• 中国出版政府奖提名奖

    中国百强科技报刊

    湖北出版政府奖

    中国高校百佳科技期刊

    中国最美期刊

    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

    内蒙古狼山地区南北向断裂构造应力场特征及其与区域构造演化关系

    李甜 解国爱 张进 曲军锋 张北航 赵衡 田荣松 艾米尔丁·艾尔肯 李法浩

    李甜, 解国爱, 张进, 曲军锋, 张北航, 赵衡, 田荣松, 艾米尔丁·艾尔肯, 李法浩, 2020. 内蒙古狼山地区南北向断裂构造应力场特征及其与区域构造演化关系. 地球科学, 45(1): 211-225. doi: 10.3799/dqkx.2018.342
    引用本文: 李甜, 解国爱, 张进, 曲军锋, 张北航, 赵衡, 田荣松, 艾米尔丁·艾尔肯, 李法浩, 2020. 内蒙古狼山地区南北向断裂构造应力场特征及其与区域构造演化关系. 地球科学, 45(1): 211-225. doi: 10.3799/dqkx.2018.342
    Li Tian, Xie Guoai, Zhang Jin, Qu Junfeng, Zhang Beihang, Zhao Heng, Tian Rongsong, Aimierding·Aierken, Li Fahao, 2020. Characteristics of the Tectonic Stress Field of the South-North Oriented Fault of the Langshan Mountain Region of Inner Mongolia and Its Relationship with Regional Tectonic Evolution. Earth Science, 45(1): 211-225. doi: 10.3799/dqkx.2018.342
    Citation: Li Tian, Xie Guoai, Zhang Jin, Qu Junfeng, Zhang Beihang, Zhao Heng, Tian Rongsong, Aimierding·Aierken, Li Fahao, 2020. Characteristics of the Tectonic Stress Field of the South-North Oriented Fault of the Langshan Mountain Region of Inner Mongolia and Its Relationship with Regional Tectonic Evolution. Earth Science, 45(1): 211-225. doi: 10.3799/dqkx.2018.342

    内蒙古狼山地区南北向断裂构造应力场特征及其与区域构造演化关系

    doi: 10.3799/dqkx.2018.342
    基金项目: 

    国家重点研发计划项目 2018YFC0603703

    国家重点研发计划项目 2017YFC0601301

    南京大学“十三五”实验教学改革研究课题项目 SY201913

    详细信息
      作者简介:

      李甜(1995-), 女, 硕士研究生, 构造地质专业

      通讯作者:

      解国爱

    • 中图分类号: P611

    Characteristics of the Tectonic Stress Field of the South-North Oriented Fault of the Langshan Mountain Region of Inner Mongolia and Its Relationship with Regional Tectonic Evolution

    • 摘要: 内蒙古狼山地区断裂构造十分复杂,主要发育有南北、东西、北东和北西走向的断裂构造.从南北向断裂的几何形态、运动性质、构造应力场特征入手进行研究,结合野外实地调查与测量,运用极射赤平投影方法,求出构造应力场的主应力轴方位,进而对本区的构造演化进行了探讨.初步认为,研究区发育的近南北向断裂至少受到过两期构造应力场的作用,第一期是在晚二叠世,由于华北克拉通向北、西伯利亚板块向南活动而形成碰撞拼贴运动所产生的近南北向近水平挤压构造应力场,此时构造应力场的主应力轴σ1为北偏东10°左右,向北倾伏,倾伏角为15°~20°.在这一期构造应力场的作用下,狼山地区发育了一套破裂系统,它们分别表现为近东西走向的挤压构造带和逆断层、近北东走向的以左行为主的走滑断层、近北西走向的以右行为主的走滑断层以及近南北走向的张性断层.这些早期的断裂系统也制约着该区域后来的构造活动,第二期构造应力场是侏罗纪以来古太平洋板块向亚洲大陆俯冲而产生的.此构造应力场的主应力轴σ1为北西-南东向,倾伏向为150°左右,倾伏角为10°~20°.第二期构造应力场的作用,使早期南北向断裂由原来的张性破裂面转为左行走滑,早期东西向断裂转为右行走滑,早期北东向左行滑动面转为压性面和褶皱轴方向,而早期的北西向破裂面则转为张性破裂性质.

