R Baía de Nossa Senhora Conglomerate
Stratigraphy Layers
EonPhanerozoic
EraCenozoic
PeriodQuaternary
EpochPleistocene
AgeLate Pleistocene
StageMarine Isotope Stage 5
SubstageMarine Isotope Substage 5e
Occurrences
| VS | Scientific Name | Archipelago | Island | Location | Min/Max Age |
|---|
Stratigraphy Data
| Designation | Baía de Nossa Senhora Conglomerate |
| Strata Number | 1 |
| Status | Accepted |
| Parent Strata | Marine Isotope Substage 5e |
| Unit Type | Lithostratigraphy |
| Scope | Local |
| Lithology | Basal conglomerate (pebble and cobbel beach deposit) |
| Max Thickness (m) | 1 |
| Top - Base Age (Ma) | 0.1225 - 0.125 |
| Chronostratigraphy - min/max age | Marine Isotope Substage 5e |
| Stratigraphy verification status | Trusted |
| Added by | Ávila, S. P. |
| Added date | 2024-04-30 16:43:08 |
References
Age Reference
Martinson, D. G., Pisias, N. G., Hays, J. D., Imbrie, J., Moore, T. C., & Shackleton, N. J. (1987). Age dating and the orbital theory of the ice ages: development of a high-resolution 0 to 300,000-year Chronostratigraphy. 1–29. Quaternary research. 27. 1. https://doi.org/10.1016/0033-5894(87)90046-9.
Martinson, D. G., Pisias, N. G., Hays, J. D., Imbrie, J., Moore, T. C., & Shackleton, N. J. (1987). Age dating and the orbital theory of the ice ages: development of a high-resolution 0 to 300,000-year Chronostratigraphy. 1–29. Quaternary research. 27. 1. https://doi.org/10.1016/0033-5894(87)90046-9.