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:
Severynka Deposit, Central Ukrainian Uranium Province, Kirovohrad Oblast, Ukraine

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

mindat Locality ID: 271956
mindat URL: http://www.mindat.org/loc-271956.html

Tectonic Settings:

Total number of sublocalities beneath "Severynka Deposit, Central Ukrainian Uranium Province, Kirovohrad Oblast, Ukraine": 0
Total number of bottom-level sublocalities: 0

Latitude: 0°0'0"N
Longitude: 0°0'0"E
Decimal Degree (lat, lon): 0,0

A	This mineral is Anthropogenic.
G	This mineral is directly dated.
B	This mineral is reported as having this age.
Y	This mineral is using an age reported as an element mineralization period.
O	This mineral is using an age calculated from all data at the locality.
R	The age displayed for this mineral originates from a different, non-child locality.
P	The 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.

No IMA Minerals occur at this locality according to mindat

Locality Notes from all Ages at Locality:

Age ID	Locality Notes
Giersdorf_00001020	Deposits 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_00001021	Deposits 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_00001022	Deposits 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 ID	Max Age (Ma)	Min Age (Ma)	Age as listed in reference	Age from other Locality	Minerals explicitely stated as having this age	MinDat Locality ID	Dated Locality (Max Age)	Location as listed in reference	Reference	Reference DOI	Reference ID	Age Notes
Giersdorf_00001022	2000	1800	2000-1800	Yes	Brannerite, Uraninite	271947	Michurinske Deposit, Central Ukrainian Uranium Province, Kirovohrad Oblast, Ukraine	Michurisnk Deposit	Laverov et al. (1992)	10.1080/00206819209465621	IGR34_549	Deposits 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_00001020	2000	1800	2000-1800		Brannerite, Uraninite	271956	Severynka Deposit, Central Ukrainian Uranium Province, Kirovohrad Oblast, Ukraine	Severisnk Deposit	Laverov et al. (1992)	10.1080/00206819209465621	IGR34_549	Deposits 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_00001021	2000	1800	2000-1800	Yes	Brannerite, Uraninite	271945	Vatutinske Deposit, Central Ukrainian Uranium Province, Kirovohrad Oblast, Ukraine	Vatutinsk Deposit	Laverov et al. (1992)	10.1080/00206819209465621	IGR34_549	Deposits 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.)

Sample	Source Locality	Reference URL

All locality data graciously provided by mindat.org

All age data...