Abstract
The north-south structural evolution in the Subandean zone (eastern side of the Central Andes) reflects the complexity of the orogenic front that propagates on an heterogeneous substratum inherited from pre-Andean palaeogeographies. The construction of balanced cross-sections shows that this north-south evolution corresponds to a progressive transformation from thick-skin transpressive deformation to thin-skin compressive deformation. The thrust front propagation is controlled, in the north, by NNE-SSW to north-south rift systems Permo-Triassic to Jurassic in age, oblique to the chain, and in the south, by the relatively isopach series of the preserved Palaeozoic silico-clastic platform.
| Translated title of the contribution | Structure and palaeogeographic control of the Peruvian Subandean zone |
|---|---|
| Original language | French |
| Pages (from-to) | 741-748 |
| Number of pages | 8 |
| Journal | Comptes Rendus de l'Academie de Sciences - Serie IIa: Sciences de la Terre et des Planetes |
| Volume | 333 |
| Issue number | 11 |
| DOIs | |
| State | Published - 15 Dec 2001 |
| Externally published | Yes |
Keywords
- Andes
- Balanced cross-section
- Peru
- Rift
- Subandean
- Tectonic inversion
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