       

    • 图  1  阿拉善地块及邻区地质图

      图中方框为研究区;据田荣松等(2017)

      Fig.  1.  Geological map of the Alxa block and its vicinity

      图  2  研究区南北向断层主要分布位置

      田荣松等(2017)修改

      Fig.  2.  The main distribution of the north-south fault in the study area

      图  3  张性破裂南北向断层剖面素描图(a1、b1、c1)、断层面擦痕(a2、b2、c2)和极射赤平投影图(a3、b3、c3)

      Fig.  3.  Profile sketch map of tensile fracture and N-S trending fault (a1, b1, c1); scratches of fault plane (a2, b2, c2); polar radiographic projection (a3, b3, c3)

      图  4  狼山群与花岗岩断层平面素描图(a); 南北向左行平移断层相当层(b);花岗岩中南北向断层素描图(c、d);花岗岩羽状张节理照片(e);狼山群拖曳褶皱素描图(f、g);狼山群拖曳褶皱野外照片(h);南北向左行平移断层剖面图(i、l、o);南北向断层带照片(j);极射赤平投影图(k、n、q);南北向左行平移断层擦痕照片(m、p)

      Fig.  4.  Plane sketch of fault in granite and Langshan Group (a); a layer of N-S scratch of left-lateral strike-slip fault (b); sketch of N-S faults in granite (c, d); picture of pinnate tension joint in granite (e); sketch of drag fold in Langshan Group (f, g); field photo of Langshan Group drag fold (h); profile map of N-S left-lateral strike-slip fault (i, l, o); N-S fault zone photograph (j); polar radiographic projection (k, n, q); photo of N-S scratch of left-lateral strike-slip (m, p)

      图  5  南北向断层平面(a);左行平移擦痕(b、h);极射赤平投影(c、f、i、l);南北向断层剖面(d、g、j);断层破碎带(e、k)

      Fig.  5.  The floor plan of N-S fault (a); scratch of left-lateral strike-slip (b, h); polar radiographic projection (c, f, i, l); profile map of N-S fault (d, g, j); fault zone (e, k)

      图  6  花岗岩与狼山群的断层接触(a、d、g);野外断层照片(b);左行擦痕的极射赤平投影(c、f、i、m);南北向断层面左行擦痕(e、h、j);派生褶皱(k);派生褶皱两翼产状统计极密图(l)

      Fig.  6.  Fault contact of granite and Langshan Group (a, d, g); field photograph of fault (b); polar radiographic projection of scratches of left-lateral (c, f, i, m); scratches of left-lateral in N-S fault (e, h, j); the derived fold (k); statistical tightness diagram from the two wings occurrence of derived fold (l)

      图  7  共轭节理赤平投影及应力场分析

      a.狼山群岩层发育的垂直于层面的早期平面共轭X型节理;b.共轭节理极密图;c.极射赤平投影,红色为地层恢复水平后的应力场

      Fig.  7.  Plane projection of conjugate jointsand stress field analysis diagram

      图  8  断层面赤平投影及应力场分析

      a.近东西走向的逆冲断层剖面;b.断层面;c.极射赤平投影

      Fig.  8.  Plane projection of fault plane and stress field analysis diagram

      图  9  应变椭球分析

      a.第一期南北向挤压构造应力场应变椭球分析;b.第二期北西‒南东向挤压构造应力场应变椭球分析

      Fig.  9.  An analysis of stress field

      图  10  褶皱的赤平投影及其相应应力场分析

      a.褶皱剖面素描图;b.褶皱露头;c.褶皱两翼产状投影极密图;d.极射赤平投影图

      Fig.  10.  Plane projection of fold and its corresponding stress field analysis diagram

