ISSN 1009-6248CN 61-1149/P Bimonthly

Supervisor:China Geological Survey

Sponsored by:XI'an Center of China Geological Survey
Geological Society of China

    • The Core Journals of China
    • The Key Magazine of China Technology
    • CSCD Included Journals
    • Scopus Included Journals
Advance Search
HE Yuanfang, ZHANG Zhenkai, GAO Feng, et al. Zircon U-Pb Ages and Geochemical Characteristics of Quartz Diorite Porphyrite from Suoerkuli Area in Altyn Tagh and their Geological Significance[J]. Northwestern Geology, 2018, 51(3): 38-52.
Citation: HE Yuanfang, ZHANG Zhenkai, GAO Feng, et al. Zircon U-Pb Ages and Geochemical Characteristics of Quartz Diorite Porphyrite from Suoerkuli Area in Altyn Tagh and their Geological Significance[J]. Northwestern Geology, 2018, 51(3): 38-52.

Zircon U-Pb Ages and Geochemical Characteristics of Quartz Diorite Porphyrite from Suoerkuli Area in Altyn Tagh and their Geological Significance

More Information
  • Received Date: December 26, 2017
  • Revised Date: March 25, 2018
  • Available Online: July 28, 2022
  • Published Date: September 04, 2018
  • In order to confirm the genesis and formation age of quartz diorite porphyrite from Suoerkuli area in Altyn Tagh, its geochemical characteristics and LA-ICP-MS zircon U-Pb age have been studied in this paper. The LA-ICP-MS zircon U-Pb dating indicates that these quartz diorite porphyrites was formed at (375.7±2.2) Ma. The geochemical data show that these rocks are relatively rich in SiO2 (61.41%~69.93%) and Al2O3 (13.48%~15.57%) contents, but low in TFeO (3.47%~4.53%), MgO (0.66%~1.83%) and CaO (2.81%~4.21%) contents, showing the features of calc-alkaline I-type granites. These rocks have relative high total REE concentration (∑REE=129.32×10-6~253.63×10-6), with fractionated REE[(La/Yb)N=6.25~8.51] and no remarkable Eu anomalies. Furthermore, they are enriched in LILE (e.g. Rb, Pb, Th and U), but depleted in HFSE (e.g. Nb, Ta and Ti). The geochemical characteristics suggest that these quartz diorite porphyrites were generated by the partial melting of basic rocks in lower crust and formed by the fractional crystallization, and the parental magma was caused by the underplating of mantle-derived materials. Based on the regional geological investigations and the spatial-temporal distribution of the coeval igneous rocks, it's considered that the quartz diorite porphyrite was emplaced in a post-orogenic extensional environment, which is related with the strike slip of Altyn Tagh Fault.
  • 曹玉亭, 刘良, 王超,等. 阿尔金南缘塔特勒克布拉克花岗岩的地球化学特征、锆石U-Pb定年及Hf同位素组成[J]. 岩石学报, 2010, 26(11):3259-3271.
    CAO Yuting,LIU Liang, WANG Chao, et al.Geochemiacal, zircon U-Pb dating and Hf isotope compositons studies for Tatelekebulake granite in South Altyn Tagh[J].Acta Petrologica Sinia,2010,26(22):3259-3271.
    车自成, 刘良, 刘洪福,等. 阿尔金山地区高压变质泥质岩石的发现及其产出环境[J]. 科学通报, 1995, 40(14):1298-1298.
    CHE Zichegn, LIU Liang, LIU Hongfu, et al.The discovery of HP metamorphic mudstone and its tectonic setting[J].Chinese Science Bulletin,1995,40(14):1298-1298.
    崔军文, 杨经绥, 李朋武,等. 阿尔金断裂:几何学、性质和生长方式[J]. 地质学报, 2001, 23(2):509-516.
