Mountain belts are characterized by sedimentary sequences that show little or no deformation.
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Q10: According to the concept of isostasy, lighter,
Q11: Orogenies are not accompanied by metamorphism and
Q12: Some accreted terranes were microcontinents similar to
Q13: One important result of orogeny is that
Q14: Fold and thrust belts are found in
Q16: The more open the folds, the less
Q17: The Andes Mountains, where the South America
Q18: The Appalachian Mountains are an example of
Q19: A cycle of splitting of a supercontinent,
Q20: In the Paleozoic Era the North American
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