大兴安岭南段阿鲁科尔沁旗地区林西组沉积环境特征及其时限的地质意义

doi:10.13278/j.cnki.jjuese.20190292

Abstract

Abstract: Aiming at the controversial issues such as the sedimentary environment, time-limit of Linxi Formation, and the final closing time of the Paleo-Asian Ocean in Xingmeng-Songnen area,a comprehensive analysis was conducted for the lithology and paleontology of Linxi Formation in Hanmiao area of Arhorchin Banner, in particular,the trace elements, and the U-Pb dating of detrital zircon. The ratio of trace elements Sr/Ba is mainly distributed between 0.05 and 0.18 (average 0.12), the ratio of B/Ga is mainly distributed between 1.84 and 3.22 (average 2.50), and the V/Cr value is between 1.36 and 2.21 (average 1.81), which indicate that the sedimentary period of Linxi Formation was an anoxic freshwater lake environment. The freshwater bivalves and leaf-lime fossils are developed in Linxi Formation. The sandstone clastic zircons of Linxi Formation have multi-epoch provenance. The youngest age is 251 Ma, reflecting the lower sedimentary age in Late Permian. Based on the above characteristics, it can be inferred that the final closing time of the Paleo-Asian Ocean in the study area is the end of the Middle Permian, and the study area transformed into continental sediments during the Late Permian.

Key words: Linxi Formation, sedimentary environment, sedimentary time-limit, Paleo-Asian Ocean, Southern Great Xing'an ranges

CLC Number:

P588.2

Dong Qingshui, He Chunsheng, Lou Renxing, Ren Xigang, Zhang Chao, Zhang Yujin, Xu Shengchuan. Geological Significance of Sedimentary Environment Characteristics and Time Limit of Linxi Formation in Arhorchin Banner, Southern Great Xing’an Range[J].Journal of Jilin University(Earth Science Edition), 2020, 50(2): 425-441.

