Discussion on evolution of Min Jiang River: Heavy mineral evidence from the Quaternary fluvial sediments in Yibin area,Sichuan Province
Li Lei1, Xiang Fang2,3, Liu Yi-Ming4, Tai Zi-Han1
1 College of Earth Sciences,Chengdu University of Technology, Chengdu 610059,China; 2 State Key Laboratory of Oil & Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059,China; 3 Institute of Sedimentary Geology,Chengdu University of Technology, Chengdu 610059,China; 4 Jiangxi Electric Power Design Institute, Nanchang 330000,China
Abstract：Heavy minerals deposited on river terraces can be used to reflect source rock properties and reveal river evolutionary processes. This study focused on the heavy minerals deposited in the lower Min Jiang River terraces and in the modern deposits. We studied paleo-current direction, characteristics of the heavy mineral assemblages, characteristic metamorphic minerals and heavy mineral characteristic indices. The results show that the lower reaches of the Min Jiang River Ⅴ- to Ⅲ-level terrace deposits consist dominantly of magmatic rock type, which mainly comes from the Longmen Shan mountain tectonic belt. The heavy minerals deposited in modern sediment come from the Songpan-Ganzi fold belt. The heavy mineral characteristic indices suggest that this change is due to headward erosion of the Min Jiang River. Affected by the phase B of the Kunhuang movement, the Min Jiang River was incised to the Wenchuan area at 0.73-0.7 Ma and the Ⅴ-level terrace formed. The Min Jiang River was strongly cut down at 0.5-0.3 Ma due to the phase C of the Kunhuang movement, and as a result the Ⅳ-level terrace formed. Influenced by Gonghe movement, the Min Jiang River was incised to the stone mark and Ⅲ-level terrace formed in 0.11-0.09 Ma. After that, the modern Min Jiang River was formed at around 27 ka.
Li Lei,Xiang Fang,Liu Yi-Ming et al. Discussion on evolution of Min Jiang River: Heavy mineral evidence from the Quaternary fluvial sediments in Yibin area,Sichuan Province[J]. JOPC, 2020, 22(4): 761-774.
[1] 崔之久,伍永秋,刘耕年,葛道凯,庞其清,许清海. 1998. 关于“昆仑—黄河运动”. 中国科学D辑: 地球科学, 28(1): 53-59. [Cui Z J,Wu Y Q,Liu G N,Ge D K,Pang Q Q,Xu Q H.1998. On the “Kunlun-Yellow River movement”. Science in China(Series D): Earth Science, 28(1): 53-59] [2] 陈心怡,黄奇瑜,邵磊. 2018. 福建闽江和九龙江现代沉积物重矿物特征及其物源意义. 古地理学报, 20(4): 637-650. [Chen X Y,Huang Q Y,Shao L.2018. Characteristics of heavy minerals in modern sediments of Min Jiang and Jiulongjiangrivers,Fujian Province and their provenance implication. Journal of Palaeogeography(Chinese Edition), 20(4): 637-650] [3] 戴宗明. 2012. 青藏高原东部四姑娘山地区晚新生代隆升. 成都理工大学博士学位论文: 1-167. [Dai Z M.2012. The Late Cenozoic Uplift of the Four-Girl Mountain Section in the Eastern Tibetan Plateau. Doctoral dissertation of Chengdu University of Technology: 1-167] [4] 方小敏,赵志军,李吉均,颜茂都,潘保田,宋春晖,戴霜. 2004. 祁连山北缘老君庙背斜晚新生代磁性地层与高原北部隆升. 