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:
Mariánské Lázně, Cheb District, Karlovy Vary Region, Czech Republic

Oldest recorded age at locality: 191
Youngest recorded age at locality: 179

mindat Locality ID: 144838
mindat URL: http://www.mindat.org/loc-144838.html

Tectonic Settings:

Total number of sublocalities beneath "Mariánské Lázně, Cheb District, Karlovy Vary Region, Czech Republic": 11
Total number of bottom-level sublocalities: 8

Number of Child Localities: 8
Child Localities:
Broumov
Dyleň
Kladská
Podhorní Hill (Podhora)
Slavkovský Les Mtn
Teplá
Tři Sekery
Trstěnice (Neudorf B. Plan; Neudorf II)

Latitude: 49°59'17"N
Longitude: 12°47'5"E
Decimal Degree (lat, lon): 49.988055555556,12.784722222222

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.

Alunite	Analcime	Andalusite	Apatite	Aragonite	Arsenic	Atelestite	Autunite	Baryte	Bismutite
Brannerite	Brochantite	Calcite	Cancrinite-sodalite	Chalcopyrite	Clay	Copper	Corundum	Covellite	Diaspore
Feldspar	Fluorite	Gismondine	Gypsum	Halotrichite	Iron	Kaolinite	Kobellite	Koritnigite	Matlockite
Meta-autunite	Mixite	Natrolite	None	Not in a structural group	Perovskite	Phosphuranylite	Pyrite	Pyrophyllite	Pyroxene
Quartz	Rocksalt	Scheelite	Sodalite	Sphalerite	Spinel	Stibnite	Talc	Tridymite	Triplite
Vivianite	Wollastonite	Zippeite	Zircon

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 As Au Ba Bi C Ca Cl Co Cr Cu F Fe H K Mg Mn Na Ni O P Pb S Sb Si Ti U V Zn

Elements from minerals reported directly at this locality: F Fe H Mn O P

Structural Groups for minerals in this locality:
Alunite Analcime Andalusite Apatite Aragonite Arsenic Atelestite Autunite Baryte Bismutite
Brannerite Brochantite Calcite Cancrinite-sodalite Chalcopyrite Clay Copper Corundum Covellite Diaspore
Feldspar Fluorite Gismondine Gypsum Halotrichite Iron Kaolinite Kobellite Koritnigite Matlockite
Meta-autunite Mixite Natrolite None Not in a structural group Perovskite Phosphuranylite Pyrite Pyrophyllite Pyroxene
Quartz Rocksalt Scheelite Sodalite Sphalerite Spinel Stibnite Talc Tridymite Triplite
Vivianite Wollastonite Zippeite Zircon

85 IMA Minerals at location:

Aegirine ()*	Aegirine-augite ()*	Andalusite ()*	Aragonite ()*	Atelestite ()*
Autunite ()*	Baryte ()*	Bismuth ()*	Bismuthinite ()*	Bismutite ()*
Bismutoferrite ()*	Brannerite ()*	Brochantite ()*	Calcite ()*	Chalcocite ()*
Chalcopyrite ()*	Cobaltkoritnigite ()*	Coffinite ()*	Covellite ()*	Diopside ()*
Eulytine ()*	Ferripyrophyllite ()*	Fluorite ()*	Galena ()*	Gismondine ()*
Goethite ()*	Gold ()*	Gypsum ()*	Halotrichite ()*	Hechtsbergite ()*
Hematite ()*	Hörnesite ()*	Hydroxylapatite ()*	Ilmenite ()*	Iron ()*
Jarosite ()*	Kobellite ()*	Leucite ()*	Magnetite ()*	Mesolite ()*
Meta-autunite ()*	Metarauchite ()*	Metatorbernite ()*	Mimetite ()*	Mixite ()*
Natrojarosite ()*	Natrolite ()*	Nepheline ()*	Orthoclase ()*	Perovskite ()*
Petitjeanite ()*	Phosphowalpurgite ()*	Phosphuranylite ()*	Preisingerite ()*	Pseudomalachite ()*
Pucherite ()*	Pyrite ()*	Quartz ()*	Retgersite ()*	Saléeite ()*
Sanidine ()*	Schreibersite ()*	Sillénite ()*	Sillimanite ()*	Smrkovecite ()*
Sodalite ()*	Sphalerite ()*	Studtite ()*	Taenite ()*	Talc ()*
Thénardite ()*	Torbernite ()*	Triplite ()*	Troilite ()*	Uraninite ()*
Uranocircite-II ()*	Uranosphaerite ()*	Vivianite ()*	Vochtenite ()*	Walpurgite ()*
Weeksite ()*	Wollastonite ()*	Yingjiangite ()*	Zavaritskite ()*	Zippeite ()*

