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青藏高原新生代构造隆升阶段的时空格局

, PP. 332-349

Keywords: 青藏高原,新生代,强构造隆升剥露阶段,高原扩展

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Abstract:

?青藏高原不同部位低温热年代学记录、沉积记录和构造变形记录揭示出存在60~35,25~17,12~8Ma(藏南17~12Ma)和大约5Ma以来4个主要强构造隆升剥露阶段.除了藏南地区在17~12Ma发生藏南拆离系的活动及其所控制的高喜马拉雅结晶基底岩系的快速抬升剥露这一特殊情况外,青藏高原不同地区主要强构造隆升剥露阶段具有准同时性.几个强隆升剥露阶段对应于几个强构造变形活动时期,反映隆升剥露主要受构造动力控制.新生代以砾岩为代表的粗碎屑物的分布、前陆盆地或走滑拉分盆地的分布及其沉积充填、角度不整合的发育和地层间断缺失,以及受断裂控制的盆山地貌变迁和高原扩展与青藏高原几个强构造抬升剥露阶段也具有良好的匹配关系.本文还讨论了青藏高原作为地表隆升的高原形成过程,揭示高原的形成是随时间演变不断扩展的过程.

References

[1]  3 王军. 西昆仑卡日巴生岩体和苦子干岩体的隆升—来自磷灰石裂变径迹分析的证据. 地质论评, 1998, 44: 435–442
[2]  4 王彦斌, 王永, 刘训, 等. 天山、西昆仑山中、新生代幕式活动的磷灰石裂变径迹纪录. 中国区域地质, 2001, 20: 94–99
[3]  5 黎敦朋, 赵越, 胡建民, 等. 青藏高原西北缘高原面与陡坡地貌形成过程的裂变径迹年代学约束. 岩石学报, 2007, 23: 900–910
[4]  6 万景林, 王二七. 西昆仑北部山前普鲁地区山体抬升的裂变径迹研究. 核技术, 2002, 25: 565–567
[5]  7 Robinson A C, Yin A, Manning C E, et al. Tectonic evolution of the northeastern Pamir: Constraints from the northern portion of theCenozoic Kongur Shan extensional system, western China. Geol Soc Am Bull, 2004, 116: 953–973??
[6]  8 许志琴, 戚学祥, 杨经绥, 等. 西昆仑康西瓦韧性走滑剪切带的两类剪切指向、形成时限及其构造意义. 地质通报, 2007, 26:1252–1261
[7]  9 Yin A, Rumelhart P E, Butler R. Tectonic history of the Altyn Tagh fault system in northern Tibet inferred from Cenozoic sedimentation.Geol Soc Am Bull, 2002, 114: 1257–1295??
[8]  10 邵龙义, 何志平, 顾家裕, 等. 塔里木盆地古近纪岩相古地理. 古地理学报, 2006, 8: 353–364
[9]  28 郑德文, 张培震, 万景林, 等. 青藏高原东北边缘晚新生代构造变形的时序—临夏盆地碎屑颗粒磷灰石裂变径迹记录. 中国科学D 辑: 地球科学, 2003, 33(增刊): 190–198
[10]  29 方小敏, 宋春晖, 戴霜, 等. 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, 2007, 14:230–242
[11]  30 张培震, 郑德文, 尹功明, 等. 有关青藏高原东北缘晚新生代扩展与隆升的讨论. 第四纪研究, 2006, 26: 5–13
[12]  31 袁道阳, 张培震, 方小敏, 等. 青藏高原东北缘临夏盆地晚新生代构造变形及过程. 地学前缘, 2007, 14: 243–250
[13]  32 宋春晖, 方小敏, 李吉均, 等. 青藏高原北缘酒西盆地13 Ma 以来沉积演化与高原隆升. 中国科学D 辑: 地球科学, 2001, 31(增刊):155–162
[14]  33 尹安, 党玉琪, 陈宣华, 等. 柴达木盆地新生代演化及其构造重建—基于地震剖面的解释. 地质力学学报, 2007, 113: 193–211
[15]  34 钟大赉, 丁林. 青藏高原的隆起过程及其机制探讨. 中国科学D 辑: 地球科学, 1996, 26: 289–295
[16]  35 来庆洲, 丁林, 王宏伟, 等. 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, 2006, 36:785–796
[17]  36 Clark M K, House M A, Royden L H, et al. Late Cenozoic uplift of southeastern Tibet. Geology, 2005, 33: 525–528??
