西秦岭埃达克岩的SHRIMP定年及其构造意义

金维浚 张旗 何登发 贾秀勤. 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.
引用本文: 金维浚 张旗 何登发 贾秀勤. 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.
JIN WeiJun,ZHANG Qi,HE DengFa and JIA XiuQin Institute of Geology and Geophysics,Chinese Academy Sciences,Beijing 100029,China Chinese Petroleum Exploration and Development Academy,Beijing 100083,China Institute of High Energy Physics,Chinese Academy Sciences,Beijing 100039,China. SHRIMP dating of adakites in western Qinling and their implications[J]. Acta Petrologica Sinica, 2005, 21(3): 959-966.
Citation: JIN WeiJun,ZHANG Qi,HE DengFa and JIA XiuQin Institute of Geology and Geophysics,Chinese Academy Sciences,Beijing 100029,China Chinese Petroleum Exploration and Development Academy,Beijing 100083,China Institute of High Energy Physics,Chinese Academy Sciences,Beijing 100039,China. SHRIMP dating of adakites in western Qinling and their implications[J]. Acta Petrologica Sinica, 2005, 21(3): 959-966.

西秦岭埃达克岩的SHRIMP定年及其构造意义

  • 基金项目:

    中国科学院知识创新工程基金“青藏高原东北缘晚新生代大陆增生与中新生代陆内变形研究”(KZCX2-SW-119)、教育部回国留学人员启动基金、中国石化南方勘探分公司和中国科学院核分析技术重点实验室(K-116)资助的项目.

  • 西秦岭从夏河-礼县一带发育许多具有埃达克岩地球化学特征的花岗岩,本文对其中的冶力关和夏河岩体进行了 SHRIMP测年,为245±6 Ma和238±4 Ma,属印支早期。西秦岭埃达克岩富K,属于高钾钙碱性系列,地质与地球化学资料表明,西秦岭埃达克岩可能形成于板块消减的活动陆缘环境,与活动陆缘加厚的下地壳熔融作用有关,说明古特提斯洋盆北部的消减作用发生在印支早期。
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  • [1]

    Atherton M P and Petford N. 1993. Generation of sodium-rich magmas from newly underplated basaltic crust. Geology, 4:596 -600

    [2]

    Chen Liang, Sun Yong, Pei, Xianzhi, Gao Min, Hong Tao, Zhang Zhengqin, Chen Wen. 2001. Northernmost paleo-tethyan oceanic basin in tibet: geochronological evidence from Ar39/Ar40 age dating of durngoi ophiolite. Chinese Science Bulletin, 46:424 -426

    [3]

    Davis G A. 2003. The Yanshan belt of North China: tectonics, adakitic magmatism, and crustal evolution. Earth Science Frontiers, 10:373-384

    [4]

    Defant M J. 2002. Reply for comment by R. Conner on the "Evidence suggests slab melting in arc magmas" by M. Defant and P.Kepezhinskas (EOS, 2001, 82: 65, 68 -69). EOS, 66: 256-257.

    [5]

    Defant M J. Drummond M S. 1990. Derivation of some modern arc magmas by melting of young subduction lithosphere . Nature, 347:662 - 665.

    [6]

    Feeley T C, Davidson J P. 1995. Petrology of ca lc-alkaline lavas at Volcan Ollague and the origin of compositional diversity at Central Andean Stratovolcanoes. Journal Petrology, 35: 1295 - 1340.

    [7]

    Feng Y M, Cao X D, Zhang E P, Hu Y X, Pan X P, YangJ L, Jia Q Z,Li W M. 2003. Tectonic evolution framework and nature of the west Qinling orogenic belt. Northwestern Geology, 36:1 -10

    [8]

    Jian P, Liu D Y, Sun X M. 2004. SHRIMP Dating or Jicha Alaskan-type Gabbro in West Yunnan Province evidence of the Early Permian Subduction. Acta Geogica Sinica, 78: 166- 170( in Chinese with English abstract)

    [9]

