Emplacement of hot Lesser Himalayan nappes from 15 to 10 Ma in the Jumla-Surkhet region, western Nepal, and their thermal imprint on the underlying Early Miocene fluvial Dumri Formation

Author:

Sakai Harutaka1,Iwano Hideki2,Danhara Tohru2,Hirata Takafumi1,Takigami Yutaka3

Affiliation:

1. Department of Geology and Mineralogy; Kyoto University; Kyoto; 606-8502; Japan

2. Kyoto Fission-Track Co. Ltd; Kyoto; 603-8832; Japan

3. Kanto Gakuen University; Ohta-shi; Gunma; 373-8515; Japan

Publisher

Wiley

Subject

Geology

Reference46 articles.

1. Amatya K. M. Jnawali B. M. 1994 Geological Map of Nepal scale 1:1,000,000.

2. Thrust tectonics and uplift of the Nepal Himalaya revealed from fission-track ages;Arita;Journal of Geography (Chigaku Zasshi),1997

3. Geology and structure of the Pokhara-Piutahn area, central Nepal;Arita;Journal of the Nepal Geological Society,1982

4. Miocene to Recent exhumation of the central Himalaya determined from combined detrital zircon fission-track and U/Pb analysis of Siwalik sediments, western Nepal;Bernet;Basin Research,2006

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