Geologias Arenas
Enviado por leon852 • 1 de Abril de 2014 • 231 Palabras (1 Páginas) • 202 Visitas
Material original con materia orgánica (MO)
Enterrada - tiempo - temperatura
Factores Críticos: Roca Madre, Ruta de Migración, Roca Reservorio, Trampa, Sello
Otros: Posibilidad de recuperación, calidad, dimensiones, mercado
The nomenclature and boundaries of the Colombian Sedimentary basins as
they appear in the ANH land map need some clarifi cation based on geological
and/or planning and operation criteria for exploration activities in the petroleum
industry.
It is important to mention that some of these regions do not strictly meet the
defi nition of a sedimentary basin, given that they correspond to areas which have
undergone diff erent geological events over time. They could be best defi ned
as Geologic Provinces which, accordingly with the USGS (2000): “each geologic
province is an area having characteristic dimensions of perhaps hundreds to
thousands of kilometers encompassing a natural geologic entity (for example,
sedimentary basin, thrust belt, delta) or some combination of contiguous
geologic entities” and their limits are drawn along natural geologic boundaries
or, in some cases, at an arbitrary water deep in the oceans. Nevertheless, the term
sedimentary basin is conserved here because it is deep-rooted in the geological
literature of Colombia. The new proposal divides the Colombian territory in 23
sedimentary basins (fi gure 4 and 5):
1. Amagá
2. Caguán-Putumayo
3. Catatumbo
4. Cauca-Patía
5. Cesar-Ranchería
6. Chocó
7. Chocó Off shore
8. Colombia
9. Colombian Deep Pacifi c
10. Eastern Cordillera
11. Eastern Llanos
12. Guajira
13. Guajira Off shore
14. Los Cayos
15. Lower Magdalena Valley
16. Middle Magdalena Valley
17. Sinú-San Jacinto
18. Sinú Off shore
19. Tumaco
20. Tumaco Off shore
21. Upper Magdalena Valley
22. Urabá
23. Vaupés-Amazonas
...