    CUI Junwen, YANG Jingsui, LI Pengwu, et al. Geometry, nature and growth mode of Altyn Fault[J]. Journal of Geology,2001, 23(2):509-516.
    胡云绪, 校培喜, 高晓峰,等. 东昆仑西段-阿尔金地区区域地层划分及地层时空格架建立[J]. 西北地质, 2010, 43(4):152-158.
    HU Yunxu, XIAO Peixi, GAO Xiaofeng, et al. Division and Space-Time Frame Foundation of Regional Stratum in the Western Sector of East Kunlun and Altyn Region[J]. Northewestern Geology,2010, 43(4):152-158.
    康磊, 刘良, 曹玉亭,等. 阿尔金南缘塔特勒克布拉克复式花岗质岩体东段片麻状花岗岩的地球化学特征、锆石U-Pb定年及其地质意义[J]. 岩石学报, 2013, 29(9):3039-3048.
    KANG Lei,LIU Liang,CAO Yuting,et al. Geochemistry,zircon U-Pb age and its geological significance of the gneissic granite from the eastern segment of the Tatelekebulake composite granite in the south Altyn Tagh[J]. Acta Petrologica Sinica,2013, 29(9):3039-3048.
    康磊, 校培喜, 高晓峰,等. 茫崖二长花岗岩、石英闪长岩的年代学、地球化学及岩石成因:对阿尔金南缘早古生代构造-岩浆演化的启示[J]. 岩石学报, 2016, 32(6):1731-1748.
    KANG Lei, XIAO Peixi, GAO Xiaofeng, et al.Chronology,geochemistry and petrogenesis of monzonitic granite and quartz diorite in Mangai area:Its inspiration to Early Paleozoic tectonic-magmatic evolution of the southern Altyn Tagh[J].Acta Petrologica Sinica,2016,32(6):1731-1748.
    刘良, 车自成, 罗金海,等. 阿尔金山西段榴辉岩的确定及其地质意义[J]. 科学通报, 1996, 41(16):1485.
    LIU Liang, CHE Zicheng, LUO Jinhai, et al. The confirmation of eclogite in west sector of Altyn and its implication[J]. Chinses Science Bulletin, 1996, 41(16):1485.
    刘良, 车自成, 王焰,等. 阿尔金高压变质岩带的特征及其构造意义[J]. 岩石学报, 1999(1):57-64.
    LIU Liang, CHE Zicheng, WANG Yan, et al. The petrological charaters and geotectonic setting of high-pressure metamorphic rock belts in Altyn Mountains[J]. Acta Petrologica Sinica,1999(1):57-64.
    刘良, 孙勇, 肖培喜,等. 阿尔金发现超高压(>3.8GPa)石榴二辉橄榄岩[J]. 科学通报, 2002, 47(9):657.
    LIU Liang, SUN Yong, XIAO Peixi, et al. The discovery of ultrahigh pressure granet lerzolite in Altyn Area[J]. Chinses Science Bulletin, 2002, 47(9):657.
    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.
    MO Xuanxue, LUO Zhaohua, DENG Jinfu, et al. Granitoids and Crustal Grouth in the East-Kunlun Orogenic Belt[J]. Geological Journal of China Universities. 2007, 13(3):403-414.
    邱检生, 胡建, 王孝磊,等. 广东河源白石冈岩体:一个高分异的Ⅰ型花岗岩[J]. 地质学报, 2005, 79(4):503-514.
    QIU Jiansheng, HU Jian, WANG Xiaolei, et al. The Baishigang Pluton in Heyuan, Guangdong Province:A Highly Fractionated I-type Granite[J]. Acta Geoglocia Sinica.2005, 79(4):503-514.
    宋忠宝, 任有祥, 李智佩,等. 北祁连山西段巴个峡-黑大坂一带几个花岗闪长岩体的侵入时代讨论——兼论古阿尔金断裂活动时间[J]. 地球学报, 2004, 25(2):205-208.
