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:
Shaft No. III, Komló, Mecsek Mts, Baranya, Hungary

Oldest recorded age at locality: 259.1
Youngest recorded age at locality: 201.3

mindat Locality ID: 106114
mindat URL: http://www.mindat.org/loc-106114.html

Tectonic Settings:

Total number of sublocalities beneath "Shaft No. III, Komló, Mecsek Mts, Baranya, Hungary": 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.

Adranosite	Alum	Arcanite	Hexahydrite	Langbeinite	Metavoltine	None	Picromerite	Sabieite	Sulphur

Adranosite-(Fe) ()*	Alum-(K) ()*	Clairite ()*	Efremovite ()*	Hexahydrite ()*
Mascagnite ()*	Metavoltine ()*	Mohrite ()*	Sabieite ()*	Salammoniac ()*
Sulphur ()*	Tschermigite ()*

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 Cl Fe H K Mg N Na O S

Elements from minerals reported directly at this locality: Al Cl Fe H K Mg N Na O S

Structural Groups for minerals in this locality:
Adranosite Alum Arcanite Hexahydrite Langbeinite Metavoltine None Picromerite Sabieite Sulphur

12 IMA Minerals at location:

Mineral name	Structural Groups	IMA Formula	Max Age (Ma)	Min Age (Ma)	# of localities containing mineral
Adranosite-(Fe) ()*	Adranosite	(NH₄)₄NaFe₂(SO₄)₄Cl(OH)₂	259.1	201.3	6
Alum-(K) ()*	Alum	KAl(SO₄)₂·12H₂O	259.1	201.3	92
Clairite ()*	None	(NH₄)₂Fe³⁺₃(SO₄)₄(OH)₃·3H₂O	259.1	201.3	8
Efremovite ()*	Langbeinite	(NH₄)₂Mg₂(SO₄)₃	259.1	201.3	13
Hexahydrite ()*	Hexahydrite	Mg(SO₄)·6H₂O	259.1	201.3	251
Mascagnite ()*	Arcanite	(NH₄)₂(SO₄)	259.1	201.3	61
Metavoltine ()*	Metavoltine	K₂Na₆Fe²⁺Fe³⁺₆O₂(SO₄)₁₂·18H₂O	259.1	201.3	78
Mohrite ()*	Picromerite	(NH₄)₂Fe²⁺(SO₄)₂·6H₂O	259.1	201.3	18
Sabieite ()*	Sabieite	(NH₄)Fe³⁺(SO₄)₂	259.1	201.3	9
Salammoniac ()*	None	(NH₄)Cl	259.1	201.3	105
Sulphur ()*	Sulphur	S	259.1	201.3	2045
Tschermigite ()*	Alum	(NH₄)Al(SO₄)₂·12H₂O	259.1	201.3	81

Locality Notes from all Ages at Locality:

Age ID	Locality Notes
Giersdorf_00000859	In the second part of the 20th century the Mecsek Mts were the target of intensive mineral exploration due to the Permian uranium mineralization of the Kővágószőlős Sandstone. The mining was discontinued in the 1980s; however, in the 1990s the western part of the mountains became a focus of interest once again due to the presence of a possible high level radioactive waste disposal site in the Permian Boda Siltstone Formation
Giersdorf_00000860	In the second part of the 20th century the Mecsek Mts were the target of intensive mineral exploration due to the Permian uranium mineralization of the Kővágószőlős Sandstone. The mining was discontinued in the 1980s; however, in the 1990s the western part of the mountains became a focus of interest once again due to the presence of a possible high level radioactive waste disposal site in the Permian Boda Siltstone Formation

Age ID

Locality Notes

Giersdorf_00000859

In the second part of the 20th century the Mecsek Mts were the target of intensive mineral exploration due to the Permian uranium mineralization of the Kővágószőlős Sandstone. The mining was discontinued in the 1980s; however, in the 1990s the western part of the mountains became a focus of interest once again due to the presence of a possible high level radioactive waste disposal site in the Permian Boda Siltstone Formation

Giersdorf_00000860

2 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_00000859	259.1	251.9	Upper Permian							Yes				12683	Kővágószőlős, Mecsek Mts, Baranya, Hungary	Kővágószőlős	Magyar et al. (2016)		FK146_223	The age of the Kővágószőlős Sandstone is described in the literature as Upper Permian in age.
	Giersdorf_00000860	251.9	201.3	Lower Triassic							Yes				12683	Kővágószőlős, Mecsek Mts, Baranya, Hungary	Kővágószőlős	Magyar et al. (2016)		FK146_223	The age of the uppermost member of the Kővágószőlős formation is described as being Triassic in age due to the presence of specific sporomorphs.

Sample	Source Locality	Reference URL

All locality data graciously provided by mindat.org

All age data...