[18]  37 张毅, 李勇, 周荣军, 等. 晚新生代以来青藏高原东缘的剥蚀过程: 来自裂变径迹的证据. 沉积与特提斯地质, 2006, 26: 97–102
[19]  38 丁林, 钟大赉, 潘裕生, 等. 东喜马拉雅构造结上新世以来快速抬升的裂变径迹证据. 科学通报, 1995, 40: 1479–1500
[20]  39 王刚, 万景林, 王二七, 等. 高黎贡山脉南部的晚新生代构造—重力垮塌及其成因. 地质学报, 2006, 80: 1262–1273
[21]  40 雷永良, 季建清, 龚道好, 等. 滇西北独龙江岩体晚中新世以来的热史和剥蚀历史的磷灰石裂变径迹记录. 岩石学报, 2006, 22:938–948
[22]  1 Arnaud N O, Brunel M, Cantagrel J M, et al. High cooling and denudation rates at Kongur Shan, eastern Pamir (Xinjiang, China) revealedby 40Ar/39Ar alkali feldspar thermochronology. Tectonics, 1993, 12: 1335–1346
[23]  2 Wang E Q, Wan J L, Liu J. Late Cenozoic geological evolution of the foreland basin bordering the west Kunlun range in Pulu Area:Constrain on timing of uplift of northern margin of the Tibet Plateau. J Geophys Res, 2003, 108: 1–15
[24]  11 Brunel M, Arnaud N, Tapponnier P, et al. Kongur Shan normal fault: Type example of mountain building assisted by extension (Karakoramfault, eastern Pamir). Geology, 2004, 22: 707–710
[25]  12 Jin X C, Wang J, Chen B W, et al. Cenozoic depositional sequences in the piedmont of the west Kunlun and their paleogeographic andtectonic implications. J Asian Earth Sci, 2003, 21: 755–765??
[26]  13 陈杰, 卢演俦, 丁国瑜. 塔里木西缘晚新生代造山过程的记录—磨拉石建造及生长地层和生长不整合. 第四纪研究, 2001, 21:528–539
[27]  14 潘燕兵, 黎敦朋, 郭芳芳, 等. 克里雅河河谷地貌与塔里木盆地早-中更新世大湖环境. 地质通报, 2008, 27: 814–822
[28]  15 Zheng H B, Powell C M, An Z S, et al. Pliocene uplift of the northern Tibetan Plateau. Geology, 2000, 28: 715–718??
[29]  16 柏道远, 孟德保, 刘耀荣, 等. 青藏高原北缘昆仑山中段构造隆升的磷灰石裂变径迹记录. 中国地质, 2003, 30: 240–246
[30]  17 拜永山, 任二峰, 范桂兰, 等. 青藏高原西北缘祁漫塔格山中新世快速抬升的磷灰石裂变径迹证据. 地质通报, 2008, 27: 1044–1048
[31]  18 陈正乐, 宫红良, 李丽, 等. 阿尔金山脉新生代隆升-剥露过程. 地学前缘, 2006, 13: 91–102
[32]  19 陈正乐, 万景林, 王小凤, 等. 阿尔金断裂带8 Ma 左右的快速走滑及其地质意义. 地球学报, 2002, 23: 295–300
[33]  20 陈正乐, 张岳桥, 王小凤, 等. 新生代阿尔金山脉隆升历史的裂变径迹证据. 地球学报, 2001, 22: 413–418
[34]  21 万景林, 王瑜, 李齐, 等. 阿尔金山北段晚新生代山体抬升的裂变径迹证据. 矿物岩石地球化学通报, 2001, 20: 222–224
[35]  22 王瑜, 万景林, 李齐, 等. 阿尔金山北段阿克塞-当金山口一带新生代山体抬升和剥蚀的裂变径迹证据. 地质学报, 2002, 76: 191–198
[36]  23 Sobel E R, Arnaud N, Jolivet M, et al. Jurassic to Cenozoic exhumation history of the Altyn Tagh range, NW China, constrained by40Ar/39Ar and apatite fission track thermochronology. In: Hendrix M S, Davis G R, eds. Paleozoic and Mesozoic Tectonic Evolution ofCentral Asia, from Continental Assembly to Intracontinental Deformation. Geol Soc Am Mem, 2001, 194: 247–267
[37]  24 Yuan W M, Dong J Q, Wang S C, et al. Apatite fission track evidence for Neogene uplift in the eastern Kunlun Mountains, northernQinghai-Tibet Plateau, China. J Asian Earth Sci, 2006, 27: 847–856??
