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Pınarbaşı, Besni District, Adıyaman Province, Turkeyi
Regional Level Types
PınarbaşıDeposit
Besni DistrictDistrict
Adıyaman ProvinceProvince
TurkeyCountry

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Latitude & Longitude (WGS84):
37° 34' 15'' North , 37° 39' 7'' East
Latitude & Longitude (decimal):
37.57084,37.65221
GeoHash:
G#:sydv8z96p
GRN:
N26E22
Type:
Deposit
Köppen climate type:
Csa : Hot-summer Mediterranean climate
Nearest Settlements:
PlacePopulationDistance
Araban11,128(2012)16.3km
Besni41,892(2012)22.8km
Gölbaşı28,078(2012)23.7km
Yavuzeli8,170(2012)29.1km
Pazarcık23,850(2010)32.4km
Mindat Locality ID:
425797
Long-form identifier:
mindat:1:2:425797:7
GUID (UUID V4):
0


Abstract of Celebi et al. (2010):

In the near vicinity of the apatite-bearing magnetite deposit of Pınarbaşı Permian-aged Malatya Metamorphites consisting of, from bottom to top, chlorite schists, sericite schists, calcschists and recrystallized limestones cover large areas. These folded and faulted metamorphic rocks, which thrust over the Eocene-aged Maden Complex, underwent one regional metamorphism and one subsequent retrograde metamorphism in the greenschist facies. Mineralizations associated with chlorite-sericite schists are in the form of magnetite-bearing apatite lenses. The ore horizons, which reach a thickness of 15 m and have a north-south strike, dip approximately 30 degrees to the west. In the field, massive, banded and disseminated ore types are distinguished. The most important ore mineral is magnetite. It is followed by hematite, siderite, goethite and specularite. The proportion of the fluorapatite, the most valuable gangue mineral, reaches up to 30% in some places. Quartz, calcite, chlorite and sericite are other common gangue minerals. Rarely, rutile, zircon, monazite and xenotime are also observed. There is a significant positive correlation between Fe, P2O5 and depth. The variograms reveal hole effects which reflect ore rock alternations. Frequency distributions of the elements are logarithmic. Magnetite reserves with an iron content of over 20% Fe are approximately 78 Mt. The average P2O5 concentration of these reserves having an average Fe tenor of 35% is 1.57%. The F concentration of 3.46% in apatite is significant. However, rare earth element (REE) concentration of apatite (900 ppm) and V concentration of magnetite (800 ppm) are low. This deposit defined as classic Kiruna-type sedimentary apatite-bearing magnetite deposit is not considered to be economically mined.

Select Mineral List Type

StandardDetailedGalleryStrunzChemical Elements

Detailed Mineral List:

ⓘ'Apatite'
Formula:Ca5(PO4)3(Cl/F/OH)
ⓘCalcite
Formula:CaCO3
ⓘ'Chlorite Group'
ⓘFluorapatite
Formula:Ca5(PO4)3F
ⓘGoethite
Formula:Fe3+O(OH)
ⓘHematite
Formula:Fe2O3
ⓘHematite var. Specularite
Formula:Fe2O3
ⓘMagnetite
Formula:Fe2+Fe3+2O4
ⓘ'Monazite Group'
Formula:REE(PO4)
ⓘMuscovite
Formula:KAl2(AlSi3O10)(OH)2
ⓘMuscovite var. Sericite
Formula:KAl2(AlSi3O10)(OH)2
ⓘQuartz
Formula:SiO2
ⓘRutile
Formula:TiO2
ⓘSiderite
Formula:FeCO3
ⓘ'Xenotime'
ⓘZircon
Formula:Zr(SiO4)

