Xi'an Center, China Geological SurveyHost
Advanced Search
Previous Article Next Article
2020 Vol. 53, No. 4
Article Contents
Article navigation > Northwestern Geology > 2020 > 53(4): 34-50
Next Article Previous Article

LI Weihong, WANG Jun, LI Xiaoqiang, WANG Yuxi. 2020. Chronology, Geochemical Characteristics of the Intermediate Acid Intrusives in Dangjinshankou, Eastern Altun and Their Tectonic Significance. Northwestern Geology, 53(4): 34-50. doi: 10.19751/j.cnki.61-1149/p.2020.04.004
Citation: LI Weihong, WANG Jun, LI Xiaoqiang, WANG Yuxi. 2020. Chronology, Geochemical Characteristics of the Intermediate Acid Intrusives in Dangjinshankou, Eastern Altun and Their Tectonic Significance. Northwestern Geology, 53(4): 34-50. doi: 10.19751/j.cnki.61-1149/p.2020.04.004
shu

Chronology, Geochemical Characteristics of the Intermediate Acid Intrusives in Dangjinshankou, Eastern Altun and Their Tectonic Significance

  • 1. Gansu Geology and Minerals Scientific Information Center, Lanzhou 730000, Gansu, China;

  • 2. Geology Survey of Gansu Province, Lanzhou 730000, Gansu, China;

  • 3. Third Institute Geology and Mineral Exploration of Gansu Province, Bureau of Geology and Mineral Rosources, Lanzhou 730050, Gansu, China

Received Date:  12 December 2019
Revised Date:  21 August 2020
    Abstract
  • The Dangjinshankou intrusive body in eastern Altun is mainly composed of granite, granodiorite and diorite. LA-ICP-MS zircon U-Pb isotopic dating shows that the weighted average age of 206Pb/238U of Dangjinshankou granite is (518±13) Ma, indicating that the emplacement age is early Cambrian. Geochemistry shows that the rock mass has a high content of sio2, and the average content of total alkali Na2O + K2O is 6.46%. The rock is rich in both sodium and potassium, but mainly rich in sodium, with low content of Fe2O3, P2O5 and MgO. The total amount of rare earth elements ∑REE is 47.28×10-6-368.74×10-6, with an average value of 225.37×10-6. As a whole, the heavy and light rare earth fractionation is obvious, δEu is 0.45-1.08, with an average value of 0.83. Negative europium is slightly anomaly， high field strength elements are enriched, and large ion lithophile elements are depleted. In HFSE elements Th, Ce, Zr, Hf are enriched while Nb, Ta are slightly depleted. In LILE elements Ba, Sr, Eu appear depleted. Rb shows strong enrichment. The granite belongs to quasi aluminous peraluminous rocks of calc-alkaline high-K calc-alkaline series. The analysis of petrogenesis and tectonic environment indicates that the intrusions in this area may form under the environment of subduction volcanic arc and later syn-collision, with the partially melted basic rocks of amphibolite facies and the participation of mantle materials. The regional geological data shows that Dangjinshankou intrusive body has a lot in common with the granitic magma activities and tectonic setting in the ophiolite belt and the Qilian orogenic belt.
    • FullText(HTML)
  • 加载中
    • References
  • 车自成,刘良,孙勇.阿尔金铅钕锶氩氧同位素研究及其早期演化[J].地球学报,1995,16(3):334-337.

    Google Scholar

    CHE Zicheng, LIU Liang, SUN Yong. U-Pb, Sm-Nd, Rb-Sr, 40Ar/39Ar and 18O/16O isotopic studies for early evolution of the structural belt in Altun Area[J]. Acta Geoscientia Sinica, 1995, 16(3):334-337.

    Google Scholar

    车自成,罗金海,刘良.中国及邻区大地构造学[M].北京:科学出版社, 2002,354-386.

    Google Scholar

    CHE Zicheng,LUO Jinhai,LIU Liang. Geotectonics of China and its adjacent area[M].Beijing:Science Press, 2002,354-386.

