Kinematics of the Greater Himalayan sequence, Dhaulagiri Himal ...

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755 756 Acknowledgments 757 758 759 760 761 762 763 764 This research was supported through a Natural Science and Engineering Research Council of Canada Discovery grant to L. Godin and Canada Graduate Scholarship to K. Larson. Discussion in the field with Dawn Kellett helped elucidate the geologic complexities of the map area. The Late Pasang Tamang, Nurbu Tamang, Pardap Tamang, Lakpa Tamang, Ngima Tamang, and Mangale Sherestsa are thanked for logistic support. S.T. Johnston and R.A. Price helped improve early versions of this paper. Reviews by M.P. Searle, R.D. Law, A.J. Martin, and an anonymous reviewer enhanced the final version of this manuscript. N. Portelance performed copy-editing of the manuscript. 36
765 766 References 767 768 769 770 771 772 773 774 775 776 777 778 779 780 781 782 783 784 785 786 787 788 789 790 791 792 793 794 795 796 Ahmad, T., Harris, N., Bickle, M., Chapman, H., Bunbury, J. & Prince C. 2000. Isotopic constraints on the structural relationships between Lesser Himalayan series and High Himalayan crystalline series, Garhwal Himalaya. Tectonophysics, 112, 467-477. Arita, K. 1983. Origin of the inverted metamorphism of the lower Himalayas, central Nepal. Tectonophysics, 95, 43-60. Bailey, C.M., Francis, B.E. & Fahrney, E.E. 2004. Strain and vorticity analysis of transpressional high-strain zones from the Virginia Piedmont, USA. In: Alsop, G.I., Holdsworth, R.E., McCaffrey, K.J.W. et als (eds) Flow processes in faults and shear zones. Geological Society, London, Special Publications, 224, 249-264. Beaumont, C., Jamieson, R.A., Nguyen, M.H. & Lee, B. 2001. Himalayan tectonics explained by extrusion of a low-viscosity crustal channel coupled to focused surface denudation. Nature, 414, 738-742. Beaumont, C., Jamieson, R.A., Nguyen, M.H. & Medvedev, S. 2004. Crustal channel flows: 1. Numerical models with applications to the tectonics of the Himalayan- Tibetan orogen. Journal of Geophysical Research, 109, 10.1029/2003JB002809. Beaumont, C., Nguyen, M.H., Jamieson, R.A. & Ellis, S. 2006. Crustal flow modes in large hot orogens. In: Law, R.D., Searle, M.P. & Godin, L. (eds) Channel flow, ductile extrusion and exhumation in continental collisional zones. Geological Society, London, Special Publications, 268, 91-146. Bhattacharya, A.R. & Weber, K. 2004. Fabric development during shear deformation in the Main Central Thrust Zone, NW-Himalaya, India. Tectonophysics, 387, 23-46. Bodenhausen, J.W.A. & Egeler, C.G. 1971. On the geology of the upper Kali Gandaki valley, Nepalese Himalayas, I. Proceedings Akademic Van Wetenschappen, 74, 526- 538. Bollinger, L. & Janots, E. 2006. Evidence for Mio-Pliocene retrograde monazite in the Lesser Himalaya, far western Nepal. European Journal of Mineralogy, 18, 289-297. Bollinger, L., Henry, P. & Avouac, J.P-. 2006. Mountain building in the Nepal Himalaya: Thermal and kinematic model. Earth and Planetary Science Letters, 244, 58-71. Bordet, P. 1961. Recherches géologiques dans l'Himalaya du Népal, région du Makalu. C.N.R.S. 37
Page 1 and 2: 1 2 3 4 5 Kinematics of the Greater
Page 3 and 4: 39 1. Introduction 40 41 42 43 44 4
Page 5 and 6: 84 85 86 87 88 provide new insight
Page 7 and 8: 129 130 131 132 133 134 135 The Dha
Page 9 and 10: 173 3.3 Greater Himalayan sequence
Page 11 and 12: 218 219 220 221 222 8 cm apart. In
Page 13 and 14: 263 quartzite and, locally, more im
Page 15 and 16: 307 308 309 310 311 312 In this stu
Page 17 and 18: 352 4.1 Quartz petrofabric analysis
Page 19 and 20: 398 399 400 401 402 403 404 405 406
Page 21 and 22: 443 444 445 446 447 448 449 maximum
Page 23 and 24: 488 489 490 491 492 the X-Z plane o
Page 25 and 26: 534 535 through the following equat
Page 27 and 28: 572 573 574 575 576 577 578 579 val
Page 29 and 30: 617 618 619 620 621 622 623 624 625
Page 31 and 32: 663 6.3 Flow kinematics 664 665 666
Page 33 and 34: 709 710 711 712 713 714 715 716 717
Page 35: 753 754 better understand the proce
Page 39 and 40: 830 831 832 833 834 835 836 837 838
Page 41 and 42: 900 901 902 903 904 905 906 907 908
Page 43 and 44: 970 971 972 973 974 975 976 977 978
Page 45 and 46: 1039 1040 1041 1042 1043 1044 1045
Page 47 and 48: 1107 1108 1109 1110 1111 1112 1113
Page 49 and 50: 1163 1164 1165 1166 1167 a leucogra
Page 51 and 52: 1205 1206 1207 1208 1209 plotted ag
Page 53 and 54: 1247 1248 1249 1250 1251 1252 1253
Page 55 and 56: 83˚ 30'E South Tibetan Detachment
Page 57 and 58: A Previous Studies (Central Nepal)
Page 59 and 60: SW NE NW SE A B W E W E C D
Page 61 and 62: 018 015 grain shape foliation 038 2
Page 63 and 64: SW A S Qtz C Qtz Ep Am Am Am Ms 200
Page 65 and 66: 10 percent pure shear 80 70 60 50 4
Page 67: (A) percent pure shear 60 50 40 30

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