Measurements of deformation lamellae in quartz grains from the Cambrian Tintic Quartzite near the Willard thrust east of Ogden, Utah, indicate a maximum compressive stress direction consistent with eastward thrusting.

This content is PDF only. Please click on the PDF icon to access.

First Page Preview

First page PDF preview
You do not have access to this content, please speak to your institutional administrator if you feel you should have access.