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Neogene ongoing tectonics in the Southern Ecuadorian Andes: analysis of the evolution of the stress field
| Content Provider | Semantic Scholar |
|---|---|
| Author | Lavenu, Alain Noblet, Christophe Winter, Th |
| Copyright Year | 1995 |
| Abstract | Abstract Microtectonic analysis of infilling deposits in South Ecuadorian Neogene basins brings to light a compressive stress field with σ1 along a NNE-SSW to NE-SW direction in the early Miocene, changing to an E-W direction in the Middle and Late Miocene. The syn-sedimentary deformations which affect the deposits of the basins suggest similar stress regimes due to a compressive ongoing tectonic system in the Miocene, for at least 15 Ma. There is a good correlation between rapid convergence in the Neogene and the time period during which the continental South Ecuadorian basins were deformed by compression (Quechua period). |
| Starting Page | 47 |
| Ending Page | 58 |
| Page Count | 12 |
| File Format | PDF HTM / HTML |
| DOI | 10.1016/0191-8141(94)E0027-V |
| Alternate Webpage(s) | http://horizon.documentation.ird.fr/exl-doc/pleins_textes/pleins_textes_6/b_fdi_39-40/43120.pdf |
| Alternate Webpage(s) | https://doi.org/10.1016/0191-8141%2894%29E0027-V |
| Volume Number | 17 |
| Language | English |
| Access Restriction | Open |
| Content Type | Text |
| Resource Type | Article |