Which of these combinations of large- scale crustal stress types and resulting strain is most likely to be correct? shear stress causing thrust faults compressive stress causing normal faults O tensional stress causing folding compressive stress causing strike-slip faults tensional stress causing normal faults

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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Which of these combinations of large-
scale crustal stress types and resulting
strain is most likely to be correct?
O shear stress causing thrust faults
compressive stress causing normal faults
tensional stress causing folding
O compressive stress causing strike-slip
faults
tensional stress causing normal faults
Transcribed Image Text:Which of these combinations of large- scale crustal stress types and resulting strain is most likely to be correct? O shear stress causing thrust faults compressive stress causing normal faults tensional stress causing folding O compressive stress causing strike-slip faults tensional stress causing normal faults
Regions where high-grade metamorphic
rocks are exposed at the Earth's surface
(such as New England and the Canadian
Shield) are:
areas undergoing dynamothermal
metamorphism in current continental
collision zones
O the exposed (exhumed) roots of former
collisional mountain belts
remnants of high-P, low-T blueschist
metamorphism in subduction zones
sutured onto continental margins
O crustal rocks exposed in horsts in
continental extension zones
O products of burial metamorphism in deep
sedimentary basins in cratonic platforms
Transcribed Image Text:Regions where high-grade metamorphic rocks are exposed at the Earth's surface (such as New England and the Canadian Shield) are: areas undergoing dynamothermal metamorphism in current continental collision zones O the exposed (exhumed) roots of former collisional mountain belts remnants of high-P, low-T blueschist metamorphism in subduction zones sutured onto continental margins O crustal rocks exposed in horsts in continental extension zones O products of burial metamorphism in deep sedimentary basins in cratonic platforms
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