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

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1004 1005 1006 1007 1008 1009 1010 1011 1012 1013 1014 1015 1016 1017 1018 1019 1020 1021 1022 1023 1024 1025 1026 1027 1028 1029 1030 1031 1032 1033 1034 1035 1036 1037 1038 Lister, G.S. & Dornsiepen, U.F. 1982. Fabric transitions in the Saxony granulite terrain. Journal of Structural Geology, 4, 81-93. Macfarlane, A.M. 1995. An evaluation of the inverted metamorphic gradient at Langtang National Park, Central Nepal Himalaya. Journal of Metamorphic Geology, 13, 595- 612. Martin, A.J., DeCelles, P.G., Gehrels, G.E., Patchett, P.J. & Isachsen, C. 2005. Isotopic and structural constraints on the location of the Main Central thrust in the Annapurna Range, central Nepal Himalaya. Geological Society of America Bulletin, 117, 926- 944. Martin, A.J., Gehrels, G.E., DeCelles & P.G. 2007. The tectonic significance of (U,Th)/Pb ages of monazite inclusions in garnet from the Himalaya of central Nepal. Chemical Geology, 244, 1-24, doi: 10.1016/j.chemgeo.2007.05.003. Nazarchuk, J.H. 1993. Structure and geochronology of the Greater Himalaya, Kali Gandaki region, west-central Nepal. MSc thesis, Carleton University, Canada. Nelson, K.D., Zhao, W., Brown, L.D., Kuo, J., Che, J., Liu, X., Klemperer, S.L., Makovsky, Y., Meissner, R., Mechie, J. et als 1996. Partially molten middle crust beneath southern Tibet: Synthesis of project INDEPTH results. Science, 274, 1684- 1688. Pande, I.C. 1950. A geological note on the Ramgarh area, Dist. Nainital (U. P.). Quarterly Journal of the Geological, Mining and Metallurgical Society of India, 22, 15-23. Parrish, R.R. & Hodges, K.V. 1996. Isotopic constraints on the age and provenance of the Lesser and Greater Himalayan sequences, Nepalese Himalaya. Geological Society of America Bulletin, 108, 904-911. Passchier, C.W. & Trouw, R.A.J. 2005. Microtectonics. 2nd ed. Springer. Paudel L.P. & Arita, K. 2000. Tectonic and polymetamorphic history of the Lesser Himalaya in central Nepal. Journal of Asian Earth Sciences, 18, 561-584. Pearson, O.N. & DeCelles, P.G. 2005. Structural geology and regional tectonic significance of the Ramgarh thrust, Himalayan fold-thrust belt of Nepal. Tectonics, 24, 1-26. Pêcher, A. 1978. Déformation et métamorphisme associés à une zone de cisaillement: exemple du grand chevauchement central Himalayen (MCT). PhD thesis, Université de Grenoble, France. Pêcher, A. 1989. The metamorphism in the central Himalaya. Journal of Metamorphic Geology, 7, 31-41. 44
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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 and 36: 753 754 better understand the proce
Page 37 and 38: 765 766 References 767 768 769 770
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: 970 971 972 973 974 975 976 977 978
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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