Mineral name	Structural Groups	IMA Formula	Max Age (Ma)	Min Age (Ma)	# of Sublocalities containing mineral	LOCALITY IDs, not mindat ids	# of localities containing mineral
Aegirine ()*	Pyroxene	NaFe³⁺Si₂O₆	191	179	1	46508	1022
Aegirine-augite ()*	Pyroxene	(Ca,Na)(Fe³⁺,Mg,Fe²⁺)Si₂O₆	191	179	1	46508	286
Andalusite ()*	Andalusite	Al₂SiO₅	191	179	1	46507	1310
Aragonite ()*	Aragonite	Ca(CO₃)	191	179	1	46508	3250
Atelestite ()*	Atelestite	Bi₂O(AsO₄)(OH)	191	179	1	46510	47
Autunite ()*	Autunite	Ca(UO₂)₂(PO₄)₂·10-12H₂O	191	179	2	46507,46510	1272
Baryte ()*	Baryte	Ba(SO₄)	191	179	1	46513	11547
Bismuth ()*	Arsenic	Bi	191	179	1	46510	1966
Bismuthinite ()*	Stibnite	Bi₂S₃	191	179	1	46510	1935
Bismutite ()*	Bismutite	Bi₂O₂(CO₃)	191	179	2	46510,46513	716
Bismutoferrite ()*	Kaolinite	Fe³⁺₂Bi(SiO₄)₂(OH)	191	179	2	46510,46513	51
Brannerite ()*	Brannerite	UTi₂O₆	191	179	1	46506	248
Brochantite ()*	Brochantite	Cu₄(SO₄)(OH)₆	191	179	1	46513	1633
Calcite ()*	Calcite	Ca(CO₃)	191	179	3	46506,46508,46513	27770
Chalcocite ()*	None	Cu₂S	191	179	1	46513	5707
Chalcopyrite ()*	Chalcopyrite	CuFeS₂	191	179	1	46513	27198
Cobaltkoritnigite ()*	Koritnigite	Co(AsO₃OH)·H₂O	191	179	1	46510	32
Coffinite ()*	Zircon	U(SiO₄)·nH₂O	191	179	1	46506	566
Covellite ()*	Covellite	CuS	191	179	1	46513	4165
Diopside ()*	Pyroxene	CaMgSi₂O₆	191	179	1	46508	4135
Eulytine ()*	None	Bi₄(SiO₄)₃	191	179	1	46510	72
Ferripyrophyllite ()*	Clay Pyrophyllite	Fe³⁺Si₂O₅(OH)	191	179	1	46510	9
Fluorite ()*	Fluorite	CaF₂	191	179	2	46506,46507	9617
Galena ()*	Rocksalt	PbS	191	179	3	46505,46506,46510	24243
Gismondine ()*	Gismondine	Ca₂(Si₄Al₄)O₁₆·8H₂O	191	179	1	46508	128
Goethite ()*	Diaspore	FeO(OH)	191	179	2	46507,46513	7437
Gold ()*	Copper	Au	191	179	1	46510	30554
Gypsum ()*	Gypsum	Ca(SO₄)·2H₂O	191	179	1	46506	6890
Halotrichite ()*	Halotrichite	Fe²⁺Al₂(SO₄)₄·22H₂O	191	179	1	46506	409
Hechtsbergite ()*	Atelestite	Bi₂O(VO₄)(OH)	191	179	1	46510	6
Hematite ()*	Corundum	Fe₂O₃	191	179	1	46508	14640
Hörnesite ()*	Vivianite	Mg₃(AsO₄)₂·8H₂O	191	179	1	46510	103
Hydroxylapatite ()*	Apatite	Ca₅(PO₄)₃OH	191	179	1	46508	367
Ilmenite ()*	Corundum	Fe²⁺Ti⁴⁺O₃	191	179	1	46508	5433
Iron ()*	Iron	Fe	191	179	1	46512	1089
Jarosite ()*	Alunite	KFe³⁺₃(SO₄)₂(OH)₆	191	179	1	46513	2228
Kobellite ()*	Kobellite	Pb₁₁(Cu,Fe)₂(Bi,Sb)₁₅S₃₅	191	179	1	46510	87
Leucite ()*	Analcime	K(AlSi₂O₆)	191	179	1	46508	233
Magnetite ()*	Spinel	Fe²⁺Fe³⁺₂O₄	191	179	2	46508,46515	14899
Mesolite ()*	Natrolite	Na₂Ca₂(Si₉Al₆)O₃₀·8H₂O	191	179	1	46508	425
Meta-autunite ()*	Meta-autunite	Ca(UO₂)₂(PO₄)₂·6H₂O	191	179	1	46507	388
Metarauchite ()*	Autunite	Ni(UO₂)₂(AsO₄)₂·8H₂O	191	179	1	46510	6