    SONG Zhongbao, REN Youxiang, LI Zhipei, et al. A disscussion on intrusion epoches of granodiorites along the Bagexia-Heidaban Zone in the western part of the North Qilian Mountains[J]. Acta Geosicientica Sinica. 2004, 25(2):205-208.
    孙吉明, 马中平, 唐卓,等. 阿尔金南缘鱼目泉岩浆混合花岗岩LA-ICP-MS测年与构造意义[J]. 地质学报, 2012, 86(2):247-257.
    SUN Jimign, MA Zhongping, TANG Zhuo, et al. LA-ICP-MS zircon dating of the Yumuquan magma mixing granite in the Southern Altyn Tagh and its tectonic significance[J]. Acta Geologica Sinica.2012, 86(2):247-257.
    王超, 刘良, 张安达,等. 阿尔金造山带南缘岩浆混合作用:玉苏普阿勒克塔格岩体岩石学和地球化学证据[J]. 岩石学报, 2008, 24(12):2809-2819.
    WANG Chao, LIU Liang, ZhANG Anda, et al. Geochemistry and petrography of Early Paleozoic Yusupuleke Tagh rapakivi-textured granite complex, South Altyn:An example fro magma mixing[J]. Acta Petrologica Sinica,2008, 24(12):2809-2819.
    王德滋, 沈渭洲. 中国东南部花岗岩成因与地壳演化[J]. 地学前缘, 2003, 10(3):209-220.
    WANG Dezi, SHEN Weizhou. Genesis of granitoids and crustal evolution in southeast China[J]. Earth Science Frontiers,2003, 10(3):209-220.
    吴才来, 郜源红, 雷敏,等. 南阿尔金茫崖地区花岗岩类锆石SHRIMP U-Pb定年、Lu-Hf同位素特征及岩石成因[J]. 岩石学报, 2014, 30(8):2297-2323.
    WU Cailai, GAO Yuanhong, LEI Min, et al. Zircon SHRIMP U-Pb dating, Lu-Hf isotopic characteristics and petrogenesis of the Palaozoic granites in Mangya area, southern Altun, NW China[J].Acta Petrologcia Sinica,2014, 30(8):2297-2323.
    吴福元, 李献华, 杨进辉,等. 花岗岩成因研究的若干问题[J]. 岩石学报, 2007, 23(6):1217-1238.
    WU Fuyuan, LI Xianhua, YANG Jinhui, et al. Discussions on the petrogenesis of granites[J]. Acta Petrologica Sinica,2007, 23(6):1217-1238.
    吴锁平, 吴才来, 陈其龙. 阿尔金断裂南侧吐拉铝质A型花岗岩的特征及构造环境[J]. 地质通报, 2007, 26(10):1385-1392.
    WU Suoping, WU Cailai, CHEN Qilong. Characteristics and tectonic setting of the Tula aluminous A-type granite at the south side of the Altyn fautl, NW China[J]. Geological Bulletion of China,2007, 23(6):1217-1238.
    肖庆辉, 邢作云, 张昱,等. 当代花岗岩研究的几个重要前沿[J]. 地学前缘, 2003, 10(3):221-229.
    XIAO Qinghui, XING Zuoyun, ZHANG Yu, et al. The major frontiers of the recent studies of granite[J]. Earth Science Frontiers, 2003, 10(3):221-229.
    许志琴,杨经绥,张建新,等. 阿尔金断裂两侧构造单元的对比及岩石圈剪切机制[J]. 地质学报, 1999(3):193-205.
    XU Zhiqin, YANG Jingsui, ZHANG Jianxin, et al. A comparison between the tectonic units on the two sides of the Altun sinistral strike-slip fault and the mechanism of lithospheric shearing[J]. Acta Geologica Sinica, 1999(3):193-205.
    杨文强,刘良,丁海波,等. 南阿尔金迪木那里克花岗岩地球化学、锆石U-Pb年代学与Hf同位素特征及其构造地质意义[J]. 岩石学报, 2012, 28(12):4139-4150.
