Mesozoic tectonic inversion in the Neuquen Basin of west-central Argentina
Mesozoic tectonic inversion in the Neuquen Basin of west-central Argentina produced two main fault systems: (1) deep faults that affected basement and syn-rift strata where preexisting faults were selectively reactivated during inversion based on their length and (2) shallow faults that affected pos...
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Format: | Others |
Language: | en_US |
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Texas A&M University
2007
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Online Access: | http://hdl.handle.net/1969.1/4717 |