      表  1  由共轭节理求出的主应力场

      Table  1.   The principal stress field obtained from conjugate joints

      地层产状 主应力轴
      σ1 σ2 σ3
      309°∠50°(左行)、倾斜(160°∠48°) 190°∠23° 322°∠50° 86°∠30°
      231°∠80°(右行)、水平状态 8°∠20° 220°∠68° 103°∠9°
      下载: 导出CSV
    • Dong, S. P., Zhang, P. Z., Zhang, H. P., et al., 2018.Drainage Responses to the Activity of the Langshan Range-Front Fault and Tectonic Implications.Journal of Earth Science, 29(1): 193-209. https://doi.org/10.1007/s12583-017-0902-8
      Gong, W. B., Hu, J. M., Wu, S. J., et al., 2017. Deformation Characteristics, Timing and Significance of the Lang Shan Sinistral Strike-Slip Ductile Shear Zone in Inner Mongolia. Earth Science Frontiers, 24(3):263-275 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dxqy201703024
      Guo, B. C., Hu, G. Z., Guo, J., et al., 2016. Characteristics of the Jilantai Ophiolitic Melange Belt in the Alxa Area, Inner Mongolia, China. Bulletin of Mineralogy, Petrology and Geochemistry, 35(2):247-254 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kwysdqhxtb201602010
      Hu, J. M., Gong, W. B., Wu, S. J., et al., 2014. LA-ICP-MS Zircon U-Pb Dating of the Langshan Group in the Northeast Margin of the Alxa Block, with Tectonic Implications. Precambrian Research, 255: 756-770. https://doi.org/10.1016/j.precamres.2014.08.013
      Li, T., Yan, X. Y., Xie, G. A., et al., 2017. The Geological Structure and Quantitative Study of the Fault in Mufushan Area in Nanjing. Journal of Geology, 41(4):631-636 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=jsdz201704016
      Li, Y. L., Zhou, H. W., Zhong, Z. Q., et al., 2009. Collision Processes of North China and Siberian Plates: Evidence from LA-ICP-MS Zircon U-Pb Age on Deformed Granite in Xar Moron Suture Zone. Earth Science, 34(6):931-938 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/dqkx200906007
      Liu, C. H., Zhao, G. C., Liu, F. L., et al., 2017. Detrital Zircon U-Pb and Hf Isotopic and Whole-Rock Geochemical Study of the Bayan Obo Group, Northern Margin of the North China Craton: Implications for Rodinia Reconstruction. Precambrian Research, 303: 372-391. https://doi.org/10.1016/j.precamres.2017.04.033
      Liu, M., Zhang, D., Xiong, G. Q., et al., 2016. Zircon U-Pb Age, Hf Isotope and Geochemistry of Carboniferous Intrusions from the Langshan Area, Inner Mongolia: Petrogenesis and Tectonic Implications. Journal of Asian Earth Sciences, 120: 139-158. https://doi.org/10.1016/j.jseaes.2016.01.005
      Meng, Q. P., He, Y. K., Zhang, W., et al., 2013. Time Constraints on the Closure of the Paleo-Asian Ocean on the Northern Margin of North China Craton:Evidence from Xihouhaozisyn-Collisional Granites in Siziwang Qi Area. Geological Bulletin of China, 32(11):1749-1759 (in Chinese with English abstract). http://cn.bing.com/academic/profile?id=0fbc28f0c1f95e9fc7eafdd321bb1390&encoded=0&v=paper_preview&mkt=zh-cn
      Peng, R. M., Zhai, Y. S., Wang, J. P., et al., 2010. Discovery of Neoproterozoic Acid Volcanic Rock in the South-Western Section of Langshan, Inner Mongolia.Chinese Science Bulletin, 55(26):2611-2620 (in Chinese). doi: 10.1360/972010-266
