Erosion During Accretion: Consequences for Planetary Iron-Silicate Ratios and Tungsten Isotope Anomalies

Details Erosion During Accretion: Consequences for Planetary Iron-Silicate Ratios and Tungsten Isotope Anomalies Erosion During Accretion: Consequences for Planetary Iron-Silicate Ratios and Tungsten Isotope Anomalies

Mar 2010

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2010lpi....41.2271d&link_type=abstract

41st Lunar and Planetary Science Conference, held March 1-5, 2010 in The Woodlands, Texas. LPI Contribution No. 1533, p.2271

Physics

Scientific paper

We model the chemical effects of impact erosion using an N-body model of
late-stage accretion. Planetary Fe:Si ratios are generally increased and
mantle tungsten isotope anomalies are also affected.

Affiliated with

Also associated with

No associations

Rating

Erosion During Accretion: Consequences for Planetary Iron-Silicate Ratios and Tungsten Isotope Anomalies 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 Erosion During Accretion: Consequences for Planetary Iron-Silicate Ratios and Tungsten Isotope Anomalies, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Erosion During Accretion: Consequences for Planetary Iron-Silicate Ratios and Tungsten Isotope Anomalies will most certainly appreciate the feedback.

Rate now

Comments { 0 }

Profile ID: LFWR-SCP-O-1208642