[38]  25 Jolivet M, Brunel M, Seward D, et al. Mesozoic and Cenozoic tectonics of the northern edge of the Tibetan Plateau: Fission trackconstraints. Tectonophysics, 2001, 343: 111–134??
[39]  26 王国灿, 向树元, Garver J I, 等. 东昆仑东段哈拉郭勒-哈图一带中生代的岩石隆升剥露—锆石和磷灰石裂变径迹年代学证据. 地球科学—中国地质大学学报, 2003, 28: 645–652
[40]  27 王岸, 王国灿, 谢德凡, 等. 东昆仑山小南川岩体裂变径迹年代与中新世晚期以来的构造地貌演化. 地球科学——中国地质大学学报, 2007, 32: 51–58
[41]  44 张岳桥, 陈文, 杨农. 川西鲜水河断裂带晚新生代剪切变形40Ar/39Ar 测年及其构造意义. 中国科学D 辑: 地球科学, 2004, 34:613–621
[42]  41 向宏发, 万景林, 韩竹军, 等. 红河断裂带大型右旋走滑运动发生时代的地质分析与FT 测年. 中国科学D 辑: 地球科学, 2006, 36:977–987
[43]  42 施小斌, 丘学林, 刘海龄, 等. 滇西临沧花岗岩基新生代剥蚀冷却的裂变径迹证据. 地球物理学报, 2006, 49: 135–142
[44]  43 张进江, 季建清, 钟大赉, 等. 东喜马拉雅南迦巴瓦构造结的构造格局及形成过程探讨. 中国科学D 辑: 地球科学, 2003, 33:373–383
[45]  45 李勇, 周荣军, Densemmore A L, 等. 龙门山断裂带走滑方向的反转及其沉积与地貌标志. 矿物岩石, 2006, 26: 26–34
[46]  46 王宗秀, 许志琴, 杨天南, 等. 川西鲜水河断裂带变形机制研究—一个浅层次高温韧性移剪切带. 中国区域地质, 1996, 3:244–251
[47]  47 王瑜, 万景林, 李大明, 等. 藏南伸展拆离系聂拉木一带构造抬升的热年代学证据. 矿物岩石地球化学通报, 2001, 20: 292–294
[48]  48 Burbank D W, Blythe A E, Putkonen J, et al. Decoupling of erosion and precipitation in the Himalayas. Nature, 2003, 426: 652–655??
[49]  49 Bojar A V, Fritz H, Nicolescu S. Timing and mechanisms of central Himalayan exhumation: Discriminating between tectonic and erosionprocesses. Terra Nova, 2005, 17: 427–433??
[50]  50 Burg J P, Nievergelt P, Oberli F, et al. Erosion of crustal folds in the Himalayan syntaxes. Terra Nostra (Bonn), 1998, 98-1: 5
[51]  51 Lee J, Hacker B R, Dingklage W S, et al. Evolution of Kangmar Dome, southern Tibet: Structural, petrologic, and thermochronologicconstraints. Tectonics, 2000, 19: 872–895??
[52]  52 Searle M P, Parrish R R, Hodges K V, et al. Shisha Pangma leucogranite, South Tibetan Himalaya: Field relations, geochemistry, age,origin, and emplacement. J Geol, 1997, 105: 295–317??
[53]  53 Schlup M, Carter A, Cosca M, et al. Exhumation history of eastern Ladakh revealed by 40Ar/39Ar and fission track ages: The Indus River-Tso Morari transect, NW Himalaya. J Geol Soc, 2003, 160: 385–399??
[54]  54 Sorkhabi R B, Stump E, Foland K A, et al. Fission-track and 40Ar/39Ar evidence for episodic denudation of the Gangotri granites in theGarhwal Higher Himalaya, India. Tectonophysics, 1996, 260: 187–199??
