留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名
邮箱
手机号码
标题
留言内容
验证码

中亚造山带西准噶尔晚古生代洋陆转换与构造演化——来自晚石炭世流纹岩的证据

史建杰 陈宣华 丁伟翠 李冰

史建杰, 陈宣华, 丁伟翠, 等, 2017. 中亚造山带西准噶尔晚古生代洋陆转换与构造演化——来自晚石炭世流纹岩的证据. 地质力学学报, 23 (1): 150-160.
引用本文: 史建杰, 陈宣华, 丁伟翠, 等, 2017. 中亚造山带西准噶尔晚古生代洋陆转换与构造演化——来自晚石炭世流纹岩的证据. 地质力学学报, 23 (1): 150-160.
SHI Jian-jie, CHEN Xuan-hua, DING Wei-cui, et al., 2017. LATE PALEOZOIC OCEAN-CONTINENT TRANSITION IN WEST JUNGGAR, CENTRAL ASIAN OROGENIC BELT:EVIDENCE FROM LATE CARBONIFEROUS RHYOLITES. Journal of Geomechanics, 23 (1): 150-160.
Citation: SHI Jian-jie, CHEN Xuan-hua, DING Wei-cui, et al., 2017. LATE PALEOZOIC OCEAN-CONTINENT TRANSITION IN WEST JUNGGAR, CENTRAL ASIAN OROGENIC BELT:EVIDENCE FROM LATE CARBONIFEROUS RHYOLITES. Journal of Geomechanics, 23 (1): 150-160.

中亚造山带西准噶尔晚古生代洋陆转换与构造演化——来自晚石炭世流纹岩的证据

基金项目: 

国家科技支撑计划重点项目暨国家305项目 2007BAB25B02

中国地质调查局地质调查项目 DD20160083

国家深部探测技术与实验研究专项 SinoProbe-08

祁连-天山盆山结合带深部地质调查 DD20160083

详细信息
    作者简介:

    史建杰(1992-), 男, 硕士研究生, 构造地质学专业。E-mail:1311618693@qq.com

    通讯作者:

    陈宣华(1967-), 男, 博士, 研究员, 从事构造地质学和矿床资源研究。E-mail:xhchen@cags.ac.cn

  • 中图分类号: P588.141;P59

LATE PALEOZOIC OCEAN-CONTINENT TRANSITION IN WEST JUNGGAR, CENTRAL ASIAN OROGENIC BELT:EVIDENCE FROM LATE CARBONIFEROUS RHYOLITES

  • 摘要: 本文在中亚造山带西部的西准噶尔地区新发现晚石炭世柱状节理流纹岩,并根据其地球化学特征探讨了其形成的构造环境。岩石化学分析的结果表明,柱状节理流纹岩的主量元素具有高钾低钠的特征,属于高钾钙碱性和钙碱性岩浆系列;球粒陨石标准化稀土元素分配模式表现为Ⅴ字型,Eu亏损,说明发生了斜长石的结晶分异。大离子亲石元素(LILE)Rb、K相对富集,高场强元素(HFSE)Nb、Ta出现负异常,反映了俯冲带岩浆的特征。研究表明该流纹岩属于A2型,形成于后造山的伸展构造环境;与该地区晚石炭世大型花岗岩类岩基具有同源性,同属于后造山伸展环境下的富碱岩浆作用。对比我国东部沿海中生代柱状节理流纹岩的大陆边缘构造环境,本研究认为西准噶尔地区在晚石炭世存在由大洋俯冲向陆内环境转变的洋陆转换特征;之前的大洋俯冲主要发育在克拉玛依-包古图-带,具有准噶尔洋板块向西北方向在哈萨克斯坦微陆块之下俯冲的构造极性。正是由晚石炭世柱状节理流纹岩所代表的后造山伸展环境下的富碱岩浆作用,终结了该地区洋陆过渡带环境。

     

  • 图  1  西准噶尔地区构造体系遥感解译及流纹岩采样点位置

    图中:P二叠世,C1t石炭系太勒古拉组,C1b石炭系包古图组,C1xb石炭系希贝库拉斯组,D泥盆世;HT哈图岩体,ME庙儿沟岩体,TE塔尔根岩体,AK阿克巴斯陶岩体,K956岩体,KL克拉玛依岩体

