Microstructural and Isotopic Constraints on Impact Basin Provenance of Detrital Shocked Minerals in the Vaal River, South Africa

Details Microstructural and Isotopic Constraints on Impact Basin Provenance of Detrital Shocked Minerals in the Vaal River, South Africa Microstructural and Isotopic Constraints on Impact Basin Provenance of Detrital Shocked Minerals in the Vaal River, South Africa

Mar 2011

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2011lpi....42.2208e&link_type=abstract

42nd Lunar and Planetary Science Conference, held March 7–11, 2011 at The Woodlands, Texas. LPI Contribution No. 1608, p.2208

Physics

Scientific paper

We present in-situ U-Th-Pb geochronology that confirms the Vredefort
Dome as the origin of detrital shocked zircon found in modern sediments
of the Vaal River at distal locations (>750 km) from the impact
structure.

Affiliated with

Also associated with

No associations

Rating

Microstructural and Isotopic Constraints on Impact Basin Provenance of Detrital Shocked Minerals in the Vaal River, South Africa 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 Microstructural and Isotopic Constraints on Impact Basin Provenance of Detrital Shocked Minerals in the Vaal River, South Africa, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Microstructural and Isotopic Constraints on Impact Basin Provenance of Detrital Shocked Minerals in the Vaal River, South Africa will most certainly appreciate the feedback.

Rate now

Comments { 0 }

Profile ID: LFWR-SCP-O-1392637