Crustal structure, gravity anomalies and subsidence history of the Parnaíba cratonic basin, Northeast Brazil
Cratonic basins cover more than 10% of Earth's continental surface area, yet their origin remains enigmatic. Here, we use a 1400 km long, deep (20 s TWTT) seismic reflection profile, five wide-angle split-spread receiver gathers, gravity anomaly and well data to constrain the origin of the Parn...
| Egile Nagusiak: | , , |
|---|---|
| Formatua: | Journal article |
| Argitaratua: |
American Geophysical Union
2017
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