References

[1] 李锦轶,高立明,孙桂华,等. 内蒙古东部双井子中三叠世同碰撞壳源花岗岩的确定及其对西伯利亚与中朝古板块碰撞时限的约束[J].岩石学报,2007,23(3):565-582. Li Jinyi, Gao Liming, Sun Guihua, et al. Determination of the Middle Triassic Syn-Collisional Crust Source Granite in Shuangjingzi, Eastern Inner Mongolia and Its Constraints on the Collision Time Limit Between Siberia and Sino Korean Ancient Plates[J]. Acta Petrologica Sinica, 2007, 23(3):565-582.
[2] 孙德有,吴福元,张艳斌,等. 西拉木伦河-长春-延吉板块缝合带的最后闭合时间:来自吉林大玉山花岗岩体的证据[J]. 吉林大学学报(地球科学版), 2004, 34(2):174-181. Sun Deyou, Wu Fuyuan, Zhang Yanbin, et al.The Final Closing Time of the West Lamulun River-Changchun-Yanji Plate Suture Zone Evidence from the Dayushan Granitic Pluton, Jilin Province[J]. Journal of Jilin University (Earth Science Edition), 2004, 34(2):174-181.
[3] 刘永江,张兴洲,金巍,等. 东北地区晚古生代区域构造演化[J].中国地质,2010,37(4):943-951. Liu Yongjiang, Zhang Xingzhou, Jin Wei, et al. Late Paleozoic Regional Tectonic Evolution in Northeast China[J]. Chinese Geology, 2010, 37(4):943-951.
[4] Tang K D. Tectonic Development of Paleozoic Foldbelts at the North Margin of the Sino-Korean Craton[J]. Tectonics,1990, 9(2):249-260.
[5] Xu B, Zhao P, Wang Y Y, et al.The Pre-Devonian Tectonic Framework of Xing'an-Mongolia Orogenic Belt (XMOB) in North China[J]. Journal of Asian Earth Sciences,2015,97:183-196.
[6] 徐备,陈斌. 内蒙古北部华北板块与西伯利亚板块之间中古生代造山带的结构与演化[J]. 中国科学:D辑,1997, 27(3):227-232. Xu Bei, Chen Bin. The Structure and Evolution of the Mesozoic Orogenic Belt Between the North China Plate and the Siberian Plate in Northern Inner Mongolia[J]. Chinese Science:Series D,1997, 27(3):227-232.
[7] 邵济安. 中朝板块北缘中段地壳演化[M]. 北京:北京大学出版社,1991:1-136. Shao Ji'an. Crustal Evolution in the Middle Part of the Northern Margin of the Sino Korean Plate[M]. Beijing:Peking University Press, 1991:1-136.
[8] 任纪舜,陈廷愚,牛宝贵,等. 中国东部及邻区大陆岩石圈的构造演化与成矿[M]. 北京:科学出版社, 1990:1-205. Ren Jishun, Chen Tingyu, Niu Baogui, et al. Tectonic Evolution and Mineralization of Continental Lithosphere in Eastern China and Its Adjacent Areas[M]. Beijing:Science Press, 1990:1-205.
[9] 曹从周,孙芳林,田昌烈,等.内蒙古贺根山地区蛇绿岩及中朝板块和西伯利亚板块之间的缝合带位置[C]//中国北方板块构造论文集. 北京:地质出版社,1986:64-86. Cao Congzhou, Sun Fanglin, Tian Changlie, et al. Ophiolite in Hegenshan Area of Inner Mongolia and the Position of Suture Zone Between China Korea Plate and Siberia Plate[C]//Proceedings of Plate Tectonics in Northern China. Beijing:Geological Publishing House, 1986:64-86.
[10] 张艳斌, 吴福元, 孙德有,等.延边"早海西期"棉田花岗岩和仲坪紫苏辉石闪长岩的单颗粒锆石U-Pb定年[J]. 地质论评, 2002,48(4):424-429. Zhang Yanbin, Wu Fuyuan, Sun Deyou, et al. Single Zircon U-Pb Dating of "Early Hercynian" Miantian Granite and Zhongping Perilla Pyroxene Diorite in Yanbian[J]. Geological Review,2002, 48(4):424-429.
[11] 张艳斌, 吴福元, 李惠民,等.吉林黄泥岭花岗岩体的单颗粒锆石U-Pb年龄[J].岩石学报, 2002,18(4):475-481. Zhang Yanbin, Wu Fuyuan, Li Huimin, et al. Single Zircon U-Pb Age of Huangniling Granite in Jilin Province[J]. Acta Petrologica Sinica,2002,18(4):475-481.
[12] 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 Genesis[J]. Acta Petrologica Sinica,2007, 23(6):1217-1238.
[13] Xiao W J, Windley F B, Hao J,et al. Accretion Leading to Collision and the Permian Solonker Suture, Inner Mongolia, China:Termination of the Central Asian Orogenic Belt[J]. Tectonics,2003, 22(6):8-17.
