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...
| Main Author: | |
|---|---|
| Other Authors: | |
| Format: | Others |
| Language: | en_US |
| Published: |
Texas A&M University
2007
|
| Subjects: | |
| Online Access: | http://hdl.handle.net/1969.1/4717 |