[55]  55 Thiede R C, Bookhagen B J, Arrowsmith R, et al. Climatic control on rapid exhumation along the southern Himalayan Front. Earth PlanetSci Lett, 2004, 222: 791–806??
[56]  56 Zeitler P K. Cooling history of the NW Himalaya, Pakistan. Tectonics, 1985, 4: 127–151??
[57]  57 王二七, 陈良忠, 陈智. 在构造和气候因素制约下的雅鲁藏布江的演化. 第四纪研究, 2002, 22: 365–373
[58]  58 丁林. 西藏雅鲁藏布江缝合带古新世深水沉积和放射虫动物群的发现及对前陆盆地演化的制约. 中国科学D 辑: 地球科学, 2003,33: 47–58
[59]  59 李国彪, 万晓樵, 其和日格, 等. 藏南岗巴-定日地区始新世化石碳酸盐岩微相与沉积环境. 中国地质, 2002, 29: 401–406
[60]  60 万晓樵. 西藏白垩纪-早第三纪有孔虫与特提斯-喜马拉雅海的演化. 微体古生物学报, 1990, 7: 169–186
[61]  61 赵政璋, 李永铁, 叶和飞, 等. 青藏高原地层. 北京: 科学出版社, 2001. 1–542
[62]  62 张克信, 王国灿, 曹凯, 等. 青藏高原新生代主要隆升事件: 沉积响应与热年代学记录. 中国科学D 辑: 地球科学, 2008, 38:1575–1588
[63]  63 Coleman M E, Hodges K V. Evidence for Tibetan plateau uplift before 14 Myr ago from a new minimum age for east west extension.Nature, 1995, 374: 49–52??
[64]  64 Coleman M E. U-Pb constraints on Oligocene-Miocene deformation and anatexis within the central Himalaya, Marsyandi valley, Nepal.Am J Sci, 1998, 298: 553–571??
[65]  65 Harris N. Significance of weathering Himalayan metasedimentary rocks and leucogranites for the Sr isotope evolution of sea water duringearly Miocene. Geology, 1995, 23: 759–798??
[66]  66 Parrish R R, Hodges K V. Miocene (22±1 Ma) metamorphism and two stage thrusting in the Greater Himalayan sequence, AnnapurnaSanctuary, Nepal. Geol Soc Am Abstr Program, 1993, 25: 174
[67]  67 潘桂棠, 王培生, 徐耀荣, 等. 青藏高原新生代构造演化. 北京: 地质出版社, 1990. 1–165
[68]  68 Harrison T M, Copeland P, Kidd W S, et al. Raising Tibet. Science, 1992, 255: 1663–1670??
[69]  69 Yin A, Harrison T M, Ryerson F J, et al. Tertiary structural evolution of the Gangdese thrust system, southeastern Tibet. J Geophys Res,1994, 99: 18175–18201??
[70]  70 李海兵, Valli F, 刘敦一, 等. 喀喇昆仑断裂的形成时代: 锆石SHRIMP U-Pb 年龄的制约. 科学通报, 2007, 52: 438–447
[71]  71 Searle M P, Godin L. The South Tibetan Detachment and the Manaslu leucogranite: A structural reinterpretation and restoration of theAnnapurna-Manaslu Himalaya, Nepal. J Geol, 2003, 111: 505–523??
[72]  72 Burchfiel B C, Chen Z L, Hodges K V, et al. The South Tibet Detachment System, Himalayan orogen: Extension contemporaneous withand parallel to shortening in a collisional mountain belt. Spec Pap Geol Soc Am, 1992, 269: 1–41
[73]  73 Hodges K V, Bowring S, Davidek K, et al. Evidence for rapid displacement on Himalayan normal faults and the importance of tectonicdenudation in the evolution of mountain ranges. Geology, 1998, 26: 483–486??
[74]  74 Harrison T M, Copeland P, Kidd W, et al. Activation of the Nyainqentanghla shear zone: Implications for uplift of the southern TibetanPlateau. Tectonics, 1995, 14: 658–676??
