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The Araripe Basin in NE Brazil: An intracontinental graben inverted to a high-standing horst
Tectonophysics, 2014Abstract The Mesozoic sediments of the Araripe Basin peak at ca. 1000 m, more than 500 m above the host Precambrian basement. This means that an intracontinental graben has been inverted to a topographically high-standing horst, which raises four fundamental questions: (1) Where are the inversion structures? (2) What is the age of the inversion?
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