sinica, 81(7): 898-905((in Chinese with English abstract).

People's Republic of China Ministry of Geology and Mineral Resources Geological Memoirs, 1991. Geological House, Beijing, 128-651 (in Chinese).

Qi, J.P., Chen, Y.J., Pirajno, F., 2005. Geological characteristics and tectonic setting of the epithermal deposits in the Northeast China. J. Mineral Petrol., 25(2): 47-59(in Chinese with English abstract).

Ren, J.S., Chen, T.Y., Niu, B.G., et al., 1992. Tectonic evolution of the continental lithosphere and metallogeny in eastern China and adjacent areas. Science Press, Beijing (in Chinese).

Rubatto, D., Gebauer, D., 2000. Use of cathodoluminescence for U-Pb zircon dating by ion microprobe: some examples from the western Alps. Cathodoluminescence in Geoscience, Springer-Verlag Berlin Heidelberg, Germany, 373-400

Shi, Y.R., Liu, D.Y., Zhang, Q., et al., 2004. SHRIMP dating of diorites and granites in southern Suzuopi, Inner Mongolia. Acta Geologica Sinica, 78(6): 789-799(in Chinese with English abstract).

Shu, Q.H., Jiang, L., Lai, Y., et al., 2009. Geoehronologyand fluid inclusion study of the Aolunhua porphyry Cu-Mo deposit in Arhorqin area, Inner Mongolia. Acta Petrologica Sinica, 25(10): 2601-2614(in Chinese with English abstract).

Stein, H.J., Markey, R.J., Morgan, J.W., et al. 2001. The remarkable Re-Os chronometer in molybdenite: how and why it works. Terra Nova, 13(6): 479-486. doi: 10.1046/j.1365-3121.2001.00395.x

Sun, X.G., Liu, J.M., Qin, F., et al., 2008. The new progress on polymetallic studies in Daxinganling-the revelation of the southern bank Xilamulun River Molybdenum polymetallic belt. China Ming Magazine, 17(2): 75-78(in Chinese with English abstract).

Valley, J.W., Chiarenzelli, J.R., MeLelland, J.M., 1994. Oxygen isolope geochemistry of zircon. Earth Plane. Sci. Lett., 126(4): 187-206. doi: 10.1016/0012-821X(94)90106-6

Wang, J.B., Wang, Y.W., Wang, L.J., 2000. Copper metallogenic setting and prospecting potential in the middle-southern part of Da Hinggam Mountaints. Geology and Prospecting, 36(5): 1-4(in Chinese with English abstract).

Wang, J.B., Xu, X., 2006. Post-collisional tectonic evolution and metallogenesis in northern Xinjiang, China. Acta Geologica Sinica, 80(1): 23-31(in Chinese with English abstract).

Wang, L.J., Hidehiko, S., Wang, J.B., et al., 2001. Ore-forming fluid and mineralization of the Huanggangliang skarn Fe-Sn deposit, Inner Mongolia. Science in China(Ser. D), 31(7): 553-562(in Chinese with English abstract).

Wang, Q., Zhu, D.C., Zhao, Z.D., et al., 2012. Magmatic zircons from I-, S- and A-type granitoids in Tibet: trace element characteristics and their application to detrital zircon provenance study. Journal of Asian Earth Sciences, 53: 59-66. doi: 10.1016/i.jseaes.2011.07.027

Xia, X.H., Zhao, Y.H., Yuan, J.Z., et al., 2002. Geology and mineralizing regularity of polymetallic sulfide deposits in Linxi-Tianshan district of Inner Mongilia. Geology of Chemical Minerals, 24(4): 198-206(in Chinese with English abstract).

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: 1069-1089. doi: 10.1029/2002TC001484

Xu, Q., Fu, S.X., Yuan, J.M., et al., 2010. Geological characteristics and prospecting marks of the Aolunhua porphyry Mo-Cu deposit, Inner Mongolia. Geology and Exploration, 46(6): 1019-1028 (in Chinese with English abstract).

Xue, H.M., Guo, L.J., Hou, Z.Q., et al., 2010. SHRIMP zircon U-Pb ages of the Middle Neopaleozoic unmetamorphosed magmatic rocks in the southwestern slope of the Da Hinggan Mountains, Inner Mongolia. Acta Petrologica et Mineralogica, 29(6): 811-823 (in Chinese with English abstract).

Zeng, Q.D., Liu, J.M., 2010. Zircon SHRIMP U-Pb dating and geological significance of the granite porphyry from Banlashan porphyry molybdenum deposit in Xilamulun molybdenum metallogenic belt. Journal of Jilin University (Earth Science Edition), 40(4): 828-834 (in Chinese with English abstract).

