Crustal structure and dynamics under Himalaya and Pamir ranges

Computer Science – Sound

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

6

Scientific paper

Gravity profiles across the Himalayas and the Karakorum and Pamir ranges are analysed using the information available from deep seismic sounding studies. Generalized inversion of a profile along with conventional modelling using multiple bodies has provided several details of the subsrufaces crustal structure. The depth of the Moho varies from 58 km under the Himalayas to 71 km under the Karakorum, and rises to 55 km under the Pamir and the Trans-Alai. Beyond this, a depression of the order of 10-12 km is depicted under the Alai ranges. About 14-15 km above the Moho there is an interface which runs almost parallel to it through the entire section. The material between this interface and the Moho has a density which i higher (~0.13 g/cm3) than the density of a typical continental lower crust and appears to represent the material underthrust from the Indianand the Eurasian plates.
Present address: Laboratory of Geophysics, Aarhus University, Finlandsgade 6-8, DK-8200 Aarhus N., Denmark

No associations

LandOfFree

Say what you really think

Search LandOfFree.com for scientists and scientific papers. Rate them and share your experience with other people.

Rating

Crustal structure and dynamics under Himalaya and Pamir ranges 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 Crustal structure and dynamics under Himalaya and Pamir ranges, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Crustal structure and dynamics under Himalaya and Pamir ranges will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-1647303

  Search
All data on this website is collected from public sources. Our data reflects the most accurate information available at the time of publication.