Spherules in a Paleoproterozoic Dolomite Layer in the Ketilidian Orogen of South Greenland are Candidates for Ejecta from the Vredefort Structure

Details Spherules in a Paleoproterozoic Dolomite Layer in the Ketilidian Orogen of South Greenland are Candidates for Ejecta from the Vredefort Structure Spherules in a Paleoproterozoic Dolomite Layer in the Ketilidian Orogen of South Greenland are Candidates for Ejecta from the Vredefort Structure

Mar 2001

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2001lpi....32.1142s&link_type=abstract

32nd Annual Lunar and Planetary Science Conference, March 12-16, 2001, Houston, Texas, abstract no.1142

Physics

Scientific paper

Mm-scale spherules form ~18% of a single meter-thick dolomite layer in
the Ketilidian orogen. Previously thought to be microfossils, their
splash-form shapes and replaced spinels(?) suggest they are impact
ejecta potentially coeval with Vredefort.

Affiliated with

Also associated with

No associations

Rating

Spherules in a Paleoproterozoic Dolomite Layer in the Ketilidian Orogen of South Greenland are Candidates for Ejecta from the Vredefort Structure 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 Spherules in a Paleoproterozoic Dolomite Layer in the Ketilidian Orogen of South Greenland are Candidates for Ejecta from the Vredefort Structure, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Spherules in a Paleoproterozoic Dolomite Layer in the Ketilidian Orogen of South Greenland are Candidates for Ejecta from the Vredefort Structure will most certainly appreciate the feedback.

Rate now

Comments { 0 }

Profile ID: LFWR-SCP-O-1009178