中国科学D辑: 地球科学, 34(2): 97-106. [Fang X M,Zhao Z J,Li J J,Yan M D,Pan B T,Song C H,Dai S.2004. Late Cenozoic magnetic strata of Laojunmiao anticline and uplift of northern Qilian mountain. Science in China(Series D): Earth Science, 34(2): 97-106] [5] 方小敏,宋春晖,戴霜,朱迎堂,高军平,张伟林. 2007. 青藏高原东北部阶段性变形隆升: 西宁、贵德盆地高精度磁性地层和盆地演化记录. 地学前缘, 14(1): 230-242. [Fang X M,Song C H,Dai S,Zhu Y T,Gao J P,Zhang W L.2007. Cenozoic deformation and uplift of the NE Qinghai Tibet: Evidence from high resolution magneto stratigraphy and basin evolution. Earth Science Frontiers, 14(1): 230-242] [6] 姜磊,刘树根,王自剑,李智武,赖东,何宇,罗强,周政,邓宾. 2019. 上扬子盆地西缘晚白垩世物源变化及指示. 地质论评, 65(2): 477-490. [Jiang L,Liu S G,Wang Z J,Li Z W,Lai D,He Y,Luo Q,Zhou Z,Deng B.2019. Provenance change and its indication of Late Cretaceous in the west margin of upper Yangtze basin. Geological Review, 65(2): 477-490] [7] 康春国,李长安,张玉芬,邵磊,江华军. 2014. 宜昌砾石层重矿物组合特征及物源示踪分析. 地质学报, 88(2): 254-261. [Kang C G,Li C A,Zhang Y F,Shao L,Jiang H J.2014. Heavy mineral characteristics of the Yichang gravel layers and provenance tracing. Acta Geologica Sinica, 88(2): 254-261] [8] 来庆洲,丁林,王宏伟,岳雅慧,蔡福龙. 2006. 青藏高原东部边界扩展过程的磷灰石裂变径迹热历史制约. 中国科学D辑: 地球科学, 36(9): 3-14. [Lai Q Z,Ding L,Wang H W,Yue Y H,Cai F L.2006. Historical constraints on apatite fission track heat during the eastern boundary extension of the Qinghai-Tibet Plateau. Science in China(Series D): Earth Science, 36(9): 3-14] [9] 黎兵. 2005. 青藏高原东缘晚新生代隆升的沉积记录与地貌响应. 成都理工大学硕士学位论文: 1-101. [Li B.2005. Sedimentology Record and Geomorphology Response for the Uplift of Eastern Margin of Tibet Plateau in the Late Cenozoic. Masteral dissertation of Chengdu University of Technology: 1-101] [10] 黎兵,李勇,张开均,张玉修,张毅,魏庆国,汪洋. 2007. 青藏高原东缘晚新生代大邑砾岩的物源分析与水系变迁. 第四纪研究, 27(1): 64-73. [Li B,Li Y,Zhang K J,Zhang Y X,Zhang Y,Wei Q G,Wang Y.2007. Provenance of the siliciclastic rocks of the Late Cenozoic Dayi formation and drainage change at eastern margin of the Tibetan Plateau. Quaternary Sciences, 27(1): 64-73] [11] 李廷栋. 1995. 青藏高原隆升的过程和机制. 地球学报,(1): 1-9. [Li T D.1995. The uplifting process and mechanism of the Qinghai-Tibet Plateau. Acta Geoscientia Sinica,(1): 1-9] [12] 李吉均,方小敏,马海洲,朱俊杰,潘保田,陈怀录. 1996. 晚新生代黄河上游地貌演化与青藏高原隆起. 中国科学D辑: 地球科学, 26(4): 316-322. [Li J J,Fang X M,Ma H Z,Zhu J J,Pan B T,Chen H L.1996. The evolution of the upper reaches of the Yellow River and the uplift of the Qinghai-Tibet Plateau in the Late Cenozoic. Science in China(Series D): Earth Science, 26(4): 316-322] [13] 李吉均,方小敏. 1998. 青藏高原隆起与环境变化研究. 科学通报, 43(15): 1569-1574. [Li J J,Fang X M.1998. Study on the uplift of Qinghai-Tibet Plateau and its environmental changes. Chinese Science Bulletin, 43(15): 1569-1574] [14] 李吉均,方小敏,潘保田,赵志军,宋友桂. 2001. 新生代晚期青藏高原强烈隆起及其对周边环境的影响. 第四纪研究, 21(5): 381-391. [Li J J,Fang X M,Pan B T,Zhao Z J,Song Y G.2001. The evolution of the upper reaches of the Yellow River and the uplift of the Qinghai-Tibet Plateau in the Late Cenozoic. Quaternary Sciences, 21(5): 381-391] [15] 李吉均. 2013. 青藏高原隆升与晚新生代环境变化. 