Metatorbernite ()*	None	Cu(UO₂)₂(PO₄)₂·8H₂O	191	179	1	46510	443
Mimetite ()*	Apatite	Pb₅(AsO₄)₃Cl	191	179	1	46510	1107
Mixite ()*	Mixite	Cu₆Bi(AsO₄)₃(OH)₆·3H₂O	191	179	1	46510	168
Natrojarosite ()*	Alunite	NaFe³⁺₃(SO₄)₂(OH)₆	191	179	1	46506	254
Natrolite ()*	Natrolite	Na₂(Si₃Al₂)O₁₀·2H₂O	191	179	1	46508	1236
Nepheline ()*	Tridymite	Na₃K(Al₄Si₄O₁₆)	191	179	1	46508	884
Orthoclase ()*	Feldspar	K(AlSi₃O₈)	191	179	1	46508	2349
Perovskite ()*	Perovskite	CaTiO₃	191	179	1	46508	495
Petitjeanite ()*	None	Bi₃O(PO₄)₂(OH)	191	179	1	46510	15
Phosphowalpurgite ()*	None	(UO₂)Bi₄O₄(PO₄)₂·2H₂O	191	179	1	46510	3
Phosphuranylite ()*	Phosphuranylite	KCa(H₃O)₃(UO₂)₇(PO₄)₄O₄·8H₂O	191	179	2	46507,46510	182
Preisingerite ()*	None	Bi₃O(AsO₄)₂(OH)	191	179	1	46510	53
Pseudomalachite ()*	None	Cu₅(PO₄)₂(OH)₄	191	179	1	46513	369
Pucherite ()*	Scheelite	Bi(VO₄)	191	179	1	46510	53
Pyrite ()*	Pyrite	FeS₂	191	179	1	46513	39462
Quartz ()*	Quartz	SiO₂	191	179	4	46506,46507,46510,46513	61156
Retgersite ()*	None	Ni(SO₄)·6H₂O	191	179	1	46510	55
Saléeite ()*	None	Mg(UO₂)₂(PO₄)₂(H₂O)₁₀	191	179	2	46507,46510	95
Sanidine ()*	Feldspar	K(AlSi₃O₈)	191	179	1	46508	598
Schreibersite ()*	None	(Fe,Ni)₃P	191	179	1	46512	374
Sillénite ()*	None	Bi₁₂SiO₂₀	191	179	1	46510	26
Sillimanite ()*	Not in a structural group	Al₂SiO₅	191	179	1	46506	1516
Smrkovecite ()*	Atelestite	Bi₂O(OH)(PO₄)	0	0	1	46510	2
Sodalite ()*	Cancrinite-sodalite Sodalite	Na₄(Si₃Al₃)O₁₂Cl	191	179	1	46508	444
Sphalerite ()*	Sphalerite	ZnS	191	179	2	46505,46506	21482
Studtite ()*	None	(UO₂)(O₂)(H₂O)₂·2H₂O	191	179	1	46507	25
Taenite ()*	None	(Ni,Fe)	191	179	1	46512	703
Talc ()*	Clay Talc	Mg₃Si₄O₁₀(OH)₂	191	179	1	46508	3337
Thénardite ()*	None	Na₂(SO₄)	191	179	1	46506	299
Torbernite ()*	None	Cu(UO₂)₂(PO₄)₂·12H₂O	191	179	2	46507,46510	1059
Triplite ()*	Triplite	Mn²⁺₂(PO₄)F	191	179	0		233
Troilite ()*	None	FeS	191	179	1	46512	1044
Uraninite ()*	Fluorite	UO₂	191	179	2	46506,46510	2718
Uranocircite-II ()*	None	Ba(UO₂)₂(PO₄)₂·10H₂O	191	179	1	46510	89
Uranosphaerite ()*	None	Bi(UO₂)O₂(OH)	191	179	1	46507	18
Vivianite ()*	Vivianite	Fe²⁺₃(PO₄)₂·8H₂O	191	179	0		636
Vochtenite ()*	None	Fe²⁺Fe³⁺(UO₂)₄(PO₄)₄(OH)·12-13H₂O	191	179	1	46507	5
Walpurgite ()*	None	Bi₄O₄(UO₂)(AsO₄)₂·2H₂O	191	179	1	46510	38
Weeksite ()*	None	(K)₂(UO₂)₂(Si₅O₁₃)·4H₂O	191	179	1	46507	42
Wollastonite ()*	Wollastonite	CaSiO₃	191	179	1	46507	1247
Yingjiangite ()*	Phosphuranylite	K₂Ca(UO₂)₇(PO₄)₄(OH)₆·6H₂O	191	179	1	46507	9
Zavaritskite ()*	Matlockite	BiOF	191	179	1	46510	26
Zippeite ()*	Zippeite	K₂[(UO₂)₄(SO₄)₂O₂(OH)₂](H₂O)₄	191	179	1	46510	175