[75]  75 刘文灿, 王瑜, 张详信, 等. 西藏南部康马岩体岩石类型及其同位素测年. 地学前缘, 2004, 11: 491–501
[76]  76 Thiede R C, Arrowsmith R, Bookhagen B J, et al. Dome formation and extension in the Tethyan Himalaya, Leo Pargil, northwest India.Geol Soc Am Bull, 2006, 118: 635–650??
[77]  112 魏启荣, 李德威, 王国灿, 等. 青藏高原北部查保马组火山岩的锆石SHRIMP U-Pb 定年和地球化学特点及其成因意义. 岩石学报,2007, 23: 2727–2736
[78]  113 李吉均, 方小敏, 潘宝田, 等. 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, 2001, 21: 381–391
[79]  114 李吉均, 方小敏. 青藏高原隆起与环境变化研究. 科学通报, 1998, 43: 1569–1574
[80]  115 施雅风, 李吉均, 李炳元, 等. 晚新生代青藏高原的隆升与东亚环境变化. 地理学报, 1999, 54: l0–2l
[81]  116 崔之久, 高全洲, 刘耕年, 等. 夷平面、古岩溶与青藏高原隆升. 中国科学D 辑: 地球科学, 1996, 26: 378–386
[82]  117 崔之久, 伍永秋, 刘耕年, 等. 关于“昆仑-黄河运动”. 中国科学D 辑: 地球科学, 1998, 28: 53–59
[83]  77 Thiede R C, Arrowsmith R, Bookhagen B J, et al. From tectonically to erosionally controlled development of the Himalayan orogen.Geology, 2005, 33: 689–692??
[84]  78 Vannay J C, Grasemann B, Rahn M, et al. Miocene to Holocene exhumation of metamorphic crustal wedges in the Himalayan orogen:Evidence for tectonic extrusion coupled to fluvial erosion. Tectonics, 2004, 23: 1–24
[85]  79 Godin L, Parrish R R, Brown R L, et al. Crustal thickening leading to exhumation of the Himalayan metamorphic core of central Nepal:Insight from U-Pb geochronology and 40Ar/39Ar thermochronology. Tectonics, 2001, 20: 729–747??
[86]  80 袁万明, 王世成, 杨志强, 等. 北喜马拉雅带构造活动的裂变径迹定年证据. 核技术, 2002, 25: 451–454
[87]  81 刘顺生, 张峰. 西藏南部地区的裂变径迹年龄和上升速率的研究. 中国科学B 辑, 1987, 17: 1000–1010
[88]  82 袁万明, 王世成, 李胜荣, 等. 西藏冈底斯带构造活动的裂变径迹证据. 科学通报, 2001, 46: 1739–1742
[89]  83 袁万明, 杜杨松, 杨立强, 等. 西藏冈底斯带南木林地区构造活动的磷灰石裂变径迹分析. 岩石学报, 2007, 23: 2911–2917
[90]  84 袁万明, 董金泉, 保增宽, 等. 西藏冈底斯地块尼木地区新第三纪构造热史的磷灰石裂变径迹约束. 原子能科学技术, 2008, 42:570–573
[91]  85 Wang Y, Zhang X M, Sun L X, et al. Cooling history and tectonic exhumation stages of the south-central Tibetan Plateau (China):Constrained by 40Ar/39Ar and apatite fission-track thermochronology (in 19th Himalaya-Karakoram-Tibet workshop). J Asian Earth Sci,2007, 29: 266–282??
[92]  86 吴珍汉, 胡道功, 刘琦胜, 等. 念青唐古拉花岗岩热演化历史和山脉隆升过程的热年代学分析. 地球学报, 2005, 26: 505–512
[93]  87 吴珍汉, 孟宪刚, 胡道功, 等. 当雄县幅地质调查新成果及主要进展. 地质通报, 2004, 23: 484–491
[94]  88 Wang C S, Zhao X X, Liu Z F, et al. Constraints on the early uplift history of the Tibetan Plateau. Proc Nat Acad Sci, 2008, 105:4987–4992??
