2020 Vol. 39, No. 7
Article Contents

CHEN Yuke. Chronology and geochemistry of the granitoids in Heri Town, Tongde County, Qinghai Province, and its tectonic significance[J]. Geological Bulletin of China, 2020, 39(7): 1015-1024.
Citation: CHEN Yuke. Chronology and geochemistry of the granitoids in Heri Town, Tongde County, Qinghai Province, and its tectonic significance[J]. Geological Bulletin of China, 2020, 39(7): 1015-1024.

Chronology and geochemistry of the granitoids in Heri Town, Tongde County, Qinghai Province, and its tectonic significance

  • In this study, the author used LA-ICP-MS zircon U-Pb isotopic dating method and obtained weighted average zircon U-Pb age of 229.7±1.0 Ma from the biotite granodiorite in Heri Town, Tongde County, Qinghai Province.The geochemical characteristics show that it belongs to high-K calcium-alkali series, and resulted from partial melting of crustal components, with weak negative Eu anomalies and right-inclined chondrite-normalized REE patterns.Based on a comprehensive analysis of previous researched, the authors hold that the biotite granodiorite was formed in the Late Triassic, and belonged to I-type granite formed in the active continental margin environment before the plane collision.Its genesis was closely related to the northward subduction of the Ańyemagen-Mianlue Ocean.The results obtained by the authors provide a new age constraint for the entrance of West Qinling into the syn-collision stage in the Indosinian.

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  • [1] Meng Q R, Zhang GW.Timing of collision of the North and South China blocks:Controversy and reconciliation[J].Geology, 1999, 27(2):123-126.

    Google Scholar

    [2] 张国伟, 张本仁, 袁学诚, 等.秦岭造山带与大陆动力学[M].北京:科学出版社, 2001:1-806.

    Google Scholar

    [3] 张宏飞, 陈岳龙, 徐旺春, 等.青海共和盆地周缘印支期花岗岩类的成因及其构造意义[J].岩石学报, 2006, 22(12):2910-2922.

    Google Scholar

    [4] 黄雄飞, 莫宣学, 喻学惠, 等.西秦岭宕昌地区晚三叠世酸性火山岩的锆石U-Pb年代学、地球化学及其地质意义[J].岩石学报, 2013, 29(11):3968-3980.

    Google Scholar

    [5] 金维浚, 张旗, 何登发, 等.西秦岭埃达克岩的SHRIMP定年及其构造意义[J].岩石学报, 2005, 21(3):959-966.

    Google Scholar

    [6] 殷勇, 殷先明.西秦岭北缘与埃达克岩和喜马拉雅型花岗岩有关的斑岩型铜-钼-金成矿作用[J].岩石学报, 2009.25(5):1239-1252.

    Google Scholar

    [7] 韦萍, 莫宣学, 喻学惠, 等.西秦岭夏河花岗岩的地球化学、年代学及地质意义[J].岩石学报, 2013, 29(11):3981-3992.

    Google Scholar

    [8] Li X W, Mo X X, Bader T, et al.Petrology, geochemistry and geochronology of the magmatic suite from the Jianzha Complex, central China:Petrogenesis and geodynamic implications[J].Journal of Asian Earth Sciences, 2014, 95C:164-181.

    Google Scholar

    [9] Sun W D, Li S G, Chen Y D, et al.Timing of synorogenic granitoids in the South Qinling, central China:Constraints on the evolution of the Qinling-Dabie Orogenic Belt[J].The Journal of Geology, 2002, 110(4):457-468.

    Google Scholar

    [10] Qin J F, Lai S C, Di C R, et al.Magma mixing origin for the post-collisional adakitic monzogranite of the Triassic Yangba pluton, northwestern margin of the South China block:Geochemistry, Sr-Nd isotopic, zircon U-Pb dating and Hf isotopic evidences[J].Contributions to Mineralogy and Petrology, 2010, 159(3):389-409. doi: 10.1007/s00410-009-0433-2

    CrossRef Google Scholar

    [11] Cao X F, Lü X B, Yao S Z, et al.LA-ICP-MS U-Pb zircon geochronology, geochemistry and kinetics of the Wenquan ore-bearing granites from West Qinling, China[J].Ore Geology Reviews, 2011, 43(1):120-131.

    Google Scholar

    [12] Dong Y P, Zhang G W, Neubauer F, et al.Tectonic evolution of the Qinling orogen, China:Review and synthesis[J].Journal of Asian Earth Sciences, 2011, 41(3):213-237.

    Google Scholar

    [13] Wang T G, Ni P, Sun W D, et al.Zircon U-Pb ages of granites at Changba and Huangzhuguan in western Qinling and implications for source nature[J].Chinese Science Bulletin, 2011, 56(7):659-669. doi: 10.1007/s11434-010-4319-5

    CrossRef Google Scholar

    [14] Zhu L M, Zhang G W, Chen Y J, et al.Zircon U-Pb ages and geochemistry of the Wenquan Mo bearing granitioids in West Qinling, China:Constraints on the geodynamic setting for the newly discovered Wenquan Mo deposit[J].Ore Geology Reviews, 2011, 39(1/2):46-62.

    Google Scholar

    [15] Guo X Q, Yan Z, Wang Z Q, et al.Middle Triassic arc magmatism along the northeastern margin of the Tibet:U-Pb and Lu-Hf zircon characterization of the Gangcha complex in the West Qinling terrane, central China[J].Journal of the Geological Society, 2012, 169(3):327-336. doi: 10.1144/0016-76492011-083

    CrossRef Google Scholar

    [16] 徐学义, 王洪亮, 陈隽璐, 等.西秦岭天水尹道寺中生代酸性火山岩锆石U-Pb定年和元素地球化学研究[J].岩石学报, 2008, 23(11):2845-2856.

