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Mylonite and porphyroclast in the Santa Catalina Mtn. Core Complex

Mylonite and porphyroclast in the Santa Catalina Mtn. Core Complex

Santa Catalina Mtns | Pima County, Arizona.  Mylonitized Oracle Granite from the lower plate of the Santa Catalina detachment fault exposed in the  Lower Tanque Verde Falls. The porphyroclast - large deformed spherical shape with an obvious tail - provides a sense of shear.  (Photo by Jessica Rudd)

Mylonite - a metamorphic rock formed by ductile deformation that accompanies intense shearing encountered during folding and faulting, a process termed cataclastic or dynamic metamorphism. In this case the Oracle granite was ductily sheared during extension that moved the rock ~20 miles northward and 2-3 miles surfaceward. The parent granite was severely pulverized, obliterating the original minerals which recrystallise as smaller, tightly intergrown grains, forming a dense, hard rock. As a result of the shearing encountered during formation, recrystallised minerals grow preferentially along planes of foliation parallel to the direction of shear. 

For a geologist's guide to the rocks and structures of the Santa Catalina Mountain core complex, see Jon Spencer's 38-pg illustrated report:

https://library.azgs.arizona.edu/item/AOFR-1552429673312-319

Photographer: Jessica Rudd

Photo Date: 2013