Oblique Impact-induced (Shock-related) Shearing and Frictional Melting in Pultusk (H5) Chondrite

Details Oblique Impact-induced (Shock-related) Shearing and Frictional Melting in Pultusk (H5) Chondrite Oblique Impact-induced (Shock-related) Shearing and Frictional Melting in Pultusk (H5) Chondrite

Mar 2010

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2010lpi....41.1140k&link_type=abstract

41st Lunar and Planetary Science Conference, held March 1-5, 2010 in The Woodlands, Texas. LPI Contribution No. 1533, p.1140

Physics

Scientific paper

In Pultusk (H5) dark clast has cataclastic texture and light clast shows
evidences for shearing. Boundary of clasts shows evidences of melting.
In whole sample silicates are of S2-S3 stage. Pultusk may have been
deformed at oblique impact-related shearing.

Affiliated with

Also associated with

No associations

Rating

Oblique Impact-induced (Shock-related) Shearing and Frictional Melting in Pultusk (H5) Chondrite 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 Oblique Impact-induced (Shock-related) Shearing and Frictional Melting in Pultusk (H5) Chondrite, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Oblique Impact-induced (Shock-related) Shearing and Frictional Melting in Pultusk (H5) Chondrite will most certainly appreciate the feedback.

Rate now

Comments { 0 }

Profile ID: LFWR-SCP-O-886002