Bel Air Mine, La Chapelle Largeau, Deux-Sèvres, Nouvelle-Aquitaine, France
|Latitude & Longitude (WGS84):||46° 56' 56'' North , 0° 50' 26'' West|
|Latitude & Longitude (decimal):||46.94889,-0.84056|
|Köppen climate type:||Cfb : Temperate oceanic climate|
|Other/historical region names associated with this locality:||Poitou-Charentes|
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32 valid minerals.
This geological map and associated information on rock units at or nearby to the coordinates given for this locality is based on relatively small scale geological maps provided by various national Geological Surveys. This does not necessarily represent the complete geology at this locality but it gives a background for the region in which it is found.
Click on geological units on the map for more information. Click here to view full-screen map on Macrostrat.org
|Permian - Carboniferous|
252.17 - 358.9 Ma
|Carboniferous-Permian plutonic rocks|
Age: Paleozoic (252.17 - 358.9 Ma)
Comments: Deep-seated to high-level intrusions are included. Many charnockites, anorthosites, and large ophiolites, classified as plutons, are distinguished in the database using the SIGNIF item. Ophiolites were classified as plutons, even where remnants may be extrusive and/or sedimentary.
Lithology: Plutonic rocks
Reference: Geological Survey of Canada. Generalized geological map of the world and linked databases. doi:10.4095/195142. Open File 2915d. 
- Lièvre, J.-M. & Johannet, J.-M. (2002): Les gisements uranifères de la bordure deux-sèvrienne du massif de Mortagne-sur-Sèvre (85). Le Cahier des Micromonteurs, 75, 8-25.(in French)
- Johannet, J.-M. (2006): Belles découvertes de dufrénite en Deux-Sèvres. Le Cahier des Micromonteurs, 93, 72-76. (in French)