Lunar Linear Rilles as Surface Manifestations of Dikes: Theoretical Considerations

Physics

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

8

Cones, Dikes, Domes, Rilles, Volcanism

Scientific paper

Linear and arcuate flat-floored rilles and v-shaped fractures are common tectonic features on the planets, are interpreted as extensional in nature, and can have a variety of modes of origin, including flexure, broad elastic expansion in the substrate, hydrofracturing, sliding of near-surface rocks along a detachment, and dike intrusion. In order to establish criteria for these different modes of origin on the Moon, and to utilize these in a better understanding of the range of tectonic forces that have influenced the lunar crust and lithosphere, we develop a theoretical treatment for the penetration of magma-filled cracks (dikes) to the vicinity of the lunar surface, and outline the predicted range of tectonic and associated volcanic features and processes. We then examine the range of rilles and associated features observed on the Moon and analyze them in the context of these predictions.

No associations

LandOfFree

Say what you really think

Search LandOfFree.com for scientists and scientific papers. Rate them and share your experience with other people.

Rating

Lunar Linear Rilles as Surface Manifestations of Dikes: Theoretical Considerations 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 Lunar Linear Rilles as Surface Manifestations of Dikes: Theoretical Considerations, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Lunar Linear Rilles as Surface Manifestations of Dikes: Theoretical Considerations will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-1615517

  Search
All data on this website is collected from public sources. Our data reflects the most accurate information available at the time of publication.