[14] 刘兵,温全波,刘永江,等.大兴安岭中段上二叠统-下三叠统接触关系研究:来自碎屑锆石年代学的证据[J].大地构造与成矿学, 2014, 38(2):408-420. Liu Bing, Wen Quanbo, Liu Yongjiang, et al. Study on the Contact Relationship Between the Upper Permian and the Lower Triassic in the Middle Part of the Daxing'anling Mountains:Evidence from Zircon Chronology[J]. Geotectonics and Metallogeny, 2014, 38(2):408-420.
[15] Zhou Jianbo,Wilde S A. The Crustal Accretion History and Tectonic Evolution of the NE China Segment of the Central Asian Orogenic Belt[J]. Gondwana Research, 2013,23:1365-1377.
[16] 张永生,牛邵武,田树刚,等.内蒙古林西地区上二叠统林西组叶肢介化石的发现及意义[J].地质通报,2012, 31(9):1394-1403. Zhang Yongsheng, Niu Shaowu, Tian Shugang, et al. Discovery and Significance of Phyllodactyls from the Upper Permian Linxi Formation in Linxi Area, Inner Mongolia[J]. Geological Bulletin of China, 2012,31(9):1394-1403.
[17] 翟大兴,张永生,田树刚,等.内蒙古林西地区上二叠统林西组沉积环境与演变[J].古地理学报,2015,17(3):359-370. Zhai Daxing, Zhang Yongsheng, Tian Shugang, et al. Sedimentary Environment and Evolution of Upper Permian Linxi Formation in Linxi Area, Inner Mongolia[J]. Journal of Paleogeography, 2015,17(3):359-370.
[18] 陈晨,彭晓蕾,洪雪,等.内蒙古东北部上二叠统林西组暗色泥岩有机地球化学特征及其意义[J].世界地质, 2013,32(2):331-336. Chen Chen, Peng Xiaolei, Hong Xue, et al.Organic Geochemical Characteristics of Dark Mudstone in Upper Permian Linxi Formation from Northeast Inner Mongolia, China[J]. World Geology, 2013,32(2):331-336.
[19] Lou Renxing, Dong Qingshui, Nie Hui. Exploration Prospects of Shale Gas Resources in the Upper Permian Linxi Formation in Suolun-Linxi Area, NE China[J]. Energy & Fuels, 2017,31:1100-1107.
[20] 郑月娟,黄欣,孙跃武,等. 松辽盆地及外围石炭系-二叠系划分与对比[J].地质与资源,2018,27(1):1-15. Zheng Yuejuan, Huang Xin, Sun Yuewu, et al. Division and Correlation of Carboniferous Permian System in Songliao Basin and Its Periphery[J]. Geology and Resources, 2018,27(1):1-15.
[21] 刘永江,张兴洲,迟效国,等.大兴安岭地区上古生界变形特征及构造层划分[J]. 吉林大学学报(地球科学版), 2011,41(5):1304-1313. Liu Yongjiang, Zhang Xingzhou, Chi Xiaoguo, et al. Deformation and Tectonic Layer Division of Upper Paleozoic in Daxing'anling Area[J]. Journal of Jilin University (Earth Science Edition), 2011,41(5):1304-1313.
[22] 朱如凯,许怀先,邓胜徽,等. 中国北方地区二叠纪岩相古地理[J].古地理学报,2007,9(2):133-142. Zhu Rukai, Xu Huaixian, Deng Shenghui, et al. Lithofacies Paleogeography of the Permian in Northern China[J]. Journal of Paleogeography, 2007,9(2):133-142.
[23] 余和中. 松辽盆地及周边地区石炭纪-二叠纪岩相古地理[J]. 沉积与特提斯地质, 2001, 21(4):71-83. Yu Hezhong. Sedimentary Facies and Palaeogeography of the Songliao Basin and Its Peripheral Areas During Carboniferous-Permian Time[J]. Sedimentary Geology and Tethyan Geology,2001, 21(4):71-83.
[24] 黄本宏.天山-兴安褶皱带石炭二叠纪植物群[J].科学通报,1980(15):703-705. Huang Benhong. Carbon Permian Flora of Tianshan-Xing'an Fold Belt[J]. Chinese Science Bulletin, 1980(15):703-705.
[25] 黄本宏.东北北部石炭-二叠纪陆相地层及古地理概况[J].地质论评,1982,28(5):395-402. Huang Benhong. Carboniferous Permian Continental Stratigraphy and Paleogeography in Northern Northeast China[J]. Geological Review, 1982,28(5):395-402.