    Jian P, Liu D, Sun X. 2003. SHRIMP dating of Carbonerous Jinshajiag ophiolite, China: Geochronological constraints for the evo1ution of Paleo-Tethys oceanic floor. Acta Geologica Sinica, 77 (2): 217 -228 (in Chinese with English abstract)

    [10]

    Jian P, Wang X F, He L Q, Wang C S. 1998. U-Pb zircon dating of the Shuanggou Ophiolite from Xingping County, Yunnan Province. Acta Petrologica Sinica, 14: 207 - 211

    [11]

    Jian P, Wang X F, He L Q, Wang C S. 1999. U-Pb zircon dating of anothosite and plagiogranite from the Jinshajiang ophiolite belt. Acta Petrologica Sinica, 15: 590 -593

    [12]

    Kay R W, Kay S M. 2002. Andean adakites: three ways to make them.Acta Petrologica Sinica, 18: 303 - 311

    [13]

    Kay S M, Mpodozis C. 2001. Central Andean ore deposits linker to evolving shallow subduction systems and thinkening crust. GSA Today, 4-9.

    [14]

    Li W P, Li X H, Lu F X. 2001. Genesis and geological significance for the middle Jurassic high Sr and lower Y type volcanic rocks in Fuxin area of West Liaoning, northeastern China. Acta Petrologica Sinica,17:523 -532( in Chinese with English abstract)

    [15]

    Liu HT, Zhang Q, Liu JM, Ye J, Zeng QD and Yu CM. 2004. Adakite versus porphyry copper and epithermal gold deposits: a possible metallogenetic specialization of magmatism required in-deep assessment. Acta Petrologica Sinica, 20(2) :205 -218(in Chinese with English abstract)

    [16]

    Pan G Q, Lu X C, Yu H E. 2001. Petrological and geochemical characteristics of Mesozoic adakite from Northern Huaiyuan and discussion on its genesis. Acta Petrologica Sinica, 17: 541 -550( in Chinese with English abstract)

    [17]

    Peacock S M, Rushmer T, Thompson A B. 1994. Partial melting of subducting oceanic crust. Earth P1anetary Science Letters, 121:227 - 244

    [18]

    Rapp R P, Xiao L, Shimizu N. 2002. Experimental Constraint on the origin of potassium-rich Adakites in eastern China. Acta Petrologica Sinica, 18: 293 -302

    [19]

    Roger F, Malavieille J, Leloup PH, Calassou S, Xu Z. 2004. Timing of granite emplacement and cooling in the Songpan-Garze Fold Belt (eastern Tibetan Plateau) with tectonic implications, Journal of Asian Earth Sciences 22: 465 481

    [20]

    Wang Q, Xu J F, Zhao Z H, Wang Renjing, Qiu Jiaxiang, Bao Zhiwei.2001. The petrogenesis and geodynamic significances of heavy rare earth element(HREE)-depleted granitoids during Yanshan period in the Dabie Mountains. Acta Petrologica Sinica, 17:551 - 564 ( in Chinese)

    [21]

    Wang Y L Zhang Qi, Wang Y. 2001. Geochemical characteristics and geodynamic significance of volcanic rocks in Ninwu area, Jiangsu Provlnc e, eastem China. Acta petrologica Sinica, 17:565 -575 (in Chinese with English abstract)

    [22]

    WangY L, Wang Y, Zhang Q, Jia X Q and Han S. 2004. The geochemical characteristic of Mesozoic intermediate acid intrusive of the Tongling area and the metallogenes-geodynamical implication.Acta Petrologica Sinica, 20(2): 325 -338 (in Chinese with English abstract)

    [23]

    Wang Y, Zhang Q. 2001. Badaling granite complexes in Beijing area:Their composition, geochemical characteristics and geological significance. Acta Petrologica Sinica, 17:533 - 540 ( in Chinese with English abstract)

    [24]

    Xiao L, Rapp PR and Xu JF. 2004. The role of deep processes controls on variation of compositions of adakitic rocks. Acta Petrologica Sinica, 20(2) :219 -228

    [25]

    Xu J F, Wang Q, Xu Y G. 2001. Geochemistry of Anjishan intermediateacid intrusive rocks in Ningzhen area: constraint to generation of adakite-like magma. Acta Petrolica Sinica, 17:576 - 584 ( in Chinese)

    [26]

    Xu J F, Wang Q. 2003. Tracing the thinkening process of continental crust through studying adakitic rocks: evidence from volcanic rocks in the north Tibet. Earth Science Frontiers, 10:401 -406.