      Shen, C. L., Zhang, M., Yang, S. S., et al., 2009.The Geological Evidences and Significance of Westard Extension of Langshan-Zhaertai Shan Rift System, Northern Margin of North China Terrane.Geology and Exploration, 45(6):661-668 (in Chinese with English abstract). http://cn.bing.com/academic/profile?id=ccff670dbc8d92cf5628c1d3c1310711&encoded=0&v=paper_preview&mkt=zh-cn
      Song, D. F., Xiao, W. J., Collins, A. S., et al., 2017. New Chronological Constrains on the Tectonic Affinity of the Alxa Block, NW China. Precambrian Research, 299: 230-243. https://doi.org/10.1016/j.precamres.2017.07.015
      Tang, J., Xu, W. L., Wang, F., et al., 2018. Subduction History of the Paleo-Pacific Slab beneath Eurasian Continent: Mesozoic-Paleogene Magmatic Records in Northeast Asia. Science China Earth Sciences. 48(5): 549-583 (in Chinese with English abstract). http://cn.bing.com/academic/profile?id=3c4a3145074916703e3f1ea35e6adbf6&encoded=0&v=paper_preview&mkt=zh-cn
      Tian, R. S., Xie, G. A., Zhang, J., et al., 2017. Deformation Characteristics of the Neoproterozoic Langshan Group in Langshan Region and Their Tectonic Implications. Geological Review. 63(5):1180-1192 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzlp201705005
      Van der Voo, R., Spakman, W., Bijwaard, H., 1999. Mesozoic Subducted Slabs under Siberia. Nature, 397(6716): 246-249. https://doi.org/10.1038/16686
      Wang, W. L., Teng, X. J., Liu, Y., et al., 2019. The Discovery of Earliest Middle Triassic C-Type Adakite from Langshan Area, Inner Mongolia and Its Tectonic Implications. Earth Science, 44(1):220-233 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/dqkx201901016
      Wang, X. J., 2012. The Geochemical Characters and Its Tectonic Implications of Ophiclites in Alax Area, Inner Mongolia(Dissertation), China University of Geosciences, Beijing (in Chinese with English abstract).
      Wang, Z. Z., Han, B. F., Feng, L. X., et al., 2015. Geochronology, Geochemistry and Origins of the Paleozoic-Triassic Plutons in the Langshan Area, Western Inner Mongolia, China. Journal of Asian Earth Sciences, 97: 337-351. https://doi.org/10.1016/j.jseaes.2014.08.005
      Wang, Z. Z., Han, B. F., Feng, L. X., et al., 2016. Tectonic Attribution of the Langshan Area in Western Inner Mongolia and Implications for the Neoarchean-Paleoproterozoic Evolution of the Western North China Craton: Evidence from LA-ICP-MS Zircon U-Pb Dating of the Langshan Basement. Lithos, 261: 278-295. https://doi.org/10.1016/j.lithos.2016.03.005
      Xiao. W. J., Han, C. M., Yuan, C., et al., 2006. Unique Carboniferous-Permian Tectonic-Metallogenic Framework of Northern Xinjiang (NW China): Constraints for the Tectonics of the Southern Paleoasian Domain. Acta Petrologica Sinica, 22(5):1062-1076 (in Chinese with English abstract). http://cn.bing.com/academic/profile?id=88f14a15822bdd3219539dce53f97d21&encoded=0&v=paper_preview&mkt=zh-cn
      Xiao, W. J., Windley, B. F., Han, C. M., et al., 2018. Late Paleozoic to Early Triassic Multiple Roll-Back and Oroclinal Bending of the Mongolia Collage in Central Asia. Earth-Science Reviews, 186: 94-128. https://doi.org/10.1016/j.earscirev.2017.09.020
