Origin of periodically spaced wrinkle ridges on the Tharsis Plateau of Mars

Mathematics – Logic

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

54

Buckling, Geological Faults, Mars Surface, Planetary Crusts, Mars Craters, Regolith, Ridges, Structural Properties (Geology), Tectonics

Scientific paper

The mechanism responsible for the periodic spacing of wrinkle ridges observed on the Tharsis Plateau of Mars is investigated by examining the characteristics of the spacing of ridges in six major provinces on the plateau; these regions were further divided into domains on the basis of ridge orientation. The ridges are interpreted to be folds resulting from buckling, followed by reverse to thrust faulting (flexure-fracture). Several buckling models that may account for the periodic nature of the ridges are analyzed. The model that would account for the periodic spacing and the asymmetric fold geometry of the ridges involves plastic yielding confined to the hinge area, that would result in rapid closing of the fold and, with continued horizontal shortening, the eventual development of reverse to thrust faulting.

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

Origin of periodically spaced wrinkle ridges on the Tharsis Plateau of Mars 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 Origin of periodically spaced wrinkle ridges on the Tharsis Plateau of Mars, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Origin of periodically spaced wrinkle ridges on the Tharsis Plateau of Mars will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-1739736

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