[26] 李福来,曲希玉,刘立,等.内蒙古东北部上二叠统林西组沉积环境[J].沉积学报, 2009, 27(2):265-272. Li Fulai, Qu Xiyu, Liu Li, et al. Sedimentary Environment of the Upper Permian Linxi Formation in Northeastern Inner Mongolia[J]. Acta Sedimentologica Sinica, 2009, 27(2):265-272.
[27] 邱余波,伊海生,蔡占虎,等.内蒙古锡林浩特-阿鲁科尔沁地区林西组岩相古地理特征[J].成都理工大学学报(自然科学版),2014,41(2):192-202. Qiu Yubo, Yi Haisheng, Cai Zhanhu, et al. Paleogeographic Characteristics of the Petrographic Facies of the Linxi Formation in Xilinhot-Alukorqin Area, Inner Mongolia[J]. Journal of Chengdu University of Technology (Natural Science Edition), 2014, 41(2):192-202.
[28] 朱常伟,张永生,何幼斌,等.内蒙古林西地区上二叠统林西组三段沉积环境分析[J].中国科技论文, 2017, 12(15):1725-1731. Zhu Changwei, Zhang Yongsheng, He Youbin, et al. Sedimentary Environment Analysis of the Third Member of the Upper Permian Linxi Formation in Linxi Area,Inner Mongolia[J]. China Science and Technology Paper, 2017, 12(15):1725-1731.
[29] 中国地质科学院地质研究所. 新疆吉木萨尔大龙口二叠-三叠纪地层及古生物[M]. 北京:地质出版社, 1986. Institute of Geology, Chinese Academy of Geosciences. Permian Triassic Strata and Paleontology, Dalongkou, Jimsar, Xinjiang[M]. Beijing:Geological Publishing House, 1986.
[30] 内蒙古自治区地质矿产矿局. 内蒙古自治区岩石地层[M]. 武汉:中国地质大学出版社, 1996. Inner Mongolia Geology and Mineral Resources Bureau. Inner Mongolia Lithostratigraphy[M]. Wuhan:China University of Geosciences Press, 1996.
[31] 郑荣才,柳梅青. 鄂尔多斯盆地长6油层组古盐度研究[J].石油与天然气地质,1999,20(1):20-25. Zheng Rongcai, Liu Meiqing.Paleosalinity Study of Chang 6 Reservoir Group in Ordos Basin[J]. Petroleum and Natural Gas Geology, 1999,20(1):20-25.
[32] 文华国,郑荣才,唐飞,等. 鄂尔多斯盆地耿湾地区长6段古盐度恢复与古环境分析[J].矿物岩石,2008,28(1):114-120. Wen Huaguo, Zheng Rongcai, Tang Fei, et al. Paleosalinity Restoration and Paleoenvironment Analysis of the Chang 6 Member in Gengwan Area, Ordos Basin[J]. Mineral Rocks, 2008,28(1):114-120.
[33] 刘招君,孟庆涛,柳蓉,等. 抚顺盆地始新统计军屯组油页岩地球化学特征及其地质意义[J].岩石学报,2009,25(10):2340-2350. Liu Zhaojun, Meng Qingtao, Liu Rong, et al.Geochemical Characteristics of Oil Shale of Eocene Jijuntun Formation and Its Geological Significance,Fushun Basin.[J]. Acta Petrologica Sinica, 2009,25(10):2340-2350.
[34] 王争鸣. 缺氧沉积环境的地球化学标志[J].甘肃地质学报,2003,12(2):55-58. Wang Zhengming. Geochemical Indicators of Anoxic Sedimentary Environment[J]. Journal of Geology of Gansu Province, 2003,12(2):55-58.
[35] 李牛,胡超涌,马仲武,等. 四川广元上寺剖面上二叠统大隆组优质烃源岩发育主控因素初探[J]. 古地理学报,2011,13(3):347-354. Li Niu, Hu Chaoyong, Ma Zhongwu, et al.Main Control Factors of High Quality Hydrocarbon Source Rocks of the Upper Permian Dalong Formation at Shangsi Section of Guangyuan,Sichuan Province[J]. Journal of Paleogeography, 2011,13(3):347-354.
[36] Blank L P, Kamo S L,Williams I S,et al. The Application of SHRIMP to Phanerozoic Geochronology:A Critical Appraisal of Four Zircon Standards[J]. Chemical Geology, 2003,200(1/2):171-188.
[37] 金玉玕,尚庆华,侯静鹏,等.中国地层典:二叠系[M].北京:地质出版社, 2000. Jin Yugan, Shang Qinghua, Hou Jingpeng, et al. Stratigraphical Lexicon of China:Permian[M].Beijing:Geological Publishing House, 2000.
[38] 汪啸风,陈孝红.中国各地质时代地层划分与对比[M].北京:地质出版社, 2005. Wan Xiaofeng, Chen Xiaohong. Stratigraphic Division and Correlation of Each Geologic Period in China[M]. Beijing:Geological Publishing House, 2005.
