Northward younging zircon fission‐track ages from 13 to 2 Ma in the eastern extension of the Kathmandu nappe and underlying Lesser Himalayan sediments distributed to the south of Mt. Everest

Author:

Nakajima Toru1ORCID,Sakai Harutaka1ORCID,Iwano Hideki2ORCID,Danhara Tohru2,Hirata Takafumi3ORCID

Affiliation:

1. Department of Geology and Mineralogy, Division of Earth Planetary Sciences, Graduate School of Science Kyoto University Kyoto 606‐8502 Japan

2. Kyoto Fission‐Track Co. Ltd Kyoto 603‐8832 Japan

3. Geochemical Research Center The University of Tokyo Tokyo 113‐0033 Japan

Publisher

Wiley

Subject

Geology

Reference92 articles.

1. Lateral extrusion, underplating, and out-of-sequence thrusting within the Himalayan metamorphic core, Kanchenjunga, Nepal

2. Kinematics of the Dadeldhura klippe shear zones (W Nepal): implications for the foreland evolution of the Himalayan metamorphic core

3. Thrust Tectonics and Uplift Process of the Nepal Himalaya Revealed from Fission-Track Ages

4. Geology and structure of the Pokhara‐Piutahn area, central Nepal;Arita K;Journal of the Nepal Geological Society,1982

5. Geology of western Nepal and a comparison with Kumaun, India;Arita K.;Journal of the Faculty of Science, Hokkaido University, Series 4, Geology and Mineralogy,1984

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