兰州大学学报(自然科学版), 49(2): 5-8. [Li J J.2013. Uplift and Late Cenozoic environmental changes of Qinghai-Tibet Plateau. Journal of Lanzhou University(Natural Sciences), 49(2): 5-8] [16] 李勇,曹叔尤,周荣军,Densmore A L,Ellis M A.2005. 晚新生代岷江下蚀速率及其对青藏高原东缘山脉隆升机制和形成时限的定量约束. 地质学报, 79(1): 29-38. [Li Y,Cao S Y,Zhou R J,Densmore A L,Ellis M A.2005. Late Cenozoic Min jiang incision rate and its constraint on the uplift of the eastern margin of the Tibetan Plateau. Acta Geologica Sinica, 79(1): 29-38] [17] 李勇,周荣军,Densmore A L,Ellis M A.2006. 青藏高原东缘大陆动力学过程与地质响应. 北京: 地质出版社,1-148. [Li Y,Zhou R J,Densmore A L,Ellis M A.2006. The Geology of the Eastern Margin of the Qinghai-Tibet Plateau. Beijing: Geological Publishing House,1-148] [18] 李勇,黎兵,Steffen D,Densmore A L,Richardson N J,周荣军,Ellis M A,张毅. 2006. 青藏高原东缘晚新生代成都盆地物源分析与水系演化. 沉积学报, 24(3): 309-320. [Li Y,Li B,Steffen D,Densmore A L,Richardson N J,Zhou R J,Ellis M A,Zhang Y.2006. Provenance analysis and drainage evolution in Late Cenozoic Chengdu Basin on eastern margin of Tibetan Plateau. Acta Sedimentologica Sinica, 24(3): 309-320] [19] 刘东生,郑绵平,郭正堂. 1998. 亚洲季风系统的起源和发展及其与两极冰盖和区域构造运动的时代耦合性. 第四纪研究,18(3): 194-204. [Liu D S,Zheng M P,Guo Z T.1998. Initiation and evolution of the Asian monsoon system timely coupled with the ice-sheet growth and the tectonic movements in Asia. Quaternary Sciences,18(3): 194-204] [20] 刘勇,赵志军,李才林,张茂桓,陈晔. 2006. 川西高原杂谷脑河阶地的形成. 地理学报, 61(3): 249-254. [Liu Y,Zhao Z J,Li C L,Zhang M H,Chen Y.2006. Formation of the Zagunao River terraces in western Sichuan plateau,China. Acta Geographica Sinica, 61(3): 249-254] [21] 刘志杰,孙永军. 2007. 青藏高原隆升与黄河形成演化. 地理与地理信息科学, 23(1): 79-82,91. [Liu Z J,Sun Y J.2007. Uplift of the Qinghai-Tibet Plateau and formation,evolution of the Yellow River. Geography and Geoinformation Science, 23(1): 79-82,91] [22] 刘树根. 1993. 龙门山造山带与川西前陆盆地形成演化. 四川成都: 成都科技大学出版社,17-117. [Liu S G.1993. The Formation and Evolution of Longmen Shan Thrust Zone and Western Sichuan. Sichuan Chengdu: Press of Chengdu University of Science and Technology,17-117] [23] 马保起,苏刚,侯治华,舒赛兵. 2005. 利用岷江阶地的变形估算龙门山断裂带中段晚第四纪滑动速率. 地震地质, 27(2): 234-242. [Ma B Q,Su G,Hou Z H,Shu S B.2005. Late Quaternary slip rate in the central part of the Longmen Shan fault zone from terrace deformation along the Min Jiang River. Seismology and Geology, 27(2): 234-242] [24] 潘保田,苏怀,刘小丰,胡小飞,周天,胡春生,李吉均. 2007. 兰州东盆地最近1.2 Ma的黄河阶地序列与形成原因. 第四纪研究, 27(2): 172-180. [Pan B T,Su H,Liu X F,Hu X F,Zhou T,Hu C S,Li J J.2007. River terraces of the Yellow River and their genesis in eastern Lanzhou Basin during last 1.2 Ma. Quaternary Sciences, 27(2): 172-180] [25] 潘桂棠,肖庆辉,陆松年,邓晋福,冯益民,张克信,张智勇,王方国,邢光福,郝国杰,冯艳芳. 2009. 中国大地构造单元划分. 中国地质, 36(1): 1-28. [Pan G T,Xiao Q H,Lu S N,Deng J F,Feng Y M,Zhang K X,Zhang Z Y,Wang F G,Xing G F,Hao G J,Feng Y F.2009. Subdivision of tectonic units in China. Geology in China, 36(1): 1-28] [26] 潘裕生. 1999. 青藏高原的形成与隆升. 