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La deformación hercínica en los Macizos Paleozoicos Nororientales de la Cordillera Ibérica
| Content Provider | Semantic Scholar |
|---|---|
| Author | Tejero, Rosa Sancho Capote, Ramón |
| Copyright Year | 1987 |
| Abstract | The structural features of the precambrian and paleozoic sediments have been studied in the outcrops located to the NE o Calatayud, in the Iberian Range. The zone was affected by three deformation phases. The first gave rise to folds with a NW-SE orientation and a generalized cleavage. The second produced reverse faults and thrusts, homoaxial with the former structures. The third is characterized by folds WNW-NW and a crenulation cleavage. These deformation phases took place during the hercynian times. |
| Starting Page | 425 |
| Ending Page | 434 |
| Page Count | 10 |
| File Format | PDF HTM / HTML |
| DOI | 10.3989/egeol.87435-6612 |
| Volume Number | 43 |
| Alternate Webpage(s) | http://estudiosgeol.revistas.csic.es/index.php/estudiosgeol/article/download/612/634 |
| Language | English |
| Access Restriction | Open |
| Content Type | Text |
| Resource Type | Article |