    Google Scholar

    [17] 尤继元, 汪泗河, 鱼欣宇, 等.青海省同仁印支期火山岩地球化学特征与构造环境分析[J].地质调查与研究, 2010, 33(4):300-308. doi: 10.3969/j.issn.1672-4135.2010.04.007

    CrossRef Google Scholar

    [18] Li X W, Mo X X, Yu X H, et al.Petrology and geochemistry of the Early Mesozoic pyroxene andesites in the Maixiu area, West Qinling, China:Products of subduction or syn-collison[J].Lithos, 2013, 172-173:158-174 doi: 10.1016/j.lithos.2013.04.010

    CrossRef Google Scholar

    [19] 路远发.GeoKit:一个用VBA构建的地球化学工具软件包[J].地球化学, 2004, 33(5):459-464. doi: 10.3321/j.issn:0379-1726.2004.05.004

    CrossRef Google Scholar

    [20] 李远友, 刘国仁, 于秀斌, 等.新疆准噶尔北缘加玛特金铜矿区辉长岩锆石U-Pb年龄、岩石地球化学特征及地质意义[J].现代地质, 2017, 31(4):651-661. doi: 10.3969/j.issn.1000-8527.2017.04.001

    CrossRef Google Scholar

    [21] 吴元保, 郑永飞, 龚冰, 等.北淮阳庐镇关岩浆岩锆石U-Pb年龄和氧同位素组成[J].岩石学报, 2004, 20(5):1007-1024.

    Google Scholar

    [22] 刘英俊, 曹励明, 李兆麟, 等.元素地球化学[M].北京:科学出版社, 1984:1-548.

    Google Scholar

    [23] 杨瀚文, 申俊峰, 魏立勇, 等.西秦岭西段共和盆地周缘西功卡花岗闪长岩体锆石U-Pb年龄、地球化学特征及其构造意义[J].现代地质, 2018, 32(2):316-328.

    Google Scholar

    [24] 李小江, 李佐臣, 杨拴海, 等.西秦岭西段然果儿岗花岗闪长岩体锆石U-Pb定年及地质意义[J].新疆地质, 2015, 33(3):393-398. doi: 10.3969/j.issn.1000-8845.2015.03.022

    CrossRef Google Scholar

    [25] 杨拴海, 李瑞保, 王伟峰, 等.西秦岭西段曲如沟花岗闪长岩年代学、地球化学特征及构造意义研究[J].西北地质, 2015, 48(2):57-72. doi: 10.3969/j.issn.1009-6248.2015.02.006

    CrossRef Google Scholar

    [26] 王德滋, 刘昌实.桐庐I型和相山S型两类碎斑熔岩对比[J].岩石学报, 1993, 9(1):44-54. doi: 10.3321/j.issn:1000-0569.1993.01.005

    CrossRef Google Scholar

    [27] 路凤香, 桑隆康, 等.岩石学[M].北京:地质出版社, 2002:1-398.

    Google Scholar

    [28] 孟繁聪, 薛怀民, 李天福, 等.苏鲁造山带晚中生代地幔的富集特征——来自辉长岩的地球化学证据[J].岩石学报, 2005, 21(6):1583-1592.

    Google Scholar

    [29] 邓晋福, 罗照华, 苏尚国, 等.岩石成因、构造环境与成矿作用[M].北京:地质出版社, 2004:1-381.

    Google Scholar

    [30] Rapp R P, Watson E B.Dehydration melting of metabasalt at 8~32kbar:Implications for continental growth and crust-mantle recycling[J].J.Petrol., 1995, 36:891-931. doi: 10.1093/petrology/36.4.891

    CrossRef Google Scholar

    [31] 潘桂棠, 陈智梁, 李兴振, 等.东特提斯地质构造形成演化[M].北京:地质出版社, 1997:1-218.

    Google Scholar

    [32] Meng Q R, Wang E, Hu J M.Mesozoic sedimentary evolution of the northwest Sichuan basin:Implication for continued clockwise rotation of the South China block[J].Geological Society of America Bulletin, 2005, 117(3/4):396-410.

    Google Scholar

    [33] 闫臻, 李继亮, 王宗起, 等.西秦岭楔的构造属性及其增生造山过程[J].岩石学报, 2012, 28(6):1808-1828.

    Google Scholar

    [34] 冯益民, 曹宣铎, 张二朋, 等.西秦岭造山带的演化、构造格局和性质[J].西北地质, 2003, 36(1):1-10. doi: 10.3969/j.issn.1009-6248.2003.01.001

    CrossRef Google Scholar

    [35] Jiang Y H, Jin G D, Liao S Y, et al.Geochemical and Sr-Nd-Hf isotopic constraints on the origin of Late Triassic granitoids from the Qinling orogen, central China:Implications for a continental arc to continent-continent collision[J].Lithos, 2010, 117(1):183-197.

    Google Scholar

    [36] Dong Y P, Liu X M, Zhang G W, et al.Triassic diorites and granitoids in the Foping area:Constraints on the conversion from subduction to collision in the Qinling orogen, China[J].Journal of Asian Earth Sciences, 2012, 47:123-142. doi: 10.1016/j.jseaes.2011.06.005

    CrossRef Google Scholar

    陕西地矿区研院有限公司.青海省同德县谷芒地区五幅1:5万区域地质矿产调查.2014.

    Google Scholar

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