      Xu, X. S., 2008. Several Problems Worthy to be Noticed in the Rewearch of Granites and Volcanic Rocks in SE China. Geological Journal of China Universities, 14(3):283-294 (in Chinese with English abstract). http://cn.bing.com/academic/profile?id=4a0fe253e7d3159ff6932cdadf03ddc1&encoded=0&v=paper_preview&mkt=zh-cn
      Xue, S., Ling, M. X., Liu, Y. L., et al., 2017. The Genesis of Early Carboniferous Adakitic Rocks at the Southern Margin of the Alxa Block, North China. Lithos, 278-281: 181-194. https://doi.org/10.1016/j.lithos.2017.01.012
      Zhai, M. G., Peng, P., 2007. Paleoproterozoic Events in the North China Craton.Acta Petrologica Sinica, 23(11):2665-2682 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/ysxb98201307018
      Zhang, B. H., Zhang, J., Zhang, Y. P., et al., 2016a. Tectonic Affinity of the Alxa Block, Northwest China: Constrained by Detrital Zircon U-Pb Ages from the Early Paleozoic Strata on Its Southern and Eastern Margins. Sedimentary Geology, 339: 289-303. https://doi.org/10.1016/j.sedgeo.2016.02.017
      Zhang, J., Zhang, B. H., Zhao, H., 2016b. Timing of Amalgamation of the Alxa Block and the North China Block: Constraints Based on Detrital Zircon U-Pb Ages and Sedimentologic and Structural Evidence. Tectonophysics, 668-669: 65-81. https://doi.org/10.1016/j.tecto.2015.12.006
      Zhang, J., Li, S. Z., Li, X. Y., et al., 2017. Yanshanian Deformation of the Luxi Area: Tectonic Response to the Paleo-Pacifc Plate Subduction. Earth Science Frontiers, 24(4):226-238 (in Chinese with English abstract).
      Zhang, J., Li, J. Y., Li, Y. F., et al., 2007. The Cenozoic Deformation of the Alxa Block in Central Asia-Question on the Northeastern Extension of the Altyn Tagh Fault in Cenozoic Time. Acta Geologica Sinica, 81(11):1481-1497 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dizhixb200711003
      Zhang, J., Li, J. Y., Liu, J. F., et al., 2012. The Relationship between the Alashan Block and the North China Block in the Early Paleozoic: Information from Zircons from the Middle Ordovician in the Eastern Margin of Alashan. Acta Petrologica Sinica, 28(9):2912-2934 (in Chinese with English abstract).
      Zhang, J., Li, J. Y., Liu, J. F., et al., 2013. LA-ICP-MS U-Pb Ages of Pillow Lava Basalts in Southwestern Langshan, Inner Mongolia and Their Implication. Geological Bulletin of China, 32(Z1):287-296 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgqydz201302008
      Zhang, W., Wu, T. R., Feng, J. C., et al. 2013. Time Constraints for the Closing of the Paleo-Asian Ocean in the Northern Alxa Region: Evidence from Wuliji Granites. Science in China (Series D), 43(8):1299-1311 (in Chinese with English abstract). http://cn.bing.com/academic/profile?id=247981492e0e3968d45bc6873be2aa66&encoded=0&v=paper_preview&mkt=zh-cn
      Zhang, X. F., Zhang, S. H., Meng, X. G., et al., 2014. The Identification of Mesozoic Pacific Plate Subduction: Evidence from Paleomagnetism of the Late Triassic Bedded Cherts in Raohe Area, Eastern Heilongjiang Province. Geology in China, 41(6):2019-2027 (in Chinese with English abstract). http://www.cqvip.com/QK/90050X/201406/663633705.html