    Google Scholar

    陈柏林,崔玲玲,白彦飞,等.阿尔金断裂走滑位移的确定——来自阿尔金山东段构造成矿带的新证据[J].岩石学报,2010,26(11):3387-3396.

    Google Scholar

    CHEN Bailin, CUI Linlin, BAI Yanfei, et al. A determining on the displacement of the Altun Tagh sinistral strike-slip fault, NW China:New evidence from the tectonic metallogenetic belt in the eastern part of Altun Tagh Mountains[J].Acta Petrologica Sinica, 2010,26(11):3387-3396.

    Google Scholar

    陈宣华,尹安,George Gehrels,等.阿尔金山东段地质热年代学与构造演化[J].地学前缘,2009,16(3):207-219.

    Google Scholar

    CHEN Xuanhua, YIN An, GEHRELS G, et al. Geothermochronology and tectonic evolution of Eastern Aityn Tagh Mountains, Northwestern China[J]. Earth Science Frontiers, 2009,16(3):207-219.

    Google Scholar

    陈宣华,George Gehrels,王小风,等.阿尔金山北缘花岗岩的形成时代及其构造环境探讨[J].矿物岩石地球化学通报,2003.22(4):294-298.

    Google Scholar

    CHEN Xuanhua, GEHRELS G, WANG Xiaofeng, et al. Granite from North Altyn Tagh, NW China:U-Pb geochronology and tectonic setting[J]. Bulletin of Mineralogy Petrology and Geochemistry, 2003, 22(4):294-298.

    Google Scholar

    崔军文,唐哲民,邓晋福,等.阿尔金断裂系[M].北京:地质出版社,1999,1-249.

    Google Scholar

    CIU Junwen, TANG Zhemin, DENG Jinfu, et al. Altyn Tagh Fault System[M]. Beijing:Geological Publishing House,1999, 1-249.

    Google Scholar

    葛肖虹,刘永江,任收麦,等.对阿尔金断裂科学问题的再认识[J].地质科学,2001, 36(3):319-325.

    Google Scholar

    GE Xiaohong, LIU Yongjiang, REN Shoumai, et al. Re-understanding on some academic problems of the Altun fault[J]. Chinese Journal of Geology, 2001, 36(3):319-325.

    Google Scholar

    郭召杰,张志诚,王建君.阿尔金山边缘蛇绿岩带的Sm-Nd等时线年龄及其大地构造意义[J]. 科学通报,1998,43(18):1981-1984.

    Google Scholar

    GUO Zhaojie, ZHANG Zhicheng, WANG Jianjun. Sm-Nd isochron age of ophiolite along northern margin of Altun Tagh mountain and its tectonic significance[J]. Chinese Science Bulletin, 1998, 43(18):1981-1984.

    Google Scholar

    康磊,校培喜,高晓峰,等.西昆仑慕士塔格岩体的岩石地球化学特征_岩石成因及其构造[J].地质通报,2012,31(12):2001-2014.

    Google Scholar

    KANG Lei, XIAO Peixi, GAO Xiaofeng, et al. Geochemical characteristics and petrogenesis of Muztagata intrusion in Western Kuniun orogenic belt and their tectonic significance[J]. Geologcal Bulletinof China, 2012, 31(12):2001-2014.

    Google Scholar

    刘良,车自成,王焰,等.阿尔金芒崖地区早古生代蛇绿岩的Sm-Nd等时线年龄证据[J].科学通报,1998.43(8):880-883.

    Google Scholar

    LIU Liang, CHE Zicheng, WANG Yan, ed al. The evidence of Sm-Nd isochron age for the Early Paleozoic ophiolite in Mangya area, Altun Mountains[J]. Chinese Science Bulletin, 1998, 43(8):880-883.

    Google Scholar

    刘良,车自成,王焰,等.阿尔金高压变质带的特征及其构造意义[J].岩石学报,1999.15(1):57- 64.