    YANG Wenqiang, LIU Liang, DING Haibo, et al. Geochemistry, geochronolgoy and zircon Hf isotopes of the Dimunalike granite in South Altyn Tagh and its geological significance[J]. Acta Pertologica Sinica,2012, 28(12):4139-4150.
    张旗,李承东. 花岗岩:地球动力学意义[M]. 北京:海洋出版社,2012, 1-276
    ZHANG Qi, LI Chengdong. Granitoids:the geodynamic significance[M]. Beijing:Maritime Press, 2012,1-276.
    周勇, 潘裕生. 阿尔金断裂早期走滑运动方向及其活动时间探讨[J]. 地质论评, 1999, 45(1):1-9.
    ZHOU Yong, PAN Yusheng. The initial shear sense of the Altun Fault and its timing[J].Geological Review,1999, 45(1):1-9.
    朱弟成, 莫宣学, 王立全,等. 西藏冈底斯东部察隅高分异I型花岗岩的成因:锆石U-Pb年代学、地球化学和Sr-Nd-Hf同位素约束[J]. 中国科学:地球科学, 2009, 39(7):833-348.
    ZHU Dicheng, MO Xuanxue, WANG Liquan, et al. The genesis of high fractionated granite:zircon U-Pb dating, geochemistry and Sr-Nd-Hf isotope[J]. Chinese Sciecne Bulletin. 2009, 39(7):833-348.
    BATCHELOR R A, BOWDEN P. Petrogenetic interpretation of granitoid rock series using multicationic parameters[J]. Chemical Geology, 1985, 48(1):43-55.
    BONIN B. A-type granites and related rocks:Evolution of a concept, problems and prospects[J]. Lithos, 2007, 97(1):1-29.
    BUROV E, JAUPART C, MARESCHAL J C. Large-scale crustal heterogeneities and lithospheric strength in cratons[J]. Earth & Planetary Science Letters, 1998, 164(1-2):205-219.
    CHAPPELL B W. Two contrasting granite type[J]. Pacific Geology, 1974, 8:173-174.
    EDWARD R S, NICOLAS ARNAUD. A possible middle Paleozoic suture in the Altyn Tagh, NW China[J]. Tectonics, 1999, 18(1):64-74.
    HOFMANN A W. Chemical differentiation of the Earth:the relationship between mantle, continental crust, and oceanic crust[J]. Earth & Planetary Science Letters, 1988, 90(3):297-314.
    JAHN B M, WU F, HONG D. Important crustal growth in the Phanerozoic:Isotopic evidence of granitoids from east-central Asia[J]. Journal of Earth System Science, 2000, 109(1):5-20.
    JAHN B M, WU F, LO C H, et al. Crust-mantle interaction induced by deep subduction of the continental crust:geochemical and Sr-Nd isotopic evidence from post-collisional mafic-ultramafic intrusions of the northern Dabie complex, central China[J]. Chemical Geology, 1999, 365(2-3):119-146.
    KANG, LIANG WANG, et al. Geochemistry and Zircon U-Pb Dating of Changshagou Adakite from the South Altyn UHPM Terrane:Evidence of the Partial Melting of the Lower Crust[J]. Acta Geologica Sinica, 2014, 88(5):1454-1465.
    KING P L, WHITE A J R, CHAPPELL B W, et al. Characterization and Origin of Aluminous A-type Granites from the Lachlan Fold Belt, Southeastern Australia[J]. Journal of Petrology, 1997, 38(3):371-391.
    LI X H, LI Z X, LI W X, et al. U-Pb zircon, geochemical and Sr-Nd-Hf isotopic constraints on age and origin of Jurassic I-and A-type granites from central Guangdong, SE China:A major igneous event in response to foundering of a subducted flat-slab?[J]. Lithos, 2007, 96(1):186-204.
