The Mineral Evolution database is currently under development.
The goal of this page is to present localities at which the mineral is found, and estimates of the oldest possible geologic age of the minerals at these localities.
Locality Name:Pays De La Loire, FranceOldest recorded age at locality: 296Youngest recorded age at locality: 170mindat Locality ID: 21902mindat URL:http://www.mindat.org/loc-21902.htmlTectonic Settings: Total number of sublocalities beneath "Pays De La Loire, France": 383Total number of bottom-level sublocalities: 255Number of Child Localities: 5Child Localities:Loire-AtlantiqueMaine-et-LoireMayenneSartheVendéeLatitude: 47°31'49"NLongitude: 0°-54'0"EDecimal Degree (lat, lon): 47.530277777778,-0.9
A
This mineral is Anthropogenic.
G
This mineral is directly dated.
B
This mineral is reported as having this age.
Y
This mineral is using an age reported as an element mineralization period.
O
This mineral is using an age calculated from all data at the locality.
R
The age displayed for this mineral originates from a different, non-child locality.
P
The age displayed for this mineral is the range of ages for this mineral at all of this locality's children.
This mineral's age has not yet been recorded.
This Mineral list contains entries from this locality, including sub-localities. Minerals in bold are reported by mindat.org as occurring directly at this locality, and do not occur at any children (sublocalities) of this locality.Elements at this locality, including sub-localities: AgAlAsAuBBaBeBiCCaCdCeClCuFFeHHgKLaLiMgMnMoNNaNbNiOPPbSSbScSiSnSrTaThTiUVWYZnZrElements from minerals reported directly at this locality: Structural Groups for minerals in this locality:
The La Commanderie Mine locality is found within the Mortagne mining district. The mine is responsible for the production of 3300 tons of Uranium metal. It is part of the Armorican Massif. The Mortagne district is also associated with the Deux-Sèvres area, all part of the Armorican Massif
Giersdorf_00000657a
The La Commanderie Mine locality is found within the Mortagne mining district. The mine is responsible for the production of 3300 tons of Uranium metal. It is part of the Armorican Massif. The Mortagne district is also associated with the Deux-Sèvres area, all part of the Armorican Massif
Giersdorf_00000658
The L'Ecarpière locality is found within the Mortagne mining district. The mine is responsible for the production of 3120 tons of Uraniium metal. It is part of the Armorican Massif.
Giersdorf_00000658a
The L'Ecarpière locality is found within the Mortagne mining district. The mine is responsible for the production of 3120 tons of Uraniium metal. It is part of the Armorican Massif.
Giersdorf_00000659
The Le Chardon locality is found within the Mortagne mining district. The mine is responsible for the production of 2745 tons of Uranium metal. It is part of the Armorican Massif.
Giersdorf_00000659a
The Le Chardon locality is found within the Mortagne mining district. The mine is responsible for the production of 2745 tons of Uranium metal. It is part of the Armorican Massif.
Giersdorf_00000661
The Penaran Mine is located in the Guérande mining district and is part of the Armorican Massif. It has produced 470 tons of Uranium metal.
Giersdorf_00000661a
The Penaran Mine is located in the Guérande mining district and is part of the Armorican Massif. It has produced 470 tons of Uranium metal.
The age of mineralization being post-cooling of the 300-340 Ma granite bodies restricts the formation of the Uranium minerals to being genetically derived.
Age of the uranium mineralization in the Armorican Massif is associated with Hercynian peraluminous granites. From pg. 262: "The precise chronology of these mineralizations is not well established. The uranium veins appear to be the oldest (290-270 Ma by U/Pb dating) but underwent late remobilization processes."
The age of mineralization being post-cooling of the 300-340 Ma granite bodies restricts the formation of the Uranium minerals to being genetically derived.
The age of mineralization being post-cooling of the 300-340 Ma granite bodies restricts the formation of the Uranium minerals to being genetically derived.
Age of the uranium mineralization in the Armorican Massif is associated with Hercynian peraluminous granites. From pg. 262: "The precise chronology of these mineralizations is not well established. The uranium veins appear to be the oldest (290-270 Ma by U/Pb dating) but underwent late remobilization processes."
The age of mineralization being post-cooling of the 300-340 Ma granite bodies restricts the formation of the Uranium minerals to being genetically derived.
The age of mineralization being post-cooling of the 300-340 Ma granite bodies restricts the formation of the Uranium minerals to being genetically derived.
Age of the uranium mineralization in the Armorican Massif is associated with Hercynian peraluminous granites. From pg. 262: "The precise chronology of these mineralizations is not well established. The uranium veins appear to be the oldest (290-270 Ma by U/Pb dating) but underwent late remobilization processes."
The age of mineralization being post-cooling of the 300-340 Ma granite bodies restricts the formation of the Uranium minerals to being genetically derived.
The age of mineralization being post-cooling of the 300-340 Ma granite bodies restricts the formation of the Uranium minerals to being genetically derived.
Age of the uranium mineralization in the Armorican Massif is associated with Hercynian peraluminous granites. From pg. 262: "The precise chronology of these mineralizations is not well established. The uranium veins appear to be the oldest (290-270 Ma by U/Pb dating) but underwent late remobilization processes."
The age of mineralization being post-cooling of the 300-340 Ma granite bodies restricts the formation of the Uranium minerals to being genetically derived.