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