    Google Scholar

    LIU Liang, CHE Zicheng, WANG Yan, et al. The evidences of Sm-Nd isochron age for the Early Paleozoic ophiplite in Mangya area, Altun Mountain[J]. Acta Petrologica Sinica, 1999, 15(1):57-64.

    Google Scholar

    刘良,康磊,曹玉亭,等.南阿尔金早古生代俯冲碰撞过程中的花岗质岩浆作用[J].中国科学(地球科学),2015, 45(8):1126-1137

    Google Scholar

    LIU Liang,KANG Lei, CAO Yutin, et al. Early Paleozoic granitic magmatism related to the processes from subduction to collision in South Altyn, NW China[J]. Scientia Sinica Terrae, 2015, 45(8):1126-1137.

    Google Scholar

    刘明强,朱永新.甘肃北山红岩井西南似斑状二长花岗岩LA-ICP-MS锆石U-Pb定年及其地质意义[J].西北地质,2018,(1):23-33.

    Google Scholar

    LIU Mingqiang, ZHU Yongxin. Zircon LA-ICP-MS U-Pb Dating of the orphyritic monzonitic granite from Southwest Hongyanjing in Beishan Area, Gansu Province and its significance[J]. Northwestern Geology, 2018,(1):23-33.

    Google Scholar

    刘文强,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.

    Google Scholar

    LIU Wenqiang, LIU Liang, DING Haibo, et al. Geochemistry, geochronology and zircon Hf isotopes of the Dimunalike granite in South Altyn Tagn and its geological significance[J]. Acta Petrologica Sinica, 2012, 28(12):4139-4150.

    Google Scholar

    刘永江,NEUBAUER F, 葛肖虹, 等. 阿尔金断裂带年代学和阿尔金山隆升[J]. 地质科学, 2007, 42(1):134-146.

    Google Scholar

    LIU Yongjiang, NEUBAUER F, GE Xiaohong, et al. Geochronology of the Altun fault zone and rising of the Altun mountains[J]. Chinese Journal of Geology, 2007, 42(1):134-146.

    Google Scholar

    刘永顺,于海峰,辛后田,等.阿尔金山地区构造单元划分和前寒武纪重要地质事件[J].地质通报,2009.28(10):1430-1438

    Google Scholar

    LIU Yongshun, YU Haifeng, XIN Houtian, et al. Tectonic units division and Precambrian significant geological events in Altyn Tagh Mountain, China[J]. Geological Bulletin of China, 2009, 28(10):1430-1438.

    Google Scholar

    陆松年,袁桂邦.阿尔金山阿克塔什塔格早前寒武纪岩浆活动的年代学证据[J].地质学报,2003,77(1):61-68.

    Google Scholar

    LU Songnian, YUAN Guibang. Geochronology of early Precambrian magmatic activities in Aketashitage, east Altyntage[J]. Acta Geologica Sinica, 2003, 77(1):61-68.

    Google Scholar

    戚学祥,吴才来,李海兵.北阿尔金喀孜萨依花岗岩锆石SHRIMP U-Pb定年及其构造意义[J].岩石学报,2005,21(3):859-866.

    Google Scholar

    QI Xuexiang, WU Cailai, LI Haibing. SHRIMP U-Pb age of zircons from Kazisayi granite in the Northern Alty Tagh mountains and its signification[J]. Acta Petrologica Sinica, 2005, 21(3):859-866.

    Google Scholar

    邱检生,肖娥,胡建,等.福建北东沿海高分异I型花岗岩的成因:锆石U-Pb年代学、地球化学和Nd-Hf同位素制约[J].岩石学报,2008,24(11):2468-2684.

    Google Scholar

    QIU Jiansheng, XIAO E, HU Jian, et al. Petrogenesis of highly fractionated I-type granites in the coastal area of northeastern Fujian Province:Constraints from zircon U-Pb geochronology, geochemistry and Nd-Hf isotopes[J]. Acta Petrologica Sinica, 2008,24(11):2468-2684.

