Fission track geochronology of India

Details Fission track geochronology of India Fission track geochronology of India

Nov 1981

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1981ineps..90..389n&link_type=abstract

Proceedings of the Indian Academy of Sciences - Earth and Planetary Sciences, Volume 90, Issue 3, pp.389-401

Computer Science

Fission Tracks, Geochronology, Closing Temperature, Cooling And Uplift Rates, Orogenic Belts

Scientific paper

The fission track ages of cogenetic/co-existing minerals namely garnet, muscovite and apatite from three mica belts i.e., Bihar, Rajasthan, Nellore of peninsular India and Himalayan region, coupled with the corresponding closing temperatures of the minerals have been used to reveal the thermal and uplift histories of these regions. The data show that the extra-peninsular part of the subcontinent during Himalayan orogenic cycle (upper cretaceous-tertiary) witnessed the highest cooling and uplift rates in comparison to the older cycles in peninsular India.

Affiliated with

Also associated with

No associations

Rating

Fission track geochronology of India does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

If you have personal experience with Fission track geochronology of India, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Fission track geochronology of India will most certainly appreciate the feedback.

Rate now

Comments { 0 }

Profile ID: LFWR-SCP-O-744338