    [27]

    Yogodzinski G M, Volynets O N, Koloskov A V, Seliverstov N I, and Matvenkov V V. 1994. Magnesian andesites and the subduction component in a strongly calc-alkaline series at Piip Volcano, far western Aleutians. J. Petrol., 35:163-204

    [28]

    Yogodzinski GM, Kay RW Bolynets ON, 1995. Magnesian andsite in the western Aleutian Komandorsy region : Implications for slab melting and processes in the mantle wedge. Geological Soc. Am. Bull. ,107,505 -519.

    [29]

    Zhang G W, Guo A L, Yao A P. 2004. Western Qinling-Songpan Continental Tectonic Node In China Continental Tectonics, Earth Science Frontier, 11: 23 - 31 ( in Chinese with English abstract)

    [30]

    Zhang G W, Zhang B R, Yuan X C. 2001. Qinling Orogen and Geodynamics, Science Press

    [31]

    Zhang Guowei, Dong Yunpeng, Lai Shaocong, Guo An Lin, Meng Qingren, Liu Shaofeng, Chen Shengyu, Yao An Ping, Zhang Zhengqin, Pei Xianzhi, Li Sanzhong. 2003. Mianlue tectonic zone and Mianlue suture zone on southern margin of Qinling Dabie orogenic belt. Chinese Science (D) , 33: 1122 - 1135

    [32]

    Zhang HF, Zhai MG, He ZF, Peng P and Xu BL. 2004. Petrogenesis and implications of the sodium-rich granites from the Kunyushan complex, eastern Shandong province. Acta Petrologica Sinica, 20(3) :369 -380

    [33]

    Zhang Q, Wang Y, Qian Q. 2001. The characteristics and tectonics metallogenic significances of the Mesozoic adakites in eastern China.Acta Petrologica Sinica, 17: 236 - 244 ( in Chinese with English abstract )

    [34]

    ZhangQ, ZhouDJ, ZhaoD S, PengXJ, LuoW L, Liu X P. 1996. Wilson cycle of the Paleo-Tethyan orogenic belt in western Yunnan:Record of magmatism and discussion on mantle process. Acta Petrologica Sinica, 12:17 -28 (in Chinese with English abstract)

    [35]

    Zhang Qi, Qin K Z, WangY L, Zhang F Q, Liu HT, Wang Y. 2004. Study on adakite broadened to challenge the Cu and Au exploration in China. Acta Petrologica Sinica, 20: 195 - 204 ( in Chinese with English abstract)

    [36]

    Zhang Qi, Wang Yan, Liu Hongtao, Wang Yuanlong, Li Zhitong. 2003. On the space-time distribution and geodynamical environment of adakites in China. Earth Science Frontier, 10:385 - 400 ( in Chinese with English abstract)

    [37]

    陈亮,孙勇,裴先治,高明,冯涛,张宗清,陈文.2001.德尔尼蛇绿岩40Ar-39Ar年龄:青藏最北端古特提斯洋盆存在和延展的证据.科学通报,46(5):424-426

    [38]

    冯益民,曹宣铎,张二朋,胡云绪,潘晓萍,杨军录,贾群子,李文明.2003.西秦岭造山带的演化、构造格局和性质.西北地质,36:1-10

    [39]

    简平,刘敦一,孙晓猛.2003.滇川西部金沙江石碳纪蛇绿岩SHRIMP测年:古特提斯洋盆演化的同位素年代学制约.地质学报,77(2):217~228.