[95]  89 张克信, 王国灿, 陈奋宁, 等. 青藏高原古近纪-新近纪隆升与沉积盆地分布耦合. 地球科学—中国地质大学学报, 2007, 32:583–597
[96]  90 钱定宇. 论秋乌煤系及拉达克至冈底斯陆缘山链磨拉石的时代. 青藏高原地质文集, 1985, 16: 229–241
[97]  91 肖劲东. 西藏阿里地区早第三纪欧利组及六射珊瑚. 青藏高原地质文集, 1988, 19: 120–131
[98]  92 章炳高, 穆西南. 西藏雅鲁藏布江以北海相第三系的发现. 地层学杂志, 1979, 3: 65–66
[99]  93 Copeland P, Harrison T M, Pan Y, et al. Thermal evolution of the Gangdese Batholith, southern Tibet: A history of episodic unroofing.Tectonics, 1995, 14: 223–236??
[100]  94 Grujic D, Coutand I, Bookhagen B, et al. Climate forcing of erosion, landscape, and tectonics in the Bhutan Himalayas. Geology, 2006, 34:801–804??
[101]  95 Burbank D W, Derry L A, France-Lanord C. Reduced Himalayan sediment production 8 Myr ago despite an intensified monsoon. Nature,1993, 364: 48–50??
[102]  96 Tapponnier P, Xu Z Q, Roger F, et al. Oblique stepwise rise and growth of the Tibet Plateau. Science, 2001, 294: 1671-1677??
[103]  97 Zhang P Z, Shen Z K, Wang M, et al. Continuous deformation of the Tibetan Plateau from global positioning system data. Geology, 2004,32: 809–812??
[104]  98 李海兵, 杨经绥, 许志琴, 等. 阿尔金断裂带的形成时代—来自于同构造生长锆石U-Pb SHRIMP 定年证据. 地质论评, 2001, (3):316–317
[105]  99 李海兵, 杨经绥. 青藏高原北部白垩纪隆升的证据. 地学前缘, 2004, 11: 345–359
[106]  100 Burchfiel B C, Chen Z L, Liu Y P, et al. Tectonics of the Longmen Shan and adjacent regions, central China. Int Geol Rev, 1995, 37:661–735??
[107]  101 Chen S F, Wilson C J L. Emplacement of the Longmen Shan thrust-nappe belt along the eastern margin of the Tibetan Plateau. J StructGeol, 1996, 18: 413–430
[108]  102 Liu Y J, Genser J, Neubauer F, et al. 40Ar/39Ar mineral ages from basement rocks in the eastern Kunlun Mountains, NW China, and theirtectonic implications. Tectonophysics, 2005, 398: 199–224??
[109]  103 王国灿, 向树元, 王岸, 等. 东昆仑及相邻地区中生代-新生代早期构造过程的热年代学记录. 地球科学—中国地质大学学报,2007, 32: 605–614
[110]  104 戴霜, 方小敏, 宋春晖, 等. 青藏高原北部的早期隆升. 科学通报, 2005, 50: 673–683
[111]  105 Rowley D B, Currie B S. Paleo-altimetry of the late Eocene to Miocene Lunpola basin, central Tibet, Nature, 2006, 439: 677–681
[112]  106 DeCelles P G, Quade J, Kapp P, et al. High and dry in central Tibet during the late Oligocene. Earth Planet Sci Lett, 2007, 253: 389–401??
[113]  107 Spicer R A, Harris N B W, Widdowson M, et al. Constant elevation of southern Tibet over the past 15 million years. Nature, 2003, 421:622–624??
[114]  108 Currie B S, Rowley D B, Tabor N J. Middle Miocene paleoaltimetry of southern Tibet: Implications for the role of mantle thickening anddelamination in the Himalayan orogen. Geology, 2005, 33: 181–184??
[115]  109 Garzione C N, DeCelles P G, Hodkinson D G, et al. East-west extension and Miocene environmental change in the southern Tibetanplateau: Thakkhola graben, central Nepal. Geol Soc Am Bull, 2003, 115: 3–20??
[116]  110 Garzione C N, Dettman D L, Quade J, et al. High times on the Tibetan plateau: Paleoelevation of the Thakkhola graben, Nepal. Geology,2000, 28: 339–342??
[117]  111 Garzione C N, Quade J, DeCelles P G, et al. Predicting paleoelevation of Tibet and the Himalaya from δ18O vs. altitude gradients inmeteoric water across the Nepal Himalaya. Earth Planet Sci Lett, 2000, 183: 215–229??

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