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Geologic province
| Oceanic crust: 0–20 Ma 20–65 Ma >65 Ma |
 | This article includes a list of general references, but it lacks sufficient corresponding inline citations. (May 2014) |
A geologic province is a spatial entity with common geologic attributes.[1] A province may include a single dominant structural element such as a basin or a fold belt, or a number of contiguous related elements. Adjoining provinces may be similar in structure but be considered separate due to differing histories.
- ^ "Geologic Province and Thermo-Tectonic Age Maps". Earthquake Hazards Program. United States Geological Survey. Archived from the original on 7 June 2014. Retrieved 6 June 2014.
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