地学前缘, 6(3): 153-163. [Pan Y S.1999. Formation and uplifting of the Qinghai-Tibet Plateau. Earth Science Frontiers, 6(3): 153-163] [27] 钱洪,马声浩,龚宇. 1995. 关于岷江断裂若干问题的讨论. 中国地震, 11(2): 140-146. [Qian H,Ma S H,Gong Y.1995. Discussions on the Min Jiang fault. Earthquake Research in China, 11(2): 140-146] [28] 钱洪,唐荣昌. 1997. 成都平原的形成与演化. 四川地震,(3): 1-7. [Qian H,Tang R C.1997. On the formation and evolution of the Chengdu Plain. Earthquake Research in Sichuan,(3): 1-7] [29] 任雪梅,杨达源,韩志勇. 2006. 长江上游水系变迁的河流阶地证据. 第四纪研究, 26(3): 115-122. [Ren X M,Yang D Y,Han Z Y.2006. Terrace evidence of river system change in the upper reaches of Chang Jiang River. Quaternary Sciences, 26(3): 115-122] [30] 孙延贵,方洪宾,张琨,赵福岳,刘世英. 2007. 共和盆地层状地貌系统与青藏高原隆升及黄河发育. 中国地质, 34(6): 1141-1147. [Sun Y G,Fang H B,Zhang K,Zhao F Y,Liu S Y.2007. Step-like landform system of the Gonghe basin and the uplift of the Qinghai Tibet Plateau and development of the Yellow River. Geology in China, 34(6): 1141-1147] [31] 施雅风. 1998. 第四纪中期青藏高原冰冻圈的演化及其与全球变化的联系. 冰川冻土, 20(3): 197-208. [Shi Y F.1998. Evolution of the cryosphere in the Tibetan Plateau,China,and its relationship with the global change in the Mid-Quaternary. Journal of Glaciology and Geocryology, 20(3): 197-208] [32] 四川省地质矿产局. 1991. 四川省区域地质志. 北京: 地质出版社,114-160. [Sichuan Bureau of Geology. 1991. Regional Geology in Sichuan Province. Beijing: Geological Publishing House,114-160] [33] 谭锡斌. 2012. 龙门山推覆构造带新生代热演化历史研究及其对青藏高原东缘隆升机制的约束. 中国地震局地质研究所博士学位论文. [Tan X B.2012. Cenozoic Thermal History of the Longmen Shan Thrust Belt: Implication for the Uplift Mechanism in the Eastern Margin of the Tibetean Plateau. Doctoral dissertation of Institute of Geology,China Earthquake Administration] [34] 吴环环. 2017. 黄河共和—贵德段河流阶地演化及其构造意义. 中国地质科学院硕士学位论文,1-73. [Wu H H.2017. The Evolution and Tectonic Meaning of Yellow River Terraces from Gonghe to Guide. Masteral dissertation of Chinese Academy of Geological Sciences,1-73] [35] 王旭光,李传友,吕丽星,董金元. 2017. 龙门山后山断裂中段汶川—茂县断裂的晚第四纪活动性分析. 地震地质, 39(3): 572-586. [Wang X G,Li C Y,Lü L X,Dong J Y.2017. Analysis of the Late Quaternary activity along the Wenchuan-Maoxian Fault—Middle of the back-range fault at the Longmen Shan fault zone. Seismology and Geology, 39(3): 572-586] [36] 向芳,朱利东,王成善,李永昭,杨文光. 2005. 长江三峡阶地的年代对比法及其意义. 成都理工大学学报(自然科学版), 32(2): 162-166. [Xiang F,Zhu L D,Wang C S,Li Y Z,Yang W G.2005. Terrace age correlation and its significance in research of Yangtze Three Gorges,China. Journal of Chengdu University of Technology(Science & Technology Edition), 32(2): 162-166] [37] 许志琴. 1992. 中国松潘—甘孜造山带的造山过程. 北京: 地质出版社,1-64. [Xu Z Q.1992. The Orogenic Process of Songpan-Ganzi Orogenic Belt in China. Beijing: Geological Publishing House,1-64] [38] 许志琴,杨经绥,李海兵,嵇少丞,张泽明,刘焰. 2011. 印度—亚洲碰撞大地构造. 地质学报, 85(1): 1-33. [Xu Z Q,Yang J S,Li H B,Ji S C,Zhang Z M,Liu Y.2011. On the tectonics of the India-Asia collision. Acta Geologica Sinica, 85(1): 1-33] [39] 杨农,张岳桥,孟辉,张会平. 2003. 川西高原岷江上游河流阶地初步研究. 