    Figure  1.  Fault tectonic system in the West Junggar and the location of the rhyolites from the remote sensing interpretation map

    图  2  柱状节理流纹岩特征

    (a)柱状流纹岩整体产出照片; (b)柱状流纹岩横切面手标本(c)、(d)镜下照片; Qtz-石英, Kfs-钾长石

    Figure  2.  Photography and microstructure of the rhyolites samples with columnar joints

    图  3  柱状节理流纹岩产出简图【位置见图 1黑色框内】

    Figure  3.  The occurrence of the Rhyolites with columnar joints

    图  4  西准噶尔地区流纹岩岩性判别图

    (a)火成岩岩岩类TAS分类图解(原图据文献[19]) (b)K2O-SiO2分类图(庙儿沟花岗岩数据据文献[20],原图据文献[21, 22])Pc—苦橄玄武岩;B—玄武岩;O1—玄武安山岩;O2—安山岩;O3—英安岩;R—流纹岩;S1—粗面玄武岩;S2—玄武质粗面安山岩;S3—粗面安山岩;T—粗面岩、粗面英安岩;F—副长石岩;U1—碱玄岩、碧玄岩;U2—响岩质碱玄岩;U3—碱玄质响岩;Ph—响岩;Ir—Irvine分界线(上方为碱性,下方为亚碱性)

    Figure  4.  Classification diagrams of rhyolites from the West Junggar area

    图  5  哈克图解

    Figure  5.  Harker diagrams (major elements vs. SiO2 content (wt.%))

    图  6  柱状节理流纹岩稀土元素球粒陨石标准化配分模式图(a)和微量元素原始地幔标准化多元素蛛网图(b)

    (原图据文献[24~25];灰色部分庙儿沟花岗岩数据据文献[22])

    Figure  6.  Chondrite-normalized REE distribution patterns(a) and primitive mantle-normalized multi-elements spider diagram(b)

    图  7  西准噶尔地区A型流纹岩判别图(底图据文献[26~29])

    Figure  7.  Classification diagrams of A-type rhyolite from the West Junggar area

    图  9  西准噶尔地区晚石炭世大地构造环境模式图

    Figure  9.  A schematic showing the development of the late Carboniferous tectonic environment in the West Junggar

    图  8  西准噶尔成矿带花岗岩类微量元素构造环境判别图解(底图据文献[28])

    a—Nb-Y;b—Ta-Yb;c—Rb-(Y+Nb);d—Rb-(Yb+Ta);syn-COLG—同碰撞花岗岩;VAG—火山岛弧花岗岩;WPG—板内花岗岩;ORG—洋脊花岗岩;post-COLG—后碰撞花岗岩

    Figure  8.  Trace element tectonic setting discrimination diagrams of granitoids from the West Junggar Metallogenic Belt

    表  1  西准噶尔地区流纹岩样品主量元素(wt%)分析结果

    Table  1.   Major elements(wt%) of rhyolites from the West Junggar

    样品号SiO2Al2O3CaOFe2O3FeOK2OMgOMnONa2OP2O5TiO2CO2H2O+LOITOTAL
    SJ150731-6-179.2013.190.190.580.334.630.180.041.510.040.090.331.621.62101.26
    SJ150731-6-276.8812.730.990.810.484.720.100.013.140.030.110.50.781.37100.74
    SJ150803-1-377.5112.530.580.900.554.560.110.013.110.030.090.50.841.26100.57
    SJ150803-1-476.4512.901.231.230.264.630.090.013.050.040.101.130.961.74101.18
    SJ150803-2-175.7812.570.152.890.182.920.060.055.130.020.240.50.580.5999.92
    SJ150803-3-177.9912.210.191.470.252.090.060.025.470.030.200.330.440.49100.26
    下载: 导出CSV

