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:
Pejo Valley (Peio Valley), Sole Valley, Trento Province (Trentino), Trentino-Alto Adige, Italy

Oldest recorded age at locality: 281
Youngest recorded age at locality: 252

mindat Locality ID: 123241
mindat URL: http://www.mindat.org/loc-123241.html

Tectonic Settings:

Total number of sublocalities beneath "Pejo Valley (Peio Valley), Sole Valley, Trento Province (Trentino), Trentino-Alto Adige, Italy": 3
Total number of bottom-level sublocalities: 2

Number of Child Localities: 2
Child Localities:
Celledizzo
Comasine

Latitude: 0°0'0"N
Longitude: 0°0'0"E
Decimal Degree (lat, lon): 0,0
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 B Be Ca Cu Fe H K Mg Na O S Si 

Elements from minerals reported directly at this locality: Al B Be Fe H Na O Si 

Structural Groups for minerals in this locality: 
AmphiboleBerylChalcopyriteClayClinozoisiteEpidoteGarnetMarcasiteMicaNone
OlivinePyritePyroxeneQuartzSpinelTourmaline

13 IMA Minerals at location:
Actinolite  (*)Almandine  (*)Augite  (*)Beryl  (*)Chalcopyrite  (*)
Chrysoberyl  (*)Epidote  (*)Magnetite  (*)Marcasite  (*)Muscovite  (*)
Pyrite  (*)Quartz  (*)Schorl  (*)
Mineral nameStructural GroupsIMA FormulaMax Age (Ma)Min Age (Ma)# of Sublocalities containing mineralLOCALITY IDs, not mindat ids# of localities containing mineral
Actinolite  (*)Amphibole   Ca2(Mg4.5-2.5Fe2+0.5-2.5)Si8O22(OH)22812521724953419
Almandine  (*)GarnetFe2+3Al2(SiO4)32812521724952353
Augite  (*)Pyroxene(Ca,Mg,Fe)2Si2O62812521724952060
Beryl  (*)BerylBe3Al2Si6O1828125204286
Chalcopyrite  (*)ChalcopyriteCuFeS228125217249527198
Chrysoberyl  (*)OlivineBeAl2O42812520321
Epidote  (*)Epidote ClinozoisiteCa2(Al2Fe3+)[Si2O7][SiO4]O(OH)2812521724958173
Magnetite  (*)SpinelFe2+Fe3+2O4281252272493,7249514899
Marcasite  (*)MarcasiteFeS22812521724955674
Muscovite  (*)Mica ClayKAl2(Si3Al)O10(OH)228125217249517380
Pyrite  (*)PyriteFeS228125217249539462
Quartz  (*)QuartzSiO228125217249561156
Schorl  (*)TourmalineNaFe2+3Al6(Si6O18)(BO3)3(OH)3(OH)28125202705


Locality Notes from all Ages at Locality:
Age IDLocality Notes
Giersdorf_00000651The Val Daone Conglomerate is a mid-Permian unit that runs through much of the south-central Alpine region. Some localities possess trace amounts of U and Cu.


4 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_00000651268266late- to post-KazanianBiostratigraphyAge is interpreted by the author as being linked to the "Mid Permian Event" which is a surge of tectonic activity that represents the final act of the Hercyanian/Variscan cycle   Yes  24815Trento Province (Trentino), Trentino-Alto Adige, ItalyTrento RegionCassinis et al. (2008) IJG127_519Age of the Val Daone Conglomerate is expressed as Mid to Upper Permian, late to post Kazanian and possibly up into the lower Tatarian. The age is derived from palynological evidence as well as other paleontological sources compiled and given an estimated age. See fig. 11
Giersdorf_00000652276273276-273Biostratigraphy    Yes  24815Trento Province (Trentino), Trentino-Alto Adige, ItalyTrento RegionCassinis et al. (2008) IJG127_519Age of the Treviogo is described as lower to middle Permian, mostly Kungarian. The age is derived from palynological evidence as well as other paleontological sources compiled and given an estimated age. See fig. 11
Giersdorf_00000653281277281-277Biostratigraphy    Yes  24815Trento Province (Trentino), Trentino-Alto Adige, ItalyTrento RegionCassinis et al. (2008) IJG127_519Age of the Collio Formation is described as lower Permian, mostly Artinskian. The numbers do not agree with the GSA's Arinskian age as the paper uses a different Time Scale. The age is derived from palynological evidence as well as other paleontological sources compiled and given an estimated age. See fig. 11
Giersdorf_00000654266252266-252Biostratigraphy    Yes  24815Trento Province (Trentino), Trentino-Alto Adige, ItalyTrento RegionCassinis et al. (2008) IJG127_519Age of the Verrucano formation is described as Upper Permian and Upper Tatarian. The age is derived from palynological evidence as well as other paleontological sources compiled and given an estimated age. See fig. 11

SampleSource LocalityReference URL

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