地质力学学报, 9(4): 363-370. [Yang N,Zhang Y Q,Meng H,Zhang H P.2003. Study of the Min Jiang River terraces in the western Sichuan plateau. Journal of Geomechanics, 9(4): 363-370] [40] 杨文光. 2005. 岷江上游阶地沉积记录与气候环境变迁研究. 成都理工大学硕士学位论文,1-85. [Yang W G.2005. Research of Sedimentary Record in Terraces and Climate Vary in the Upper Reaches of Min Jiang River,China. Masteral dissertation of Chengdu University of Technology,1-85] [41] 曾允孚,夏文杰. 1984. 沉积岩石学. 北京: 地质出版社, 1-64. [Zeng Y F,Xia W J.1984. Sedimentary Petrology. Beijing: Geological Publishing House, 1-64] [42] 张会平,杨农,张岳桥,孟晖. 2006. 岷江水系流域地貌特征及其构造指示意义. 第四纪研究, 26(1): 126-135. [Zhang H P,Yang N,Zhang Y Q,Meng H.2006. Geomorphology of the Ming Jiang drainage system(Sichuan,China)and its structural implications. Quaternary Sciences, 26(1): 126-135] [43] 张克信,王国灿,洪汉烈,徐亚东,王岸,曹凯,骆满生,季军良,肖国桥,林晓. 2013. 青藏高原新生代隆升研究现状. 地质通报, 32(1): 3-20. [Zhang K X,Wang G C,Hong H L,Xu Y D,Wang A,Cao K,Luo M S,Ji J L,Xiao G Q,Lin X.2013. The study of the Cenozoic uplift in the Tibetan Plateau: A review. Geological Bulletin of China, 32(1): 3-20] [44] 张建,胡小飞,耿豪鹏,陈殿宝,潘保田. 2016. 钻孔及现代河流重矿物特征揭示的更新世以来酒东盆地水系演化历史. 地理科学, 36(10): 1595-1604. [Zhang J,Hu X F,Geng H P,Chen D B,Pan B T.2016. Drainage evolution history in Jiudong basin since the Pleistocene inferred from heavy mineral characteristics in cores and modern fluvial deposits. Scientia Geographica Sinica, 36(10): 1595-1604] [45] 张俊宇. 2018. 大渡河中下游河流阶地序列及其对山体隆升的响应. 辽宁师范大学硕士学位论文,1-85. [Zhang J Y.2018. River Terrace Sequence of the Middle and Lower Reaches of Da Du River and Its Response to Mountain Uplift. Masteral dissertation of Liaoning Normal University,1-85] [46] 赵红格,刘池洋. 2003. 物源分析方法及研究进展. 沉积学报, 21(3): 409-415. [Zhao H G,Liu C Y.2003. Approaches and prospects of provenance analysis. Acta Sedimentologica Sinica, 21(3): 409-415] [47] 赵小麟,邓起东,陈社发. 1994. 岷山隆起的构造地貌学研究. 地震地质, 16(4): 429-439. [Zhao X L,Deng Q D,Chen S F.1994. Tectonic geomorphology of the Min Shan uplift in western Sichuan,southwestern China. Seismology and Geology, 16(4): 429-439] [48] 郑勇,孔屏. 2013. 四川盆地西缘晚新生代大邑砾岩的物源及其成因: 来自重矿物和孢粉的证据. 岩石学报, 29(8): 2949-2958. [Zheng Y,Kong P.2013. Provenance and origin of the Late Cenozoic Dayi conglomerates in the western margin of the Sichuan Basin: New insights from heavy mineral and spore-pollen assemblages. Acta Petrologica Sinica, 29(8): 2949-2958] [49] 朱俊霖. 2014. 岷江上游地区阶地初步研究. 成都理工大学硕士学位论文. [Zhu J L.2014. A Preliminary Study on the Upper Reaches of Min Jiang River Terrace. Masteral dissertation of Chengdu University of Technology] [50] 周荣军,蒲晓虹,何玉林,黎小刚,戈天勇. 2000. 四川岷江断裂带北段的新活动、岷山断块的隆起及其与地震活动的关系. 