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:
Nogueira Do Cravo, Oliveira De Azeméis, Aveiro, Portugal

Oldest recorded age at locality: 405
Youngest recorded age at locality: 270

mindat Locality ID: 251809
mindat URL: http://www.mindat.org/loc-251809.html

Tectonic Settings:

Total number of sublocalities beneath "Nogueira Do Cravo, Oliveira De Azeméis, Aveiro, Portugal": 1
Total number of bottom-level sublocalities: 1

Number of Child Localities: 1
Child Localities:
Pintor Mine

Latitude: 40°53'37"N
Longitude: 8°27'35"W
Decimal Degree (lat, lon): 40.893611111111,-8.4597222222222

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: Ag As Au Cu Fe O Pb S Si Sn Zn 

Elements from minerals reported directly at this locality: 

Structural Groups for minerals in this locality: 
ArsenopyriteBaryteChalcopyriteCopperNonePyriteQuartzRocksaltRutileSphalerite

10 IMA Minerals at location:
Anglesite  (*)Arsenopyrite  (*)Cassiterite  (*)Chalcopyrite  (*)Galena  (*)
Gold  (*)Pyrite  (*)Quartz  (*)Silver  (*)Sphalerite  (*)
Mineral nameStructural GroupsIMA FormulaMax Age (Ma)Min Age (Ma)# of Sublocalities containing mineralLOCALITY IDs, not mindat ids# of localities containing mineral
Anglesite  (*)BarytePb(SO4)4052701980082734
Arsenopyrite  (*)ArsenopyriteFeAsS4052701980089052
Cassiterite  (*)RutileSnO24052701980085171
Chalcopyrite  (*)ChalcopyriteCuFeS240527019800827198
Galena  (*)RocksaltPbS40527019800824243
Gold  (*)CopperAu40527019800830554
Pyrite  (*)PyriteFeS240527019800839462
Quartz  (*)QuartzSiO240527019800861156
Silver  (*)CopperAg4052701980085186
Sphalerite  (*)SphaleriteZnS40527019800821482



1 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
Kristen002524405270Hercynian Orogeny     Yes Pb, Zn, Cu, Ag46301Aveiro, PortugalAviero DistrictMarques de Sá et al. (2014)10.1016/j.oregeorev.2014.03.001OGR62_54studied depoists correspond to veins emplaced in E-W fractures, generated late relatively to the Hercynian orogeny


SampleSource LocalityReference URL


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