    Google Scholar

    万景林,王瑜,李齐,等.阿尔金山北段晚新生代山体抬升的裂变径迹证据[J].矿物岩石地球化学通报,2001,20(4):222-224.

    Google Scholar

    WAN Jinglin, WANG Yu, LI Qi, et al. FT Evidence of Late Cenozoic uplift in Northern Altyn[J]. Bulletin of Mineralogy Petrology and Geochemistry, 2001, 20(4):222-224.

    Google Scholar

    王国良,陈发彬,李五福,等.北-中祁连过渡带龙王山花岗岩体与花石峡钨钼矿关系讨论[J].西北地质,2018,(4):227-243.

    Google Scholar

    WANG Guoliang, CHEN Fabin, LI Wufu, et al. Discussion on the relationship between the Longwangshan granite mass and the Huashixia W Mo deposit in the transitional belt of Northern Central Qilian[J]. Northwestern Geology, 2018,(4):227-243.

    Google Scholar

    王鸿祯,王自强,朱鸿,等.中国晚元古代构造及古地理[J].地质科学,1980,(2):103-111.

    Google Scholar

    WANG Hongzhen, WANG Ziqiang, ZHU Hong, et al. Late Proterozoic structure and palaeogeography of China[J]. Chinese Journal of Geology, 1980, (2):103-111.

    Google Scholar

    王立社,杨鹏飞,段星星,等.阿尔金南缘中段清水泉斜长花岗岩同位素年龄及成因研究[J].岩石学报,2016,32(3):759-774.

    Google Scholar

    WANG Lishe, YANG Pengfei, DUAN Xingxing, et al. Isotopic age and genesis of plagiogranite from Qingshuiquan area in the middle of South Altyn Tagh[J]. Acta Petrologica Sinica, 2016,32(3):759-774.

    Google Scholar

    王立社,张巍,段星星,等.阿尔金环形山花岗片麻岩同位素年龄及成因研究[J].岩石学报,2015,31(1):119-132.

    Google Scholar

    WANG Lishe, ZHANG Wei, DUAN Xingxing, et al. Isotopic age and genesis of the monzogranitic gneiss at the Huanxingshan in middle Altyn Tagh[J]. Acta Petrologica Sinica, 2015, 31(1):119-132.

    Google Scholar

    王焰,刘良,车自成,等.阿尔金茫崖地区早古生代蛇绿岩的地球化学特征[J].地质评论,1999,45(增刊):1010-1014.

    Google Scholar

    WANG Yan,LIU Liang,CHE Zicheng, et al. Geochemical characteristics of Early Paleozoic ophiolite in Mangnai area, Altun Mountains[J]. Geological Review, 1999, 45(S1):1010-1014.

    Google Scholar

    王玉玺,第鹏飞,陈万峰,等.塔里木板块东南缘多坝沟金矿区花岗岩类年代学、地球化学特征及找矿意义[J].西北地质, 2017a, 50(1):134-150.

    Google Scholar

    WANG Yuxi, DI Pengfei, CHEN Wanfeng, et al. Geochemical characteristics and prospecting significance of granites from Duobagou gold deposit in the southeastern Tarim Basin[J]. Northweatern Geology, 2017a, 50(1):134-150.

    Google Scholar

    王玉玺,王金荣,周小玲,等. Columbia 超大陆裂解:来自塔里木克拉通东南缘大红山A型花岗岩的证据[J].地质学报, 2017b, 91(11):2369-2386.

    Google Scholar

    WANG Yuxi, WANG Jinrong, ZHOU Xiaoling, et al. The cracking of Columbia supercontinent from the evidence of the Dahongshan A-type granites in the southeastern Tarim Craton[J]. Acta Geologica Sinica, 2017b, 91(11):2369-2386.

    Google Scholar

    吴才来,姚尚志,曾令森,等.北阿尔金巴什考供-斯米尔布拉克花岗杂岩特征及锆石SHRIMP U-Pb定年[J].中国科学(D辑),2007,37(1):10-26.

