Mineral Evolution Database
Created and maintained by the Mineral Evolution Project in partnership with RRUFF and mindat.
Mineral locality data provided by mindat.org



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:
Lignol, Morbihan, Brittany, France

Oldest recorded age at locality: 290
Youngest recorded age at locality: 210

mindat Locality ID: 155611
mindat URL: http://www.mindat.org/loc-155611.html

Tectonic Settings:

Total number of sublocalities beneath "Lignol, Morbihan, Brittany, France": 8
Total number of bottom-level sublocalities: 6

Number of Child Localities: 6
Child Localities:
Keriar
Kerlec'h (Kerler)
Kerségalec
Le Henguer (Le Hinguer)
Penderff Hamlet
Saint-Yves

Latitude: 48°0'58"N
Longitude: 3°16'13"W
Decimal Degree (lat, lon): 48.016111111111,-3.2702777777778

AThis mineral is Anthropogenic.
GThis mineral is directly dated.
BThis mineral is reported as having this age.
YThis mineral is using an age reported as an element mineralization period.
OThis mineral is using an age calculated from all data at the locality.
RThe age displayed for this mineral originates from a different, non-child locality.
PThe 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: Al As Ba Bi Ca Ce Cu Fe H K O P Pb S Si Ti U 

Elements from minerals reported directly at this locality: 

Structural Groups for minerals in this locality: 
ArsenicAutuniteChalcopyriteCopperCovelliteDiasporeFluoriteMarcasiteNoneNot in a structural group
PhosphuranylitePyriteQuartzRhabdophaneRocksaltStibniteWölsendorfite

27 IMA Minerals at location:
Anatase  (*)Autunite  (*)Bismuth  (*)Bismuthinite  (*)Chalcocite  (*)
Chalcopyrite  (*)Copper  (*)Covellite  (*)Cuprite  (*)Curite  (*)
Dewindtite  (*)Galena  (*)Goethite  (*)Kasolite  (*)Marcasite  (*)
Ningyoite  (*)Phosphuranylite  (*)Pyrite  (*)Quartz  (*)Sabugalite  (*)
Torbernite  (*)Uraninite  (*)Uranocircite-II  (*)Uranophane-α  (*)Uranosphaerite  (*)
Wölsendorfite  (*)Zeunerite  (*)
Mineral nameStructural GroupsIMA FormulaMax Age (Ma)Min Age (Ma)# of Sublocalities containing mineralLOCALITY IDs, not mindat ids# of localities containing mineral
Anatase  (*)Not in a structural groupTiO22902101533432162
Autunite  (*)AutuniteCa(UO2)2(PO4)2·10-12H2O290270553342,53343,53344,53345,533481272
Bismuth  (*)ArsenicBi2902101533431966
Bismuthinite  (*)StibniteBi2S32902101533431935
Chalcocite  (*)NoneCu2S1533425707
Chalcopyrite  (*)ChalcopyriteCuFeS2290210253342,5334327198
Copper  (*)CopperCu2902101533433846
Covellite  (*)CovelliteCuS2902101533434165
Cuprite  (*)Not in a structural groupCu2O2902101533432970
Curite  (*)NonePb3+x[(UO2)4O4+x(OH)3-x]2·2H2O15334451
Dewindtite  (*)PhosphuranyliteH2Pb3(UO2)6O4(PO4)4·12H2O290210453342,53343,53344,5334582
Galena  (*)RocksaltPbS230210253343,5334424243
Goethite  (*)DiasporeFeO(OH)2902101533437437
Kasolite  (*)NonePb(UO2)(SiO4)·H2O153344198
Marcasite  (*)MarcasiteFeS22902101533435674
Ningyoite  (*)Rhabdophane(U,Ca,Ce)2(PO4)2·1-2H2O29027015334333
Phosphuranylite  (*)PhosphuranyliteKCa(H3O)3(UO2)7(PO4)4O4·8H2O290270353343,53344,53345182
Pyrite  (*)PyriteFeS2290210453342,53343,53344,5334839462
Quartz  (*)QuartzSiO2290210653342,53343,53344,53345,53346,5334861156
Sabugalite  (*)NoneHAl(UO2)4(PO4)4·16H2O15334287
Torbernite  (*)NoneCu(UO2)2(PO4)2·12H2O290270453343,53344,53345,533481059
Uraninite  (*)FluoriteUO2290270453343,53344,53345,533462718
Uranocircite-II  (*)NoneBa(UO2)2(PO4)2·10H2O15334489
Uranophane-α  (*)NoneCa(UO2)2(SiO3OH)2·5H2O290270353343,53344,53345890
Uranosphaerite  (*)NoneBi(UO2)O2(OH)15334418
Wölsendorfite  (*)WölsendorfitePb7(UO2)14O19(OH)4·12H2O15334443
Zeunerite  (*)AutuniteCu(UO2)2(AsO4)2·12H2O153342185



Locality Notes from all Ages at Locality:
Age IDLocality Notes
Giersdorf_00000656The Kerlec'h locality is found within the Pontivy region of France. It is responsible for producing 400 tons of Uranium metal. Uranium in the Pontivy district is usually found intragranitic, the granite is cut by a system of transverse mineralized fractures, preferentially located on the northern part of the Massif. It is within the fractures that the Uranium can be found.
Giersdorf_00000656aThe Kerlec'h locality is found within the Pontivy region of France. It is responsible for producing 400 tons of Uranium metal. Uranium in the Pontivy district is usually found intragranitic, the granite is cut by a system of transverse mineralized fractures, preferentially located on the northern part of the Massif. It is within the fractures that the Uranium can be found.


2 Ages assigned to this locality:

Excel IDMax Age (Ma)Min Age (Ma)Age as listed in referenceDating MethodAge InterpretPrioritized?Sample SourceSample NumRun NumAge from other LocalityDated MineralMinerals explicitely stated as having this ageAge applies to these ElementsMinDat Locality IDDated Locality (Max Age)Location as listed in referenceReferenceReference DOIReference IDAge Notes
Giersdorf_00000656290270290-270U-PbThe age of mineralization being post-cooling of the 300-340 Ma granite bodies restricts the formation of the Uranium minerals to being genetically derived.     U19712Kerlec'h (Kerler), Lignol, Morbihan, Brittany, FranceKerlec'hChauris et al. (1994) PMGFRA_243Age 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."
Giersdorf_00000656a230210230-210K-ArThe age of mineralization being post-cooling of the 300-340 Ma granite bodies restricts the formation of the Uranium minerals to being genetically derived.     Pb, Zn19712Kerlec'h (Kerler), Lignol, Morbihan, Brittany, FranceKerlec'hChauris et al. (1994) PMGFRA_243from pg 262: "The lead-zinc veins (230-210 Ma, K-Ar dating) seem to be the youngest and the antimony veins are of intermediate age"


SampleSource LocalityReference URL


All locality data graciously provided by mindat.org

All age data...

Other copyright data...