Detrital-zircon fission-track ages from the Lower Cenozoic sediments, NW Himalayan foreland basin: Clues for exhumation and denudation of the Himalaya during the India-Asia collision-Reference-Cited by-同舟云学术

Detrital-zircon fission-track ages from the Lower Cenozoic sediments, NW Himalayan foreland basin: Clues for exhumation and denudation of the Himalaya during the India-Asia collision

Published:2009-02-05 Issue:3-4 Volume:121 Page:519-535
ISSN:0016-7606
Container-title:Geological Society of America Bulletin
language:en
Short-container-title:Geological Society of America Bulletin

Author:

Jain A.K.,Lal Nand,Sulemani B.,Awasthi A.K.,Singh Sandeep,Kumar Rajeev,Kumar Devender

Publisher

Geological Society of America

Subject

Geology

Reference130 articles.

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3. Zircon and sphene as fission track geochronometer and geothermometer: A reappraisal

4. Bera M.K. Sarkar A. Chakraborty P.P. Loyal R.S. Sanyal P. 2008, Marine to continental transition in Himalayan foreland: Geological Society of America Bulletin, doi: 10.1130/B26265.1.

5. Fission-track Analysis of Detrital Zircon

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