    Google Scholar

    WU Cailai, YAO Shangzhi, ZENG Lingseng, et al. Characteristics and zircon SHRIMP U-Pb dating of theBashkaogong Smilbulak granite complex in North Altyn[J]. Chinese Science(D), 2007, 37(1):10-26.

    Google Scholar

    吴才来,徐学义,高前明.北祁连早古生代花岗质岩浆作用及构造演化[J].岩石学报,2010,26(4):1027-1044.

    Google Scholar

    WU Cailai, XU Xueyi, GAO Qianming.Early Palaezoic granitoid magmatism and tectonic evolution in North Qilian, NW China[J]. Acta Petrologica Sinica, 2010, 26(4):1027-1044.

    Google Scholar

    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.

    Google Scholar

    WU Fuyuan, LI Xianhua, YANG Jinhui, et al. Discussions on the petrogenesis of granites[J]. Acta Petrologica Sinica, 2007, 23(6):1217-1238.

    Google Scholar

    伍跃中,王战,过磊,等.阿尔金山西南段花岗岩类的时空变化与构造作用——来自钾钠含量变化的证据[J].大地构造与成矿学,2009,33(4):537-587.

    Google Scholar

    WU Yuezhong, WANG Zhan, GUO Lei, et al. Tectoniccontrol for temporal and spatial variation of granitoids in southwest sector of Altyn Mountains:Evidence from changes of potassium and sodium in granitoids[J]. Geotectonica et Metallogenia, 2009, 33(4):537-587.

    Google Scholar

    校培喜.阿尔金山中段苏吾什杰岩体(群)地质特征[J].西北地质,2003,36(3):14-23.

    Google Scholar

    XIAO Peixi. The geological features of Suwushijie rockbody (group) in Altyn Tagh middle-zone[J]. Northwestern Geology, 2003, 36(3):14-23.

    Google Scholar

    肖庆辉,邱瑞照,邓晋福,等.中国花岗岩与大陆地壳生长方式初步研究[J].中国地质,2005,32(3):343-352.

    Google Scholar

    XIAO Qinghui, QIU Ruizhao, DENG Jinfu, et al. Granitoids and continental crustal growth modes in China[J]. Chinese Geology, 2005, 32(3):343-352.

    Google Scholar

    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, 73(3):193-205.

    Google Scholar

    XU Zhiqin, YANG Jingsui, ZHANG Jianxin, et al. A comparison between the tectonic units on the sides of the Altun sinistral strike-slip fault and the mechanism of lithospheric shearing[J]. Acta Geologica Sinica, 1999, 73(3):193-205.

    Google Scholar

    杨屹,陈宣华,GEHRELS G,等.阿尔金山早古生代岩浆活动与金成矿作用[J].矿床地质,2004.23(4):464-472.

    Google Scholar

    YANG Yi, CHEN Xuanhua, GEHRELS G, et al. Early Paleozoic magmatism and gold metallogenesis in Altun Mountains, Northwest China[J]. Mineral Deposits, 2004, 23(4):464-472.

    Google Scholar

    张安达,刘良,孙勇,等.阿尔金超高压花岗质片麻岩中锆石SHRIMP U-Pb定年及其地质意义[J].科学通报,2004,49(22):2335-2341.

    Google Scholar

    ZHANG Anda, LIU Liang, SUN Yong,et al. SHRIMP U-Pb zircon ages for the UHP metamorphosed granitoid gneiss in Altyn Tagh and their geological significance[J]. Chinese Science Bulletin, 2004, 49(22), 2335-2341.

    Google Scholar

    张旗,潘国强,李承东,等.花岗岩构造环境问题关于花岗岩研究的思考之三[J].岩石学报,2007,23(11):2683-2698.

    Google Scholar

    ZHANG Qi, PAN Guoqiang, LI Chendong, et al. Are discrimination diagrams always indicative of correct technic settings of granites? Some crucial questions on granite study (3)[J]. Acta Petrologica Sinica, 2007, 23(11):2683-2698.