    表  2  西准噶尔地区流纹岩样品微量元素分析结果

    Table  2.   Trace elements (10-6) of rhyolites from the West Junggar

    微量元素样品中微量元素含量/10-6
    SJ150731-6-1SJ150731-6-2SJ150803-1-3SJ150803-1-4SJ150803-2-1SJ150803-3-1
    La25.1021.0024.2024.4032.6027.90
    Ce61.5051.9058.9059.3058.5060.30
    Pr8.636.717.978.099.788.31
    Nd35.4028.8032.9033.0041.4037.00
    Sm9.396.988.198.289.708.30
    Eu0.170.170.160.181.721.11
    Gd10.006.838.248.449.278.26
    Tb1.801.231.481.541.481.37
    Dy12.208.109.669.989.249.02
    Ho2.651.682.072.081.911.87
    Er7.324.835.706.225.335.40
    Tm1.070.700.830.890.800.80
    Yb6.644.544.955.475.315.11
    Lu0.990.670.720.810.810.74
    Y69.2043.7051.6055.9049.4046.30
    Ba257.00207.00201.00196.00871.00542.00
    Rb138.00106.00103.00106.0063.9053.30
    Th12.109.5511.3011.206.417.66
    Lu0.990.670.720.810.810.74
    Nb6.236.276.306.478.959.26
    Ta0.630.640.590.570.650.64
    Sr24.3032.5033.2046.7033.9042.70
    Zr100.0091.3094.2099.20344.00355.00
    Hf4.414.124.154.3011.1011.60
    U3.082.152.412.272.502.48
    下载: 导出CSV
  • [1] 杨高学, 李永军, 刘振伟, 等.西准噶尔玛依拉山组志留纪玄武岩的地球化学特征及构造意义[J].大地构造与成矿学, 2012, 36(1):127~136. http://www.cnki.com.cn/Article/CJFDTOTAL-DGYK201201020.htm

    YANG Gao-xue, LI Yong-jun, LIU Zhen-wei, et al. Geochemistry of the Basalts from the Silurian Maylashan Formation in the West Junggar and its Tectonic Implications[J]. Geotectonica et Metallogenia, 2012, 36(1):127~136. http://www.cnki.com.cn/Article/CJFDTOTAL-DGYK201201020.htm
    [2] 苏玉平, 唐红峰, 侯广顺, 等.新疆西准噶尔达拉布特构造带铝质A型花岗岩的地球化学研究[J].地球化学, 2006, 35(1):55~67. http://www.cnki.com.cn/Article/CJFDTOTAL-DQHX200601006.htm

    SU Yu-ping, TANG Hong-feng, HOU Guang-shun, et al. Geochemistry of aluminous A-type granites along Darabut tectonic belt in West Junggar, Xinjiang[J]. Geochimica, 2006, 35(1):55~67. http://www.cnki.com.cn/Article/CJFDTOTAL-DQHX200601006.htm
    [3] Chen, B., Arakawa, Y.. Elemental and Nd-Sr isotopic geochemistry of granitoids from the West Junggar foldbelt (NW China), with implications for Phanerozoic continental growth[J]. Geochimica et Cosmochimica Acta, 2005, 69(22):1307~1320. http://www.academia.edu/10823263/Late_Paleozoic_volcanic_record_of_the_Eastern_Junggar_terrane_Xinjiang_Northwestern_China_Major_and_trace_element_characteristics_Sr_Nd_isotopic_systematics_and_implications_for_tectonic_evolution
    [4] 高睿, 肖龙, 王国灿, 等.西准噶尔晚古生代岩浆活动和构造背景[J].岩石学报, 2013, 29(10):3413~3434. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201310008.htm

    GAO Rui, XIAO Long, WANG Guo-can, et al. Paleozoic magmatism and tectonic setting in West Junggar[J]. Acta Petrologica Sinica, 2013, 29(10):3413~3434. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201310008.htm
    [5] 尹继元, 袁超, 孙敏, 等.新疆哈图早二叠世富镁闪长岩的时代、地球化学特征和可能的成因机制[J].岩石学报, 2012, 28(7):2171~2181. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201207019.htm

    YIN Ji-yuan, YUAN Chao, SUN Min, et al. Age, geochemical features and possible petrogenesis mechanism of Early Permian magnesian diorite in Hatu, Xinjiang[J]. Acta Petrologica Sinica, 2012, 28(7):2171~2182. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201207019.htm
    [6] 涂光炽.初议中亚成矿域[J].地质科学, 1999, 34(4):397~404. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKX199904000.htm

    TU Guang-zhi. On the central Asia metallogenic province[J]. Science Geologica Sinica, 1999, 34(4):397~404. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKX199904000.htm
    [7] 何国琦, 朱永峰.中国新疆及其邻区地质矿产对比研究[J].中国地质, 2006, 33(3):451~460. http://www.cnki.com.cn/Article/CJFDTOTAL-DIZI200603000.htm