[39] 杨兵,张雄华,葛梦春,等. 内蒙古林西地区晚二叠世-早三叠世孢粉组合及三叠系的发现[J]. 地球科学:中国地质大学学报,2014,39(7):784-794. Yang Bing, Zhang Xionghua, Ge Mengchun, et al. Late Permian-Early Triassic Palynological Assemblages in Linxi, Inner Mongolia and Discovery of Triassic Strata[J]. Earth Science:Journal of China University of Geosciences, 2014,39(7):784-794.
[40] 李树才,张雄华, 李沅柏,等. 内蒙古林西地区林西组地质时代及沉积环境[J]. 地质科技情报,2019, 38(1):1-7. Li Shucai, Zhang Xionghua, Li Yuanbai, et al. Geological Age of Linxi Formation in Linxi, Inner Mongolia, and Its Sedimentary Environment[J]. Geological Science and Technology Information, 2019,38(1):1-7.
[41] 朱儒峰, 郑广瑞. 大兴安岭南部下三叠统幸福之路组的建立及其地质意义[J]. 中国区域地质,1992(3):219-225. Zhu Rufeng, Zheng Guangrui.The Establishment of the Lower Triassic Xingfuzhilu Formation in the Southern Secter of the Greater Khingan Mountains and Its Geological Implications[J]. Regional Geology of China, 1992(3):219-225.
[42] 张渝金,张超,郭建刚,等. 大兴安岭南段阿鲁科尔沁旗坤都地区林西组碎屑锆石U-Pb年龄、地球化学特征及其地质意义[J].地质通报,2018,37(9):1682-1692. Zhang Yujin, Zhang Chao, Guo Jiangang, et al. U-Pb Dating of Detrital Zircons and Geochemical Characteristics of Linxi Formation in the Kundu Area of Ar Horqin Banner, Southern Da Xing'anling Mountains and Their Geological Significance[J]. Geological Bulletin of China, 2018, 37(9):1682-1692.
[43] 韩杰,周建波,张兴洲,等. 内蒙古林西地区上二叠统林西组砂岩碎屑锆石的年龄及其大地构造意义[J].地质通报,2011,30(2):258-269. Han Jie, Zhou Jianbo, Zhang Xingzhou, et al. Detrital Zircon U-Pb Dating from Sandstone of the Upper Permian Linxi Formation,Linxi Area, Inner Mongolia, China and Its Tectonic Implications[J]. Geological Bulletin of China, 2011, 30(2):258-269.
[44] Miao L C, Fan W M, Liu D Y, et al. Geochronology and Geochemistry of the Hegenshan Ophiolitic Complex:Implications for Late-Stage Tectonic Evolution of the Inner Mongolia-Daxing'anling Orogenic Belt, China[J]. Journal of Asian Earth Sciences, 2008,32:348-370.
[45] 关庆彬,刘正宏,白新会,等.内蒙古巴林右旗新开坝地区大石寨组火山岩形成时代及构造背景[J].岩石学报, 2016,32(7):2029-2040. Guan Qingbin,Liu Zhenghong,Bai Xinhui, et al. Age and Tectonic Setting of Volcanic Rocks of the Dashizhai Formation from Xinkaiba, Balinyouqi Area, Inner Mongolia[J]. Acta Petrologica Sinica,2016,32(7):2029-2040.
[46] 梅可辰,李秋根,王宗起,等. 内蒙古中部苏尼特左旗大石寨组流纹岩SHRIMP锆石U-Pb年龄、地球化学特征及其构造意义[J]. 地质通报, 2015,34(12):2181-2194. Mei Kechen, Li Qiugen, Wang Zongqi, et al. SHRIMP Zircon U-Pb Age, Geochemistry and Tectonic Significance of the Dashizhai Formation Rhyolites in Sunid Left Banner, Middle Part of Inner Mongolia[J]. Geological Bulletin of China, 2015, 34(12):2181-2194.
[47] 范宏瑞, 胡芳芳, 杨奎峰, 等. 内蒙古白云鄂博地区晚古生代闪长质-花岗质岩石年代学框架及其地质意义[J]. 岩石学报, 2009,25(11):2933-2938. Fan Hongrui, Hu Fangfang, Yang Kuifeng, et al. Chronological Framework of Late Paleozoic Diorite Granitic Piutons in the Bayan Obo Area, Inner Mongolia,and Tectonic Significance[J]. Acta Petrologica Sinica, 2009,25(11):2933-2938.
[48] 陈斌,赵国春,Wilde S.内蒙古苏尼特左旗南两类花岗岩同位素年代学及其构造意义[J].地质论评,2001,47(4):361-367. Chen Bin, Zhao Guochun, Wilde S. Isotopic Geochronology and Its Tectonic Significance of Two Types of Granites in the South of Sunitzuo Banner, Inner Mongolia[J]. Geological Review,2001, 47(4):361-367.
