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                             12 results found
no title author magazine year volume issue page(s) type
1 Conference report: 16th Himalaya–Karakorum–Tibet workshop, Schloss Seggau, Austria 4–6 April 2001 Stüwe, K.
2002
21 3 p. 217-219
3 p.
article
2 Contents continued from OBC 2002
21 3 p. 340-
1 p.
article
3 Geochemical characteristics of Mesoproterozoic clastic sedimentary rocks from the Chakrata Formation, Lesser Himalaya: implications for crustal evolution and weathering history in the Himalaya Rashid, S.A.
2002
21 3 p. 283-293
11 p.
article
4 Geology, geochemistry and Ar–Ar geochronology of the Nangimali ruby deposit, Nanga Parbat Himalaya (Azad Kashmir, Pakistan) Pêcher, A.
2002
21 3 p. 265-282
18 p.
article
5 Inside front cover (Editorial Board) 2002
21 3 p. IFC-
1 p.
article
6 New constraints on the India–Asia collision: the Lower Miocene Gangrinboche conglomerates, Yarlung Tsangpo suture zone, SE Tibet Aitchison, Jonathan C.
2002
21 3 p. 251-263
13 p.
article
7 Ore mineralization causing slope failure in a high-altitude mountain crest—on the collapse of an 8000m peak in Nepal Weidinger, Johannes T.
2002
21 3 p. 295-306
12 p.
article
8 Oxygen isotope trends and anomalies in granitoids of the Tibetan plateau Blattner, Peter
2002
21 3 p. 241-250
10 p.
article
9 Paleosols of middle Holocene age in the Thakkhola basin, central Nepal, and their paleoclimatic significance Saijo, Kiyoshi
2002
21 3 p. 323-329
7 p.
article
10 Sm–Nd mineral ages of pegmatite veins and their host rocks from Swat area, Chilas complex, northern Pakistan Ali, A.
2002
21 3 p. 331-339
9 p.
article
11 The Beimarang mélange (southern Tibet) brings additional constraints in assessing the origin, metamorphic evolution and obduction processes of the Yarlung Zangbo ophiolite Huot, François
2002
21 3 p. 307-322
16 p.
article
12 Thrusting, extension, and doming during the polyphase tectonometamorphic evolution of the High Himalayan Crystalline Zone in NW India Robyr, M
2002
21 3 p. 221-239
19 p.
article
                             12 results found
 
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