    HE Guo-qi, ZHU Yong-feng. Comparativestudy of the geology and mineral resources in Xinjiang, China, and its adjacent regions[J]. Geology in China, 2006, 33(3):451~460. http://www.cnki.com.cn/Article/CJFDTOTAL-DIZI200603000.htm
    [8] 朱永峰, 何国琦, 安芳.中亚成矿域核心地区地质演化与成矿规律[J].地质通报, 2007, 26(9):1167~1177. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD200709019.htm

    ZHU Yong-feng, HE Guo-qi, AN Fang. Geological evolution and metallogeny in the core part of the central Asia metallogenic domain[J]. Geological Bulletin of China, 2007, 26(9):1167~1177. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD200709019.htm
    [9] 肖文交, 舒良树, 高俊, 等.中亚造山带大陆动力学过程与成矿作用[J].新疆地质, 2008, 26(1):4~8. http://www.cnki.com.cn/Article/CJFDTOTAL-ZGJB200903011.htm

    XIAO Wen-jiao, SHU Liang-shu, GAO Jun, et al. Continental dynamics of the central Asian orogenic belt and its metallogeny[J]. Xinjiang Geology, 2008, 26(1):4~8. http://www.cnki.com.cn/Article/CJFDTOTAL-ZGJB200903011.htm
    [10] 陈宣华, 陈正乐, 杨农.区域成矿与矿田构造研究——构建成矿构造体系[J].地质力学学报, 2009, 15(1):1~19. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?file_no=20090101&flag=1

    CHEN Xuan-hua, CHEN Zheng-le, YANG Nong. Study on regional mineralization and ore-field structure:Bring on the building of mineralizing tectonic systems[J]. Journal of Geomechanics, 2009, 15(1):1~19. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?file_no=20090101&flag=1
    [11] 陈宣华, 屈文俊, 韩淑琴, 等.巴尔喀什成矿带Cu-Mo-W矿床的辉钼矿Re-Os同位素年龄测定及其地质意义[J].地质学报, 2010, 84(9):1333~1348. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201009008.htm

    CHEN Xuan-hua, QU Wen-jun, HAN Shu-qin, et al. Re-Os dating of molybdenites from Cu-Mo-W deposits in Balkhash metallogenic belt, Kazakhstan and its geological significance[J]. Acta Geologica Sinica, 2010, 84(9):1333~1348. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201009008.htm
    [12] 陈宣华, 杨农, 叶宝莹, 等.中亚成矿域多核成矿系统西准噶尔成矿带构造体系特征及其对成矿作用的控制[J].大地构造与成矿学, 2011, 35(3):325~338. http://www.cnki.com.cn/Article/CJFDTOTAL-DGYK201103001.htm

    CHEN Xuan-hua, YANG Nong, YE Bao-ying, et al.Western Junggar Tectonic System and Its Control on Metallogenesis in Multi-Core Metallogenic System, Central Asia[J]. Geotectonic et Metallogenia, 2011, 35(3):325~338. http://www.cnki.com.cn/Article/CJFDTOTAL-DGYK201103001.htm
    [13] Xiao, W. J., Windley, B. F., Sun, S., et al. A tale of amalgamation of three Permo-Triassic collage systems in Central Asia:Oroclines, sutures, and terminal accretion[J]. Annu. Rev. Earth Planet. Sci, 2015, 43:477~507. doi: 10.1146/annurev-earth-060614-105254
    [14] Heinhorst, J., Lehmann, B., Ermolov, P., et al. Paleozoic crustal growth and metallogeny of Central Asia:Evidence from magmatic-hydrothermal ore systems of Central Kazakhstan[J]. Tectonophysics, 2000, 328(1/2):69~87. doi: 10.1007/s00126-006-0070-x
    [15] 陈宣华, 聂兰仕, 丁伟翠, 等.西准噶尔走滑断裂系元素分布特征及其成矿意义[J].岩石学报, 2015, (2):371~387. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201502006.htm
    [16] 陈宣华, 陈正乐, 白彦飞, 等.中亚成矿域西部巴尔喀什-准噶尔成矿带晚古生代成矿作用大爆发[J].地球科学与环境学报, 2016, 38(3):285~305. http://www.cnki.com.cn/Article/CJFDTOTAL-XAGX201603001.htm