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 4 - Oxides and Hydroxides
ⓘGoethite4.00.Fe3+O(OH)
ⓘMagnetite4.BB.05Fe2+Fe3+2O4
ⓘHematite4.CB.05Fe2O3
ⓘvar. Specularite4.CB.05Fe2O3
ⓘQuartz4.DA.05SiO2
ⓘRutile4.DB.05TiO2
Group 5 - Nitrates and Carbonates
ⓘCalcite5.AB.05CaCO3
ⓘSiderite5.AB.05FeCO3
Group 8 - Phosphates, Arsenates and Vanadates
ⓘFluorapatite8.BN.05Ca5(PO4)3F
Group 9 - Silicates
ⓘZircon9.AD.30Zr(SiO4)
ⓘMuscovite9.EC.15KAl2(AlSi3O10)(OH)2
ⓘvar. Sericite9.EC.15KAl2(AlSi3O10)(OH)2
Unclassified
ⓘ'Chlorite Group'-
ⓘ'Monazite Group'-REE(PO4)
ⓘ'Xenotime'-
ⓘ'Apatite'-Ca5(PO4)3(Cl/F/OH)

List of minerals for each chemical element

HHydrogen
HⓘGoethiteFe3+O(OH)
HⓘMuscoviteKAl2(AlSi3O10)(OH)2
HⓘMuscovite var.SericiteKAl2(AlSi3O10)(OH)2
HⓘApatiteCa5(PO4)3(Cl/F/OH)
CCarbon
CⓘCalciteCaCO3
CⓘSideriteFeCO3
OOxygen
OⓘCalciteCaCO3
OⓘFluorapatiteCa5(PO4)3F
OⓘGoethiteFe3+O(OH)
OⓘHematiteFe2O3
OⓘMagnetiteFe2+Fe23+O4
OⓘMonazite GroupREE(PO4)
OⓘMuscoviteKAl2(AlSi3O10)(OH)2
OⓘQuartzSiO2
OⓘRutileTiO2
OⓘSideriteFeCO3
OⓘZirconZr(SiO4)
OⓘHematite var.SpeculariteFe2O3
OⓘMuscovite var.SericiteKAl2(AlSi3O10)(OH)2
OⓘApatiteCa5(PO4)3(Cl/F/OH)
FFluorine
FⓘFluorapatiteCa5(PO4)3F
FⓘApatiteCa5(PO4)3(Cl/F/OH)
AlAluminium
AlⓘMuscoviteKAl2(AlSi3O10)(OH)2
AlⓘMuscovite var.SericiteKAl2(AlSi3O10)(OH)2
SiSilicon
SiⓘMuscoviteKAl2(AlSi3O10)(OH)2
SiⓘQuartzSiO2
SiⓘZirconZr(SiO4)
SiⓘMuscovite var.SericiteKAl2(AlSi3O10)(OH)2
PPhosphorus
PⓘFluorapatiteCa5(PO4)3F
PⓘMonazite GroupREE(PO4)
PⓘApatiteCa5(PO4)3(Cl/F/OH)
ClChlorine
ClⓘApatiteCa5(PO4)3(Cl/F/OH)
KPotassium
KⓘMuscoviteKAl2(AlSi3O10)(OH)2
KⓘMuscovite var.SericiteKAl2(AlSi3O10)(OH)2
CaCalcium
CaⓘCalciteCaCO3
CaⓘFluorapatiteCa5(PO4)3F
CaⓘApatiteCa5(PO4)3(Cl/F/OH)
TiTitanium
TiⓘRutileTiO2
FeIron
FeⓘGoethiteFe3+O(OH)
FeⓘHematiteFe2O3
FeⓘMagnetiteFe2+Fe23+O4
FeⓘSideriteFeCO3
FeⓘHematite var.SpeculariteFe2O3
ZrZirconium
ZrⓘZirconZr(SiO4)

Other Regions, Features and Areas containing this locality

Arabian PlateTectonic Plate
AsiaContinent
Indian Plate (India Plate)
Turkey

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References

Celebi, Hüseyin, Helvaci, Cahit, Uçurum, Ali (2010) Apatite-bearing magnetite deposit of Pinarbasi (Adiyaman): Geological, geochemical and economical potential. Bulletin of the Mineral Research and Exploration: 141: 27-52. https://dergipark.org.tr/en/download/article-file/44751
www.getamap.net (n.d.)https://www.getamap.net/maps/turkey/adiyaman/_pinarbasi/
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