    Google Scholar

    菅坤坤,刘向东,何元方,等. 阿尔金中段大通沟花岗岩体年代学、地球化学特征及其成因[J]. 中国地质, 2018, 45(4):740-752.

    Google Scholar

    JIAN Kunkun,LIU Xiangdong,HE Yuanfang,et al. Geochronology, geochemistry and petrogenesis of the Datonggou granitic plutons in the middle section of Altun Mountains[J]. Geology in China, 2018, 45(4):740-752(in Chinese with English abstract).

    Google Scholar

    郑健康. 阿尔金造山带东段地质构造演化概论[J]. 青海地质,1995,4(2):1-10.

    Google Scholar

    ZHENG Jiankang. Outline of geological tectonic evolution in the eastern Altun orogenic belt[J]. Qinghai Geology, 1995, 4(2):1-10.

    Google Scholar

    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.

    Google Scholar

    ZHOU Yong, PAN Yusheng. Theinitial shear sense of the Allun Fault and its timing[J]. Geological Review, 1999,45(1):1-9.

    Google Scholar

    国家地震局《阿尔金活动断裂带》课题组.阿尔金活动断裂带[M].北京:地震出版社,1992.

    Google Scholar

    Research group of Altun active fault zone, State Seismological Bureau. Altun active fault belt[M]. Beijing:Earthquake Press,1992.

    Google Scholar

    ANDERSEN T. Correction of common lead in U-Pb analyses that do not report204Pb[J]. Chemical Geology, 2002, 192(1):59-79.

    Google Scholar

    BARTH M G, MC DONOUGH W F, RUDNICK R L. Tracking the budget of Nb and Ta in the continental crust[J].Chemical Geology,2000,165(3/4):197-213.

    Google Scholar

    BURCHFIEL B C, DENG Q, MOLNAR P, et al. Intracrustal de-tachment with zones of continentaldeformation[J]. Geology, 1989, 17:748-752.

    Google Scholar

    CHAPPELL B W, WHITE A J R. Two contrasting granite type[J]. Pacific Geol, 1974, (8):173-174.

    Google Scholar

    COLLINS W J, BEAMS D, White A J R, et al. Nature and origin of A type granites with particular reference to south-eastern Australia[J]. Contrib Mineral Petrol, 1982, (80):189-200.

    Google Scholar

    FRANCALANCI L, TAYLORSR S R, MCCULLOCH M T. Geochemical and iso-topic variations in the calcalkaline rocks of Aeolian arc, southern Tyrrhenian Sea, Italy:constraints on magma genesis[J]. Contrib Mineral Petrol, 1993, 113:300-313.

    Google Scholar

    GREEN T H, PEARSON N J. An experimental study of Nb and Ta partitioning between Ti-rich minerals and silicate liquids at high pressure and temperature[J]. Geochimica Et Cosmochimica Acta, 1987,51 (1):55-62.

    Google Scholar

    GREEN T H. Significance of Nb/Ta as an indicator of geochemical processes in the crust-mantle system[J]. Chemical Geology, 1995,120(3-4):347-359.

    Google Scholar

    JACKSON S E, PEARSON N J, GRIFFIN W L, et al. The application of laser ablation-inductively coupled plasma-mass spectrometry to in situ U-Pb zircon geochronology[J]. Chemical Geology, 2004, 211(1):47-69.

    Google Scholar

    JUNG S, PFANDER J A. Source composition and melting temperatures of orogenic granitoid:constraints from CaO/Na2O, Al2O3/TiO2 and accessory mineral saturation thermometry[J]. European Journal of Mineralogy, 2007, 19:859-870.

    Google Scholar

    LIU Liang, WANG Chao, CAO Yuting, et al. Geochronology of multi-stage metamorphic events:Constraintson episodic zircon growth from the UHP eclogite in the South Altyn,NW China[J].Lithos,2012.136-139:10-26.