Zhang, J.F., Li, Z.T., Jin, C.M., 2004. Adakites in northeastern China and their mineralized implications. Acta Petrologica Sinica, 20(2): 361-368 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB200402015.htm

Zhang, J.F., Quan, H., Wu, G., et al., 2000. Tectonic setting of Mesozoic volcanic rocks in Northeast China. Journal of Precious Metallic Geology, 9(1): 33-38 (in Chinese with English abstract). http://search.cnki.net/down/default.aspx?filename=GJSD200001005&dbcode=CJFD&year=2000&dflag=pdfdown

Zhang, K., Nie, F.J., Hou, W.R., et al., 2012. Re-Os isotopic age dating of molybdenite separates from Hashitu Mo deposit in Linxi County of Inner Mongolia and its geological significance. Mineral Deposits, 31 (1): 129- 138(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-KCDZ201201012.htm

Zhang, L.C., Wu, H.Y., Chen, Z.G., et al., 2009. The metallogenic regularity and herent property of metallugens for Cu-Au-Mo deposits between south and north edges of NCC. Acta Mineralogica Sinica, (S1): 39-40(in Chinese).

Zhang, M., Zhai, Y.S., Shen, C.L., et al., 2011. Metallogenic system of copper polymetallic deposits in the middle-southern part of Da Hinggan Mountains, China. Geoscience, 25(5): 819-831(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-XDDZ201105002.htm

Zhang, Y.B., Sun, S.H., Mao, Q., 2006. Mesozoic O-type adakitic volcanic rocks and its petrogenesis, paleo-tectonic dynamic and mineralization significance of the eastern side of southern Da Hinggan, China. Acta Petrological Sinica, 22(9): 2289-2304 (in Chinese with English abstract). http://www.oalib.com/paper/1472201

Zhao, Y.M., 1997. Metallogeny and prospective evaluation of copper-polymetallic deposits in the Da Hinggan Mountains and its adjacent regions. Earthquake Publishing House, Beijing (in Chinese).

Zhou, Z.H., Liu, H.W., Chang, G.X., et al., 2011. Meneralogical 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). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSKW201101013.htm

陈斌, 赵国春, Wilde, S., 2001. 内蒙古苏尼特左旗南两类花岗岩同位素年代学及其构造意义. 地质论评, 47(4): 361-367. doi: 10.3321/j.issn:0371-5736.2001.04.005

郭利军, 谢玉玲, 侯增谦, 等, 2009. 内蒙古拜仁达坝银多金属矿矿床地质及成矿流体特征. 岩石矿物学杂志, 28(1): 26-36. doi: 10.3969/j.issn.1000-6524.2009.01.004

李锦轶, 1998. 中国东北及邻区若干地质构造问题的新认识. 地质论评, 44(4): 339-347. doi: 10.3321/j.issn:0371-5736.1998.04.002

李锦轶, 高立明, 孙桂华, 等, 2007. 内蒙古东部双井子中三叠同碰撞壳源花岗岩的确定及其对西伯利亚与中朝古板块碰撞时限的约束. 岩石学报, 23(3): 565-582. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200703006.htm

刘家军, 邢永亮, 王建平, 等, 2010. 内蒙拜仁达坝超大型Ag-Pb-Zn多金属矿床中针硫锑铅矿的发现与成因意义. 吉林大学学报(地球科学版), 40(3): 565-572. https://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ201003013.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. doi: 10.3321/j.issn:1005-2321.2004.01.024

吕志成, 段国正, 刘丛强, 等, 2000. 大兴安岭地区银矿床类型、成矿系列及成矿地球化学特征. 矿物岩石地球化学通报, 19(4): 305-309. doi: 10.3969/j.issn.1007-2802.2000.04.037

马星华, 陈斌, 赖勇, 等, 2009. 内蒙古敖仑花斑岩钼矿床成岩成矿年代学及地质意义. 岩石学报, 25(11): 2939-2950. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200911025.htm

聂凤军, 张万益, 杜安道, 等, 2007. 内蒙古小东沟斑岩型钼矿床辉钼矿铼-锇同位素年龄及地质意义. 地质学报, 81(7): 898-905. doi: 10.3321/j.issn:0001-5717.2007.07.004

内蒙古自治区地质矿产局, 1991. 内蒙古自治区区域地质志. 北京: 地质出版社, 128-651.

