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:
Ceno Valley, Taro Valley, Parma Province, Emilia-Romagna, Italy


mindat Locality ID: 158513
mindat URL: http://www.mindat.org/loc-158513.html

Tectonic Settings:

Total number of sublocalities beneath "Ceno Valley, Taro Valley, Parma Province, Emilia-Romagna, Italy": 13
Total number of bottom-level sublocalities: 10

Number of Child Localities: 4
Child Localities:
Bardi
Solignano
Varano De' Melegari
Varsi

Latitude: 44°38'0"N
Longitude: 9°43'52"E
Decimal Degree (lat, lon): 44.633333333333,9.7311111111111

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 Ba C Ca Cu F Fe H K Mg Mn Na Ni O P S Si Sr Ti Zn 

Elements from minerals reported directly at this locality: 

Structural Groups for minerals in this locality: 
ApatiteAragoniteBaryteCalciteChalcopyriteClayCoronaditeCorundumDiasporeGypsum
KaoliniteLepidocrociteMilleriteNoneNot in a structural groupPalygorskitePyriteQuartzRutileSerpentine
SphaleriteSpinelTalcTitanite

26 IMA Minerals at location:
Anatase  (*)Aragonite  (*)Baryte  (*)Calcite  (*)Chalcopyrite  (*)
Dolomite  (*)Fluorapatite  (*)Goethite  (*)Gypsum  (*)Hematite  (*)
Hollandite  (*)Ilmenite  (*)Kaolinite  (*)Lepidocrocite  (*)Lizardite  (*)
Magnetite  (*)Millerite  (*)Palygorskite  (*)Pyrite  (*)Quartz  (*)
Rutile  (*)Sphalerite  (*)Talc  (*)Titanite  (*)Todorokite  (*)
Vaesite  (*)
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 groupTiO2268973,689842162
Aragonite  (*)AragoniteCa(CO3)368978,68980,689853250
Baryte  (*)BaryteBa(SO4)668975,68976,68979,68980,68981,6898411547
Calcite  (*)CalciteCa(CO3)968975,68976,68978,68979,68980,68981,68983,68984,6898527770
Chalcopyrite  (*)ChalcopyriteCuFeS2268983,6898527198
Dolomite  (*)NoneCaMg(CO3)2268980,689849895
Fluorapatite  (*)ApatiteCa5(PO4)3F368978,68980,689812740
Goethite  (*)DiasporeFeO(OH)468978,68979,68980,689857437
Gypsum  (*)GypsumCa(SO4)·2H2O368978,68980,689856890
Hematite  (*)CorundumFe2O3568978,68980,68981,68984,6898514640
Hollandite  (*)CoronaditeBa(Mn4+6Mn3+2)O16168985243
Ilmenite  (*)CorundumFe2+Ti4+O3368983,68984,689855433
Kaolinite  (*)Clay KaoliniteAl2Si2O5(OH)4268978,689805591
Lepidocrocite  (*)LepidocrociteFe3+O(OH)168980581
Lizardite  (*)Serpentine ClayMg3Si2O5(OH)4268983,68985359
Magnetite  (*)SpinelFe2+Fe3+2O416898514899
Millerite  (*)MilleriteNiS1689851066
Palygorskite  (*)Palygorskite Clay(Mg,Al)2Si4O10(OH)·4H2O168979306
Pyrite  (*)PyriteFeS216898539462
Quartz  (*)QuartzSiO2268973,6898461156
Rutile  (*)RutileTiO21689855614
Sphalerite  (*)SphaleriteZnS16898521482
Talc  (*)Clay TalcMg3Si4O10(OH)21689853337
Titanite  (*)TitaniteCaTi(SiO4)O368983,68984,689854899
Todorokite  (*)None(Na,Ca,K,Ba,Sr)1-x(Mn,Mg,Al)6O12·3-4H2O268980,68985433
Vaesite  (*)PyriteNiS2168985106



No ages have been assigned to this locality yet.

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All locality data graciously provided by mindat.org

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