    Google Scholar

    LIU Sheng, HU Ruizhong, GAO Shan, et al. U-Pb zircon, geochemical and Sr-Nd-Hf isotopic constraints on age and origin of Jurassic I and Atype granites from central Guangdong, SE China:A major igneousevent in response to foundering of a subducted flat-slab?[J]. Lithos, 2007, 96(1-2):186-204.

    Google Scholar

    LIU Y J, GENSER J, GE X H, NEUBAUER F, et al. 40Ar/39 Ar age evidence for Altyn fault tectonic activities in western China[J]. Chinese Science Bulletin, 1995. 48(18):2024-2030.

    Google Scholar

    LIU Y J, NEUBAUER F, GENSER J, et al. Geochronology of the initiation and displacement of the Altyn Strike-Slip Fault, western China[J]. Journal of Asian Earth Sciences,2007.29(2-3):243-252.

    Google Scholar

    LOISELLE M C, WONES D S. Characteirstics and origin of anorogenie granites[J]. Geoloigcal Society of AmeircanAbstrats with Programs,1979,11:468.

    Google Scholar

    LUDWIG K R. Mathematical-statistical treatment of data and errors for230Th/U geochronology[J]. Reviews in Mineralogy and Geochemistry, 2003, 52(1):631-656.

    Google Scholar

    MILLER C F, MC DOWELL 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.

    Google Scholar

    PATINO DOUNCE A E. What do experiments tell us about the relative contribution of crust and mantle to the origins of granitic magma. Castro A, Femandez C and Vigneresse JL. Understanding Granites:Intergrating New and Clsssical Techniques[J]. Geological Society of London, Special Publication,1999,168:55-75.

    Google Scholar

    PITCHER W S. Granite type and tectonic environment. In:Mountain building processes[M].London:Academic Press, 1983, 19-40.

    Google Scholar

    PITCHER W S. The nature and origin of granite. In:Pitcher WS(ed.). Granite type and tectonic environment. mountain building processes[M]. London:Academic Press,1993,19-40.

    Google Scholar

    MILLER C, SCHUSTER R, KLOTZLI U, et al. Post-collisional potassic and ultrapotassic magmatism in SW Tibet:Geochemical and Sr-Nd-Pb-O isotopic constraints for mantle source characteristics and petrogenesis[J]. Journal of Petrology, 1999,40(9):1399-1424.

    Google Scholar

    SOBEL ER, ARNAUD N. A possible middle Paleozoic suture in the AltunTagh, NW China[J]. Tectonics, 1999. 18(1):64-74.

    Google Scholar

    YIN A, GEHRELS G, CHEN X H. Evidence for 280km of Cenozoic left slip motion along the eastern segment of the AltynTagh fault system, western China[J]. Eos Trans. AGU, 1999, 80(17), FallMeet. Suppl. F1018.

    Google Scholar

    TAPPONIER P, MOLNAR P. Active faulting and Cenozoic tectonics of China[J]. Geophys Res.1977, 82:20-24.

    Google Scholar

    TAYLOR S R, MCLENNAN S M. Thecontinental curst, its composition and evolution[M]. Oxford:Blackwell, 1985:312.

    Google Scholar

    VAN A E, RYAN C G, JACKSON S E, et al. Data reduction software for LA-ICP-MS in the EarthSciences[J]. Mineralogical Association of Canada, 2001, 29:239-243.

    Google Scholar

    WAN Y S. Ba anomaly and its geochemical significance[J]. Continental Dynamics, 1999,4(1):84-87.

    Google Scholar

    WILSON M. Igneous petrogenesis[M]. London:Unwin Hyman Press, 1989:295-323.

    Google Scholar

    • Relative Articles
  • Cited by
  • Supplements
    • Proportional views
  • 加载中
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

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索
Export Citation
PDF
XML

Article Metrics

Article views(854) PDF downloads(249) Cited by(0)

Access History

Other Articles By Authors

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    版权所有：中国地质调查局发展研究中心 copyright @2020