    CHEN Xuan-hua, CHEN Zheng-le, BAI Yan-fei, et al. Late Paleozoic concentrated mineralization of Balkhash-Junggar metallogenic belt in the western part of the Central Asian Metallogenic Domain[J]. Journal of Earth Science and the Environment, 2016, 38(3):285~305. http://www.cnki.com.cn/Article/CJFDTOTAL-XAGX201603001.htm
    [17] YANG Gao-xue, LI Yong-jun, Santosh, M., et al. Geochronology and geochemistry of basaltic rocks from the Sartuohai ophioliticmélange, NW China:Implications for a Devonian mantle plume within the Junggar Ocean[J]. Journal of Asian Earth Sciences, 2012, 59:141~155. doi: 10.1016/j.jseaes.2012.07.020
    [18] 韩宝福, 季建清, 宋彪, 等.新疆准噶尔晚古生代陆壳垂向生长(Ⅰ):后碰撞深成岩浆活动的时限[J].岩石学报, 2006, 22(5):1077~1086. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200605003.htm

    HAN Bao-fu, JI Jian-qing, SONG Biao, et al. Late Paleozoic vertical growth of continental crust around the Junggar Basin, Xinjiang, China (Part Ⅰ):Timing of post-collisional plutonism[J]. Acta Petrologica Sinica, 2006, 22(5):1077~1086 http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200605003.htm
    [19] 李永军, 王祚鹏, 段丰浩, 等.新疆西准噶尔额敏前陆盆地的构造特征及其演化[J].大地构造与成矿学, 2016, 40(3):419~428. http://www.cnki.com.cn/Article/CJFDTOTAL-DGYK201603002.htm

    LI Yong-jun, WANG Zuo-peng, DUAN Feng-hao, et al. Tectonics andevolution of the E'min foreland basin in West Junggar, Xinjiang[J]. Geotectonica et Metallogenia, 2016, 40(3):419~428. http://www.cnki.com.cn/Article/CJFDTOTAL-DGYK201603002.htm
    [20] Le, Bas, M. J., Le, Maitre, R. W., Streckeisen, A., et al. A chemical classification of volcanic rocks on the total alkali-silica diagram[J]. Petrol. 1986, 27(3):745~750. doi: 10.1093/petrology/27.3.745
    [21] 黄鹏辉, 陈宣华, 王志宏, 等.西准噶尔成矿带晚古生代花岗岩类岩浆活动及其构造意义[J].大地构造与成矿学, 2016, 40(1):145~160. http://www.cnki.com.cn/Article/CJFDTOTAL-DGYK201601013.htm

    HUANG Peng-hui, CHEN Xuan-hua, WANG Zhi-hong, et al. Late Paleozoicgranitic magmatism in West Junggar metallogenic belt (Xinjiang), Central Asia, and its tectonic implication[J]. Geotectonica et Metallogenia, 2016, 40(1):145~160. http://www.cnki.com.cn/Article/CJFDTOTAL-DGYK201601013.htm
    [22] Peccerillo, R., Taylor, S. R.. Geochemistry of Eocene calc-alkaline volcanic rocks from the Kastamonu area, northern Turkey[J]. Contributions to Mineralogy and Petrology, 1976, 58(1):63~81. doi: 10.1007/BF00384745
    [23] Middlemost, E. A. K.. Magmas and magmatic rocks[M]. London:Longman, 1985:1~266.
    [24] Wilson, M.. Igneous petrogenesis:A global tectonic approach[M]. London:Unwin Hyman, 1989:1~466.
    [25] Boynton, W. V.. Cosmochemistry of the rare earth elements:Meteorite studies[J]. Developement in Geochemistry, 1984, 2:63~114. doi: 10.1016/B978-0-444-42148-7.50008-3
    [26] Sun, S. S., McDonough, W. F.. Chemical and isotopic systematics of oceanic basalts:Implications for mantle composition andprocesses[C]//Saunders A D, Norry M J. Magmatism in the ocean basins. Oxford:Blackwell, 1989:313~346.
    [27] Whalen, J. B., Currie, K. L., Chappell, et al. A-type granites:Geochemical characteristics, discrimination and petrogenesis[J]. Contrib. Mineral. Petrol., 1987, 95:407~419. doi: 10.1007/BF00402202
    [28] Eby, G. N.. Chemical subdivision of the A-type granitoids:Petrogenetic and tectonic implications[J]. Geology, 1992, 20(7):641~644. doi: 10.1130/0091-7613(1992)020<0641:CSOTAT>2.3.CO;2
    [29] Pearce, J. A., Harris, N. B. W., Tindle, A. G..Trace element discrimination diagrams for the tectonic interpretation of granitic rocks[J]. J Petrol, 1984, 25(4):956~983. doi: 10.1093/petrology/25.4.956
    [30] Pearce, J. A..Sources and settings of granitic rocks[J]. Episodes, 1996, 19(4):120~125 http://www.oalib.com/references/17346114
    [31] 徐松年.浙江中生代酸性火山岩柱状节理构造的发现及其地质意义[J].岩石学报, 1995, (03):325~332. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB199503008.htm