    LIEGEOIS J P, NAVEZ J, HERTOGEN 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(1-4):1-28.
    LIU M. Cenozoic extension and magmatism in the North American Cordillera:the role of gravitational collapse[J]. Tectonophysics, 2001, 342(3):407-433.
    MCLENNAN B. The continental crust:its composition and evolution[M]. Blackwell scientific publication, 1985.1-312.
    MILLER C F, MCDOWELL S M, MAPES R W. Hot and cold granites? Implications of zircon saturation temperatures and preservation of inheritance[J]. Geology, 2003, 31(6):529-532.
    PEARCE J A, HARRIS N B W, TINDLE A G. Trace Element Discrimination Diagrams for the Tectonic Interpretation of Granitic Rocks[J]. Journal of Petrology, 1984, 25(4):956-983.
    PITCHER W S. Granites and yet more granites forty years on[J]. Geologische Rundschau, 1987, 76(76):51-79.
    RUDNICK R L, FOUNTAIN D M. Nature and composition of the continental crust:A lower crustal perspective[J]. Reviews of Geophysics, 1995, 33(3):267-309.
    RYERSON F J, WATSON E B. Rutile saturation in magmas:implications for Ti, Nb, Ta depletion in island-arc basalts[J]. Earth & Planetary Science Letters, 1987, 86(2-4):225-239.
    SCHOTT B, YUEN D A, SCHMELING H. The significance of shear heating in continental delamination[J]. Physics of the Earth & Planetary Interiors, 2000, 118(3):273-290.
    SUN S S, MCDONOUGH W F. Chemical and isotopic systematics of oceanic basalts:implications for mantle composition and processes[J]. Geological Society London Special Publications, 1989, 42(1):313-345.
    SUPPE J, HUBERT A, WANG X. Geological Society of America Abstract with Programs[M]. 2002.
    WATSON E B, HARRISON T M. Zircon saturation revisited:temperature and composition effects in a variety of crustal magma types[J]. Earth & Planetary Science Letters, 1983, 64(2):295-304.
    WHALEN J B, CYRRIE K L, CHAPPELL B W. A-type granites:geochemical characteristics, discrimination and petrogenesis[J]. Contributions to Mineralogy & Petrology, 1987, 95(4):407-419.
    WRIGHT J B. A simple alkalinity ratio and its application to question of non-orogenic granite geneses[J]. Geological Magazine, 1969, 106(4):370-384.
    WU F Y, JAHN B M, WILDE S A, et al. Highly fractionated I-type granites in NE China (I):geochronology and petrogenesis[J]. Lithos, 2003, 66(3):241-273.
    XU Y G. Thermo-tectonic destruction of the archaean lithospheric keel beneath the Sino-Korean Craton in China:Evidence, timing and mechanism[J]. Physics and Chemistry of the Earth Part A-Solid Earth and Geodesy, 2001, 26(9-10):747-757.
    YAMASAKI T. Localized rheological weakening by grain-size reduction during lithospheric extension[J]. Tectonophysics, 2004, 386(3):117-145.
    YANG H, GE W, ZHAO G, et al. Early Permian-Late Triassic granitic magmatism in the Jiamusi-Khanka Massif, eastern segment of the Central Asian Orogenic Belt and its implications[J]. Gondwana Research, 2015, 27(4):1509-1533.
    YUAN H, GAO S, LIU X, et al. Accurate U-Pb Age and Trace Element Determinations of Zircon by Laser Ablation-Inductively Coupled Plasma-Mass Spectrometry[J]. Geostandards & Geoanalytical Research, 2010, 28(3):353-370.
    ZHOU D, GRAHAM S A. Extrusion of the Altyn Tagh wedge:A kinematic model for the Altyn Tagh fault and palinspastic reconstruction of northern China[J]. Geology, 1996, 24(5):427.
  • Related Articles

Catalog

    Article views (2117) PDF downloads (2644) Cited by()

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return