Locality Notes from all Ages at Locality:

Age ID	Locality Notes
Giersdorf_00000829	The Zadní Chodov uranium deposit was mined from 1952 to 1992 and was ranked among medium-size uranium deposits in the Bohemian Massif. The totalmine production of low-grade uranium ore (0.195 wt.% U) was 4151 t U. The deposit, which is located in the northern tectonic block of the Bor pluton, was investigated by mine workings down to levels of 1250m in a length of over 2.5 km. The contact with the Moldanubian high-grade metasediments is tectonic, comprising several parallel shear structures to the Zadní Chodov fault,which forms the western boundary of the Bor pluton. Migmatised biotite paragneisses of the Moldanubian Varied Group predominate and they contain intercalations of quartzites, amphibolites, calc-silicate rocks and crystalline limestones. Dykes and bodies of amphibole-biotite tonalites and biotite granites cut the paragneisses. Aplite, pegmatite and lamprophyre dykes occur but are less frequent and are particularly developed above and below large shear zones. Uranium mineralisation is associated with the N-S trending zones of the Zadní Chodov fault in areas of their intersection with NW-SE trending fault structures, which form a NW continuation of the Central fault. The Zadní Chodov shear zone has been verified in an extent exceeding 20 km, its thickness in the middle part reaches 500m, and the dip is 50–75° to the east. This dislocation passes northwards into the Eastern shear zone of the Zadní Chodov deposit. The infill of the shear zones consists of intensely altered and crushed rocks with chlorite-rich and/or clay-mineral-rich assemblages. Uranium mineralisation was concentrated into three shear zones

Age ID

Locality Notes

Giersdorf_00000829

The Zadní Chodov uranium deposit was mined from 1952 to 1992 and was ranked among medium-size uranium deposits in the Bohemian Massif. The totalmine production of low-grade uranium ore (0.195 wt.% U) was 4151 t U. The deposit, which is located in the northern tectonic block of the Bor pluton, was investigated by mine workings down to levels of 1250m in a length of over 2.5 km. The contact with the Moldanubian high-grade metasediments is tectonic, comprising several parallel shear structures to the Zadní Chodov fault,which forms the western boundary of the Bor pluton. Migmatised biotite paragneisses of the Moldanubian Varied Group predominate and they contain intercalations of quartzites, amphibolites, calc-silicate rocks and crystalline limestones. Dykes and bodies of amphibole-biotite tonalites and biotite granites cut the paragneisses. Aplite, pegmatite and lamprophyre dykes occur but are less frequent and are particularly developed above and below large shear zones. Uranium mineralisation is associated with the N-S trending zones of the Zadní Chodov fault in areas of their intersection with NW-SE trending fault structures, which form a NW continuation of the Central fault. The Zadní Chodov shear zone has been verified in an extent exceeding 20 km, its thickness in the middle part reaches 500m, and the dip is 50–75° to the east. This dislocation passes northwards into the Eastern shear zone of the Zadní Chodov deposit. The infill of the shear zones consists of intensely altered and crushed rocks with chlorite-rich and/or clay-mineral-rich assemblages. Uranium mineralisation was concentrated into three shear zones

1 Ages assigned to this locality:

	Excel ID	Max Age (Ma)	Min Age (Ma)	Age as listed in reference	Dating Method	Age Interpret	Prioritized?	Sample Source	Sample Num	Run Num	Age from other Locality	Dated Mineral	Minerals explicitely stated as having this age	Age applies to these Elements	MinDat Locality ID	Dated Locality (Max Age)	Location as listed in reference	Reference	Reference DOI	Reference ID	Age Notes
	Giersdorf_00000829	191	179	185±6	U-Pb	Mesozoic recrystallization of brannerite during the main ore stage.		brannerite			Yes	Brannerite	Brannerite, Coffinite, Uraninite	U	106091	Zadní Chodov (Hinterkotten), Planá U Mariánských Lázní, Tachov District, Plzeň Region, Czech Republic	Zadní Chodov Uranium Deposit	René (2017)	10.1016/j.oregeorev.2016.09.033	OGR81_188	Age of uranium mineralization

Sample	Source Locality	Reference URL

All locality data graciously provided by mindat.org

All age data...