Exhumation of the Neuquén Basin in the southern Central Andes (Malargüe fold and thrust belt) from field data and low-temperature thermochronology
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文摘

75–55 and 15–10 Ma cooling episodes (AFT) detected on samples of the Neuquén Basin.

Late Eocene-early Oligocene cooling episode is recognized near the orogenic front.

75–55 and 15–10 Ma cooling episodes coincide with periods of mountain building.

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