Which factor does not contribute to the development of foliation in metamorph OA differential stress OB. rotation of platy or elongate minerals within the rock O C. ductile deformation of the rock O D. dissolution of minerals from regions of high pressure and recrystallizatic OE. pressure that is applied to the rock uniformly in all directions Which mineral would provide the strongest evidence of shock metamorphism ca OA zeolite O B.quartz OC stishovite OD. muscovite

Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
Section: Chapter Questions
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OD marble
E. quartzite
Which factor does not contribute to the development of foliation in metamorphic
OA differential stress
O B. rotation of platy or elongate minerals within the rock
O C. ductile deformation of the rock
O D. dissolution of minerals from regions of high pressure and recrystallization
O E pressure that is applied to the rock uniformly in all directions
Which mineral would provide the strongest evidence of shock metamorphism caus
O A. zeolite
O B. quartz
O
C. stishovite
OD.muscovite
OE. kaolinite (clay)
Which statement best describes mylonites?
OA typically composed of very coarse, angular fragments
OBfom in deep portions of tau
Transcribed Image Text:OD marble E. quartzite Which factor does not contribute to the development of foliation in metamorphic OA differential stress O B. rotation of platy or elongate minerals within the rock O C. ductile deformation of the rock O D. dissolution of minerals from regions of high pressure and recrystallization O E pressure that is applied to the rock uniformly in all directions Which mineral would provide the strongest evidence of shock metamorphism caus O A. zeolite O B. quartz O C. stishovite OD.muscovite OE. kaolinite (clay) Which statement best describes mylonites? OA typically composed of very coarse, angular fragments OBfom in deep portions of tau
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