Die Geologie des Mondes

Details Die Geologie des Mondes Die Geologie des Mondes

Sep 1982

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1982nw.....69..405v&link_type=abstract

Naturwissenschaften, Volume 69, Issue 9, pp.405-419

Computer Science

Scientific paper

A summary of lunar geology. Light feldspathic rocks which constitute the highland areas are components of the primeval crust of the Moon. Dark pyroxeneand ilmenite-rich basaltic lava flows — resulting from partial melting processes in the lunar mantle — filled the Maria basins, 3.1 3.9 × 109 years ago. Craters of all sizes and large circular basins were formed by impacting bodies from outside which produced the regolith blanket — a mass of comminuted rocks with fragments of impact breccias, impact melt glasses and impact melt rocks.

Affiliated with

Also associated with

No associations

Rating

Die Geologie des Mondes 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 Die Geologie des Mondes, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Die Geologie des Mondes will most certainly appreciate the feedback.

Rate now

Comments { 0 }

Profile ID: LFWR-SCP-O-1262341