[49] 刘建峰,迟效国,张兴洲,等.内蒙古西乌旗南部石炭纪石英闪长岩地球化学特征及其构造意义[J].地质学报,2009, 83(3):365-376. Liu Jianfeng, Chi Xiaoguo, Zhang Xingzhou, et al. Geochemical Characteristics and Tectonic Significance of Carboniferous Quartz Diorite in the South of Xiwu Banner, Inner Mongolia[J]. Acta Geologica Sinica,2009, 83(3):365-376.
[50] 韩国卿,刘永江,温泉波,等. 西拉木伦河缝合带北侧二叠纪砂岩碎屑锆石LA-ICP-MS U-Pb年代学及其构造意义[J].地球科学:中国地质大学学报,2011,36(4):687-702. Han Guoqing, Liu Yongjiang, Wen Quanbo, et al. LA-ICP-MS U-Pb Dating of Detrital Zircons from the Permian Sandstones in North Side of Xar Moron River Suture Belt and Its Tectonic Implications[J]. Earth Science:Journal of China University of Geosciences,2011, 36(4):687-702.
[51] Liu Y J, Li W M, Feng Z Q, et al. A Review of the Paleozoic Tectonics in the Eastern Part of Central Asian Orogenic Belt[J]. Gondwana Research, 2017, 43:123-148.
[52] Wu F Y, Yang J H, Lo C H, et al. Jiamusi Massif in China:A Jurassic Accrationary Terrane in the Western Pacific[J]. The Island Arc, 2007,16:156-172.
[53] Zhou J B, Wilde S A, Zhao G C, et al. Was the Eastetnmost Segment of the Central Asian Orogenic Belt Serived From Gondwana or Siberia:An Intriguing Dilemma[J]. Geodynamics, 2010, 50(3/4):300-317.
[54] Zheng Y F, Fu B, Gong B, et al. StableIsotope Geochemistry of Ultrahigh Pressure Metamorphic Rocks from the Dabie-Sulu Orogen in China:Implications for Geodynamics and Fluid Regime[J]. Earth Science Reviews, 2003, 62:105-161.
[55] 李雨柯. 内蒙古东部索伦二叠纪哲斯组碎屑锆石U-Pb年龄及其大地构造意义[J].科学技术与工程, 2012, 25(12):6269-6277. Li Yuke. Zircon U-Pb Age and Its Geotectonic Significance of the Permian Zhes Formation in the Eastern Part of Inner Mongolia[J]. Science and Technology and Engineering, 2012, 25(12):6269-6277.
[56] 郭晓丹, 周建波, 张兴洲, 等. 内蒙古西乌珠穆沁旗本巴图组碎屑锆石LA-ICP-MS U-Pb年龄及其意义[J]. 地质通报, 2011, 30(2/3):278-290. Guo Xiaodan, Zhou Jianbo, Zhang Xingzhou, et al. The Detrital Zircon LA-ICP-MS U-Pb Ages and Its Significance of Benbatu Formation in Xiwuzhumuqinqi, Inner Mongolia, China[J]. Geological Bulletin of China, 2011, 30(2/3):278-290.
[57] 葛梦春, 周文孝, 于涛, 等. 内蒙古锡林郭勒杂岩解体及表壳岩系年代确定[J]. 地学前缘, 2011, 18(5):182-195. Ge Mengchun, Zhou Wenxiao, Yu Tao, et al. Disintegration and Supracrustal Rocks Dating of Xilin Gol Complex,Inner Mongolia,China[J]. Earth Science Frontiers, 2011, 18(5):182-195.
[58] 马文璞. 区域构造解析:方法理论和中国板块构造[M].北京:地质出版社, 1992. Ma Wenpu. Regional Tectonic Analysis Methodology and Plate Tectonics in China[M]. Beijing:Geological Publishing House, 1992.
[59] 卜建军,何卫红,张克信,等. 古亚洲洋的演化:来自古生物地层学方面的证据[J].地球科学,(2019-04-10)[2019-09-20].doi:10.3799/dqkx.2019.068. Bu Jianjun, He Weihong, Zhang Kexin,et al. Evolution of the Paleo-Asian Ocean:Evidence from Paleontology and Stratigraphy[J]. Geoscience, (2019-04-10)[2019-09-20]. doi:10.3799/dqkx.2019.068.
[60] 邵济安,唐克东,何国琦,等.内蒙古早二叠世构造古地理的再造[J].岩石学报,2014,30(7):1858-1866. Shao Ji'an,Tang Kedong, He Guoqi. Early Permian Tectono-Palaeogeographic Reconstruction of Inner Mongolia,China[J]. Acta Petrologica Sinica,2014,30(7):1858-1866.

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Geological Significance of Sedimentary Environment Characteristics and Time Limit of Linxi Formation in Arhorchin Banner, Southern Great Xing’an Range

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