    [40]

    简平,刘敦一,孙晓猛.2004.滇西吉岔阿拉斯加型辉长岩SHRIMP测年:早二叠世俯冲事件的证据.地质学报,78(2):166-170.

    [41]

    简平,汪啸风,何龙清,王传尚.1998.云南新平县双沟蛇绿岩U-Pb年代学初步研究.岩石学报,4:207-211

    [42]

    简平,汪啸风,何龙清,王传尚.1999.金沙江蛇绿岩中斜长岩和斜长花岗岩的U-Pb年龄及地质意义.岩石学报,15:590-593

    [43]

    李伍平,李献华,路风香.2001.辽西中侏罗世高Sr低Y型火山岩的成因及其地质意义.岩石学报,17:523-532

    [44]

    刘红涛,张旗,刘建明,叶杰,曾庆栋,于昌明.2004.埃达克岩与CuAu成矿作用:有待深入研究的岩浆成矿关系.岩石学报,20(2):205-218

    [45]

    潘国强,陆现彩,干航波.2001.北淮阳中生代adakite岩石地球化学特征及成因讨论.岩石学报,17:541-550

    [46]

    孙卫东,李曙光,Yadong Chen,李育敬.2000.南秦岭花岗岩锆石U-Pb定年及其地质意义.地球化学,29(3),209-216

    [47]

    王强,许继锋,赵振华,王人镜,邱家骧,包志伟.2001.大别山燕山期亏损重稀土元素花岗岩类的成因及动力学意义.岩石学报,17:551-564

    [48]

    王焰,张旗.2001.八达岭花岗杂岩的组成、地球化学特征及其意义.岩石学报,17:533-540

    [49]

    王元龙,王焰,张旗,贾秀琴,韩松.2004.铜陵地区中生代中酸性侵入岩的地球化学特征及其成矿地球动力学意义.岩石学报,20(2),325-338

    [50]

    王元龙,张旗,王焰.2001.宁芜火山岩的地球化学特征及其意义.岩石学报,17:565-575

    [51]

    肖龙,Rapp R P,许继峰.2004.深部过程对埃达克质岩石成分的制约,岩石学报,20(2):219-228

    [52]

    许继峰,王强,徐义刚,赵振华,熊小林.2001.宁镇地区中生代安基山中酸性侵入岩的地球化学:亏损重稀土和钇的岩浆产生的限制.岩石学报,17:576-584

    [53]

    许继峰,王强.2003. Adakitie火成岩对大陆地壳增厚过程的指示:以青藏北部火山岩为例.地学前缘,10:401-406.

    [54]

    张国伟,董云鹏,赖绍聪,郭安林,孟庆任,刘少峰,程顺有,姚安平,张宗清,裴先治,李三忠.2003.秦岭-大别造山带南缘勉略构造带与勉略蛇绿岩.中国科学(D辑),33:1122-1135

    [55]

    张国伟,张本仁,袁学诚.2001.秦岭造山带和大陆动力学.北京:科学出版社

    [56]

    张国伟,郭安林,姚安平.2004.中国大陆构造中的西秦岭-松潘大陆构造结,地学前缘,11(3),23-31

    [57]

    张华锋,翟明国,何中甫,彭澎,许保良.2004.胶东昆嵛山杂岩中高锶花岗岩地球化学成因及其意义.20(3):369-380

    [58]

    张旗,秦克章,王元龙,张福勤,刘红涛,王焰.2004.加强埃达克岩研究,开创中国Cu、Au等找矿工作的新局面.岩石学报,20(2),195-204

    [59]

    张旗,王焰,刘红涛,王元龙,李之彤.2003.中国埃达克岩的时空分布及其形成背景附:《国内关于埃达克岩的争论》.地学前缘,10(4):385-400

    [60]

    张旗,王焰,钱青,杨进辉,王元龙,赵太平,郭光军.2001.中国东部燕山期埃达克岩的特征及其构造:成矿意义.岩石学报,17(2),236-244

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出版历程
收稿日期:  2005-01-27
修回日期:  2005-01-27
刊出日期:  2005-05-31

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