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| | proterozoic rocks |
 | | The primary objective is to obtain knowledge of the structural geology of the Proterozoic rocks in western Colorado, eastern Utah, Arizona, and New Mexico, and to interpret the differences in deformation between the Paleoproterozoic and Mesoproterozoic rocks, the forces required for the deformation, and their general location. |
 | | The Paleoproterozoic rocks of the Cerbat Mountains of northwestern Arizona are described as containing metavolcanic and metasedimentary rocks that have been intruded by granitoids and which experienced two periods of deformation (Duebendorfer et al, 2001). |
 | | Paleoproterozoic rocks are composed primarily of seven types of gneiss, one of which is a garnet-sillimanite-biotite gneiss, two types of schist, and an amphibolite (Siddoway et al, 2000). |
| www.mesastate.edu /snsm/geology/classes/seminar/ahosack/protrx.html (1833 words) |
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