地震地质, 22(3): 285-294. [Zhou R J,Pu X H,He Y L,Li X G,Ge T Y.2000. Study of the Min Jiang River Terraces in the western Sichuan plateau. Seismology and Geology, 22(3): 285-294] [51] Arnaud N O,Brunel M,Cantagrel J M,Tapponnier P.1993. High cooling and denudation rates at Kongur Shan,Eastern Pamir(Xinjiang,China)revealed by 40Ar/39Ar Aralkali feldspar thermochronology. Tectonics, 12(6): 1335-1346. [52] Burbank,Pinter.1999. Landscape evolution: The interactions of tectonics and surface processes. Basin Research, 11(1): 1-6. [53] Chang E Z.2000. Geology and tectonics of the Songpan-Ganzi Fold Belt,southwestern China. International Geology Review, 42(9): 813-831. [54] Fang X M,Zhang W L,Meng Q Q,Gao J P,Wang X M,King J,Song C H,Dai S,Miao Y F.2007. High-resolution magnetostratigraphy of the Neogene Huaitoutala section in the eastern Qaidam Basin on the NE Tibetan Plateau,Qinghai Province,China and its implication on tectonic uplift of the NE Tibetan Plateau. Earth and Planetary Science Letters, 258: 293-306. [55] Harrison T M,Copeland P,Kidd W S F,Yin A.1992. Raising Tibet. Science, 255: 1663-1670. [56] Kirby E,Whipple K X,Burchfiel B C,Tang W Q,Berger G,Sun Z M,Chen Z L.2000. Neotectonics of the Min Shan,China: Implications for mechanisms driving Quaternary deformation along the eastern margin of the Tibetan Plateau. Geological Society of America Bulletin, 112(3): 375-393. [57] Kirby E,Reiners P W,Krol M A,Whipple K X,Hodges K V,Farley K A,Tang W Q,Chen Z L.2002. Late Cenozoic evolution of the eastern margin of the Tibetan Plateau: Inferences from 40Ar/39Ar and(U-Th)/He thermochronology. Tectonics, 21(1): 1-19. [58] Li J J,Fang X M,Song C H,Pan B T,Ma Y Z,Yan M D.2014. Late Miocene-Quaternary rapid stepwise uplift of the NE Tibetan Plateau and its effects on climatic and environmental changes. Quaternary Research, 81(3): 400-423. [59] Li Y,Allen P A,Densmore A L,Xu Q.2003. Evolution of the Longmen Shan foreland Basin(western Sichuan,China)during the Late Triassic Indosinian orogeny. Basin Research, 15(3): 117-138. [60] Liu C R,Yin G M,Zhang H P,Zheng W J,Voinchet P,Han F,Wang D,Song W J,Bahain J J.2013. ESR geochronology of the Min Jiang River terraces at Wenchuan,eastern margin of Tibetan Plateau,China. Geochronometria, 40(4): 360-367. [61] Morton A C.1985. Heavy minerals in provenance studies. In: Zuffa G G(ed). Provenance of Arenites. Dordrecht: Springer. [62] Morton A C,Smale D.1990. The effects of transport and weathering on heavy minerals from the Cascade River,New Zealand. Sedimentary Geology, 68(1): 117-123. [63] Morton A C,Hallsworth C R.1999. Processes controlling the composition of heavy mineral assemblages in sandstones. Sedimentary Geology, 124(1-4): 3-29. [64] Roser B P,Korsch R J.1985. Plate tectonics and geochemical composition of sandstones: A discussion. Journal of Geology, 93(1): 81-84. [65] Weltje G J,Eynatten H V.2004. Quantitative provenance analysis of sediments: Review and outlook. Sedimentary Geology, 171(1): 1-11. [66] Xie S C,Pancost R D,Chen L,Evershed R P,Yang H,Zhang K X,Huang J H,Xu Y D.2012. Microbial lipid records of highly alkaline deposits and enhanced aridity associated with significant uplift of the Tibetan Plateau in the Late Miocene. Geology, 40(4): 291-294.