      Zheng, R. G., Wu, T. R., Zhang, W., et al., 2013. Geochronology and Geochemistry of the Yagan Granite in the Northern Margin of the Alxa Block: Constraints on the Tectonic Evolution of the Southern Altaids. Acta Petrologica Sinica, 29(8):2665-2675 (in Chinese with English abstract).
      公王斌, 胡健民, 吴素娟, 等, 2017.内蒙古狼山左行走滑韧性剪切带变形特征、时间及意义.地学前缘, 24(3):263-275. http://d.old.wanfangdata.com.cn/Periodical/dxqy201703024
      郭秉成, 胡国泽, 郭婧, 等, 2016.阿拉善吉兰泰地区蛇绿混杂堆积带特征.矿物岩石地球化学通报, 35(2): 247-254. doi: 10.3969/j.issn.1007-2802.2016.02.009
      李甜, 燕晓莹, 解国爱, 等, 2017.南京幕府山地区地质构造特征及断层量化.地质学刊, 41(4):631-636. doi: 10.3969/j.issn.1674-3636.2017.04.016
      李益龙, 周汉文, 钟增球, 等, 2009.华北与西伯利亚板块的对接过程:来自西拉木伦缝合带变形花岗岩锆石LA-ICP-MS U-Pb年龄证据.地球科学, 34(6):931-938. doi: 10.3321/j.issn:1000-2383.2009.06.007
      孟庆鹏, 贺元凯, 张文, 等, 2013.华北板块北缘古大洋闭合时间的限定——来自四子王旗西后壕子同碰撞花岗岩的证据.地质通报, 32(11):1749-1759. doi: 10.3969/j.issn.1671-2552.2013.11.007
      彭润民, 翟裕生, 王建平, 等, 2010.内蒙狼山新元古代酸性火山岩的发现及其地质意义.科学通报, 55(26):2611-2620. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kxtb201026008
      沈存利, 张梅, 杨帅师, 等, 2009.华北陆块北缘西段狼山-渣尔泰山裂陷槽西延的地质依据及其意义.地质与勘探, 45(6):661-668. http://d.old.wanfangdata.com.cn/Periodical/dzykt200906005
      唐杰, 许文良, 王枫, 等, 2018.古太平洋板块在欧亚大陆下的俯冲历史:东北亚陆缘中生代-古近纪岩浆记录.中国科学:地球科学, 48(5):549-583. http://www.cnki.com.cn/Article/CJFDTotal-JDXK201805004.htm
      田荣松, 解国爱, 张进, 等, 2017.内蒙古狼山地区新元古代狼山群变形特征及区域构造意义.地质论评, 63(5):1180-1192. http://d.old.wanfangdata.com.cn/Periodical/dzlp201705005
      王文龙, 滕学建, 刘洋, 等, 2019.内蒙古狼山地区中三叠世早期C型埃达克岩的发现及其构造意义.地球科学, 44(1):220-233. doi: 10.3799/dqkx.2018.275
      王行军, 2012.内蒙古阿拉善地区蛇绿岩的地球化学特征及其构造意义(博士学位论文).北京: 中国地质大学. http://cdmd.cnki.com.cn/Article/CDMD-11415-1012364413.htm
      肖文交, 韩春明, 袁超, 等, 2006.新疆北部石炭纪-二叠纪独特的构造-成矿作用:对古亚洲洋构造域南部大地构造演化的制约.岩石学报, 22(5):1062-1076. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200605002
      徐夕生. 2008.华南花岗岩-火山岩成因研究的几个问题.高校地质学报, 14(3):283-294. doi: 10.3969/j.issn.1006-7493.2008.03.001
      翟明国, 彭澎, 2007.华北克拉通古元古代构造事件.岩石学报, 23(11):2665-2682. doi: 10.3969/j.issn.1000-0569.2007.11.001
      张剑, 李三忠, 李玺瑶, 等, 2017.鲁西地区燕山期构造变形:古太平洋板块俯冲的构造响应.地学前缘, 24(4):226-238. http://d.old.wanfangdata.com.cn/Periodical/dxqy201704021
      张进, 李锦轶, 李彦峰, 等, 2007.阿拉善地块新生代构造作用——兼论阿尔金断裂新生代东向延伸问题.地质学报, 81(11):1481-1497. doi: 10.3321/j.issn:0001-5717.2007.11.003
      张进, 李锦轶, 刘建峰, 等, 2012.早古生代阿拉善地块与华北地块之间的关系:来自阿拉善东缘中奥陶统碎屑锆石的信息.岩石学报, 28(9):2912-2934. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201209020
      张进, 李锦轶, 刘建峰, 等, 2013.内蒙古狼山西南地区枕状玄武岩LA-ICP-MS锆石U-Pb年龄及意义.地质通报, 32(Z1):287-296. http://d.old.wanfangdata.com.cn/Periodical/zgqydz201302008
      张文, 吴泰然, 冯继承, 等, 2013.阿拉善地块北缘古大洋闭合的时间制约:来自乌力吉花岗岩体的证据.中国科学(D辑), 43(8):1299-1311. http://www.cnki.com.cn/Article/CJFDTotal-JDXK201308006.htm
      张雪锋, 张世红, 孟宪刚, 等, 2014.太平洋板块中生代俯冲构造事件的响应:来自黑龙江东部饶河三叠纪层状燧石的古地磁证据.中国地质, 41(6):2019-2027. doi: 10.3969/j.issn.1000-3657.2014.06.016
      郑荣国, 吴泰然, 张文, 等, 2013.阿拉善地块北缘雅干花岗岩体地球化学、地质年代学及其对区域构造演化制约.岩石学报, 29(8):2665-2675. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201308004
    • 加载中
    图(10) / 表(1)
    计量
    • 文章访问数:  4221
    • HTML全文浏览量:  1436
    • PDF下载量:  101
    • 被引次数: 0
    出版历程
    • 收稿日期:  2018-09-26
    • 刊出日期:  2020-01-15

    目录

      /

      返回文章
      返回