    XU Song-nian. Dsicovery of columnar jointstructure of mesozolc acidic volcanic rocks in ZheJiang province and its geological siginificance[J]. Acta Petrologica Sinca, 1995, 31(3):325~332. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB199503008.htm
    [32] 胡小猛, 许红根, 陈美君, 等.雁荡山流纹岩地貌景观特征及其形成发育规律[J].地理学报, 2008, (3):270~279. doi: 10.11821/xb200803005

    HU Xiao-meng, XU Honggen, CHEN Mei-jun, et al. The rhyolite landforms and development law in Yandang Mt[J]. Acta Geographica Sinica. 2008, (3):270~279. doi: 10.11821/xb200803005
    [33] 邢广福, 陶奎元, 杨祝良, 等.中国东南沿海中生代火山岩成因研究现状与展望[J].矿物岩石地球化学通报, 1999, 18(3):189~193. http://www.cnki.com.cn/Article/CJFDTOTAL-KYDH903.010.htm

    XING Guang-fu, TAO Kui-yuan, YANG Zhu-liang, et al., The summarizing about the reasons causing the formation of Mesozoic igneous rock in southeast China near the reason[J]. The Bulletin of Mineralogy, Petrology and Geochemistry, 1999, 18(3):189~193. http://www.cnki.com.cn/Article/CJFDTOTAL-KYDH903.010.htm
    [34] 赵恒乐, 陈宣华, 屈文俊, 等.巴尔喀什成矿带博尔雷斑岩铜矿床地质特征与成矿时代[J].地质力学学报, 2010, (4):340~348. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?file_no=20100402&flag=1

    ZHAO Heng-le, CHEN Xuan-hua, QU Wen-jun, et al., Geological characteristics and metallogenic age of borly porphyry cu deposits in balkhash metallogenic belt, Kazakhstan[J].Journal of geomechanics, 2010, (4):340~348. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?file_no=20100402&flag=1
    [35] 张耀玲, 张绪教, 胡道功, 等.东昆仑造山带纳赤台群流纹岩SHRIMP锆石U-Pb年龄[J].地质力学学报, 2010, (1):21~27+50. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?file_no=20100103&flag=1

    ZHANG Yao-ling, ZHANG Xu-jiao, HU Dao-gong, et al., Zircon U-Pb age for rhyolitic ruffs of the naocangjiangou formation in the east kulun orogenic belt and their implication[J].Journal of geomechanics, 2010, (1):21~27+50. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?file_no=20100103&flag=1
    [36] 陈宣华, 王小凤, 杨风, 等.阿尔金山北缘早古生代岩浆活动的构造环境[J].地质力学学报, 2001, (3):193~200. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?file_no=20010330&flag=1

    CHEN Xuan-hua, WANG Xiao-feng, YNAG Feng, et al. Tectonic environments of magmatism in earlyPaleozoic in the north altyn tagh, China[J]. Journal of geomechanics, 2001, (3):193~200. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?file_no=20010330&flag=1
  • 加载中
图(9) / 表(2)
计量
  • 文章访问数:  160
  • HTML全文浏览量:  104
  • PDF下载量:  14
  • 被引次数: 0
出版历程
  • 收稿日期:  2016-10-12
  • 刊出日期:  2017-02-28

目录

    /

    返回文章
    返回