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:
Boltysh Crater, Kirovohrad Oblast, Ukraine

Oldest recorded age at locality: 2000
Youngest recorded age at locality: 1800

mindat Locality ID: 240430
mindat URL: http://www.mindat.org/loc-240430.html

Tectonic Settings:

Total number of sublocalities beneath "Boltysh Crater, Kirovohrad Oblast, Ukraine": 0
Total number of bottom-level sublocalities: 0

Latitude: 48°53'59"N
Longitude: 32°15'0"E
Decimal Degree (lat, lon): 48.899722222222,32.25

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 Al Au C Ca Ce Cu Fe K Na O P Pb Pt S Si Th Ti Zn Zr 

Elements from minerals reported directly at this locality: Ag Al Au C Ca Ce Cu Fe K Na O P Pb Pt S Si Th Ti Zn Zr 

Structural Groups for minerals in this locality: 
AcanthiteBaddeleyiteCalciteChalcopyriteCopperCorundumFeldsparMonaziteNickelineNone
PotaritePyritePyroxeneQuartzRocksaltSphaleriteZircon

23 IMA Minerals at location:
Acanthite  (*)Albite  (*)Anorthite  (*)Baddeleyite  (*)Chalcopyrite  (*)
Cheralite  (*)Copper  (*)Ferrosilite  (*)Galena  (*)Gold  (*)
Hematite  (*)Ilmenite  (*)Monazite-(Ce)  (*)Platinum  (*)Pyrite  (*)
Pyrrhotite  (*)Quartz  (*)Sanidine  (*)Siderite  (*)Silver  (*)
Sphalerite  (*)Tulameenite  (*)Zircon  (*)
Mineral nameStructural GroupsIMA FormulaMax Age (Ma)Min Age (Ma)# of Sublocalities containing mineralLOCALITY IDs, not mindat ids# of localities containing mineral
Acanthite  (*)AcanthiteAg2S2000180002793
Albite  (*)FeldsparNa(AlSi3O8)2000180008803
Anorthite  (*)FeldsparCa(Al2Si2O8)2000180001036
Baddeleyite  (*)BaddeleyiteZrO2200018000238
Chalcopyrite  (*)ChalcopyriteCuFeS220001800027198
Cheralite  (*)MonaziteCaTh(PO4)220001800050
Copper  (*)CopperCu2000180003846
Ferrosilite  (*)PyroxeneFe2+2Si2O620001800084
Galena  (*)RocksaltPbS20001800024243
Gold  (*)CopperAu20001800030554
Hematite  (*)CorundumFe2O320001800014640
Ilmenite  (*)CorundumFe2+Ti4+O32000180005433
Monazite-(Ce)  (*)MonaziteCe(PO4)200018000945
Platinum  (*)CopperPt200018000485
Pyrite  (*)PyriteFeS220001800039462
Pyrrhotite  (*)NickelineFe7S82000180009056
Quartz  (*)QuartzSiO220001800061156
Sanidine  (*)FeldsparK(AlSi3O8)200018000598
Siderite  (*)CalciteFe(CO3)2000180006417
Silver  (*)CopperAg2000180005186
Sphalerite  (*)SphaleriteZnS20001800021482
Tulameenite  (*)PotaritePt2CuFe20001800048
Zircon  (*)ZirconZr(SiO4)2000180005251



Locality Notes from all Ages at Locality:
Age IDLocality Notes
Giersdorf_00001020Deposits are associated with a granitic gneiss dome and are stockwork-metasomatic deposit associated with alkaline metasomatism. The ore deposits cluster about centers of albitite bodies and are upward-branching lenses and stocks. Their thicknesses vary from 3-5 meters to tens of meters; they extend horizontally from tens to a few hundreds of meters and extend vertically for 1 km or more.
Giersdorf_00001021Deposits are associated with a granitic gneiss dome and are stockwork-metasomatic deposit associated with alkaline metasomatism. The ore deposits cluster about centers of albitite bodies and are upward-branching lenses and stocks. Their thicknesses vary from 3-5 meters to tens of meters; they extend horizontally from tens to a few hundreds of meters and extend vertically for 1 km or more.
Giersdorf_00001022Deposits are associated with a granitic gneiss dome and are stockwork-metasomatic deposit associated with alkaline metasomatism. The ore deposits cluster about centers of albitite bodies and are upward-branching lenses and stocks. Their thicknesses vary from 3-5 meters to tens of meters; they extend horizontally from tens to a few hundreds of meters and extend vertically for 1 km or more.


3 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_00001022200018002000-1800     YesBrannerite, Uraninite 271947Michurinske Deposit, Central Ukrainian Uranium Province, Kirovohrad Oblast, UkraineMichurisnk DepositLaverov et al. (1992)10.1080/00206819209465621IGR34_549Deposits formed from the late stage of early Proterozoic protoactivation which developed as a consequence of granitization (2 Ga.) and proceeded synchronously with emplacement of rapakivi granitic plutons in neighboring blocks. (1.8 Ga.)
Giersdorf_00001020200018002000-1800     YesBrannerite, Uraninite 271956Severynka Deposit, Central Ukrainian Uranium Province, Kirovohrad Oblast, UkraineSeverisnk DepositLaverov et al. (1992)10.1080/00206819209465621IGR34_549Deposits formed from the late stage of early Proterozoic protoactivation which developed as a consequence of granitization (2 Ga.) and proceeded synchronously with emplacement of rapakivi granitic plutons in neighboring blocks. (1.8 Ga.)
Giersdorf_00001021200018002000-1800     YesBrannerite, Uraninite 271945Vatutinske Deposit, Central Ukrainian Uranium Province, Kirovohrad Oblast, UkraineVatutinsk DepositLaverov et al. (1992)10.1080/00206819209465621IGR34_549Deposits formed from the late stage of early Proterozoic protoactivation which developed as a consequence of granitization (2 Ga.) and proceeded synchronously with emplacement of rapakivi granitic plutons in neighboring blocks. (1.8 Ga.)


SampleSource LocalityReference URL


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