祁进平, 陈衍景, Pirajno, F., 2005. 东北地区浅成低温热液矿床的地质特征和构造背景. 矿物岩石, 25(2): 47-59. doi: 10.3969/j.issn.1001-6872.2005.02.009

任纪舜, 陈廷愚, 牛宝贵, 等, 1992. 中国东部及邻区大陆岩石圈的构造演化与成矿. 北京: 科学出版社.

石玉若, 刘敦一, 张旗, 等, 2004. 内蒙古苏左旗地区闪长-花岗岩类SHRIMP年代学. 地质学报, 78(6): 789-799. doi: 10.3321/j.issn:0001-5717.2004.06.009

舒启海, 蒋林, 赖勇, 等, 2009. 内蒙古阿鲁科尔沁旗敖仑花斑岩铜钼矿床成矿时代和流体包裹体研究. 岩石学报, 25(10): 2601-2614. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200910024.htm

孙兴国; 刘建明; 覃锋, 等, 2008. 大兴安岭成矿研究新进展——西拉木伦河南岸Mo多金属成矿带的发现. 中国矿业, 17(2) : 75-78. doi: 10.3969/j.issn.1004-4051.2008.02.022

王京彬, 王玉往, 王莉娟, 2000. 大兴安岭中南段铜矿成矿背景及找矿潜力. 地质与勘探, 36(5): 1-4. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKT200005000.htm

王京彬, 徐新. 2006. 新疆北部后碰撞构造演化与成矿. 地质学报, 80(1): 23-31. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200601002.htm

王莉娟, 岛崎英彦, 王京彬, 等, 2001. 黄岗梁矽卡岩型铁锡矿床成矿流体及成矿作用. 中国科学(D辑), 31(7): 553-562. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200107003.htm

夏学惠, 赵玉海, 袁家忠, 等, 2002. 内蒙古林西—天山地区多金属硫化物矿床地质及成矿规律. 化工矿产地质, 24(4): 198-206. doi: 10.3969/j.issn.1006-5296.2002.04.002

徐巧, 付水兴, 袁继明, 等, 2010. 赤峰敖仑花钼铜矿床地质特征及找矿标志. 地质与勘探, 46(6): 1019-1028. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKT201006007.htm

薛怀民, 郭利军, 侯增谦, 等, 2010. 大兴安岭西南坡成矿带晚古生代中期未变质岩浆岩的SHRIMP锆石U-Pb年代学. 岩石矿物学杂志, 29(6): 811-823. doi: 10.3969/j.issn.1000-6524.2010.06.016

曾庆栋, 刘建明, 2010. 西拉沐伦钼矿带半拉山斑岩钼矿床花岗斑岩锆石SHRIMP U-Pb测年及其地质意义. 吉林大学学报(地球科学版), 40(4): 828-834. https://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ201004013.htm

张炯飞, 李之彤, 金成沫, 2004. 中国东北部地区埃达克岩及其成矿意义. 岩石学报, 20(2): 361-368. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200402015.htm

张炯飞, 权恒, 武广, 等, 2000. 东北地区中生代火山岩形成的构造环境. 贵金属地质, 9(1): 33-38. doi: 10.3969/j.issn.1671-1947.2000.01.006

张可, 聂凤军, 侯万荣, 等, 2012. 内蒙古林西县哈什吐钼矿床辉钼矿铼-锇年龄及其地质意义. 矿床地质, 31 (1): 129-138. https://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ201201012.htm

张连昌, 吴华英, 陈志广, 等, 2009. 华北地台南北缘斑岩型铜金钼矿床成矿规律与专属性研究. 矿物学报, (S1): 39-40. https://www.cnki.com.cn/Article/CJFDTOTAL-KWXB2009S1020.htm

张梅, 翟裕生, 沈存利, 等, 2011. 大兴安岭中南段铜多金属矿床成矿系统. 现代地质, 25(5): 819-831. doi: 10.3969/j.issn.1000-8527.2011.05.001

张永北, 孙世华, 毛骞, 2006. 大兴安岭南段东麓中生代O型埃达克质火山岩及其成因、古构造环境和找矿意义. 岩石学报, 22(9): 2289-2304. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200609003.htm

赵一鸣, 1997. 大兴安岭及其邻区铜多金属矿床成矿规律与远景评价. 北京: 地震出版社.

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. doi: 10.3969/j.issn.1000-6524.2011.01.009

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(8) / Tables(3)

Get Citation

PDF

XML

Article views (759) PDF downloads(18)

Metallogenic Granitoid of Aolunhua Mo Deposit at North Bank of Xilamulun River

doi: 10.3799/dqkx.2012.137

Abstract

References

Proportional views

Catalog

通讯作者: 陈斌, bchen63@163.com

Proportional views

Export File

Citation

Format

Content