Cool. Now that you can interpret
structures formed by plastic deformations of layered rocks. Let's
move on to brittle structures-- joints and faults.
Back | Next
Back
to Table of Contents
Please report problems to: gary.calderone@gccaz.edu
URL:
http://www.gc.maricopa.edu/academicdepartments/physicalscience/gjc-nsf/mplrfold/mplrfold56.html
Last
update: Tuesday, 16-Oct-2012 07:38:54 US Mountain Standard Time
Legal Disclaimer