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Conselheiro Pena pegmatite district, Conselheiro Pena, Minas Gerais, Brazili
Regional Level Types
Conselheiro Pena pegmatite districtPegmatite Field
Conselheiro PenaTown
Minas GeraisState
BrazilCountry

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Latitude & Longitude (WGS84):
19° 10' 23'' South , 41° 28' 20'' West
Latitude & Longitude (decimal):
KΓΆppen climate type:
Mindat Locality ID:
394
Long-form identifier:
mindat:1:2:394:9
GUID (UUID V4):
b20667d7-af6e-437f-ae75-af1065144cff


The Conselheiro Pena Pegmatite District lies 50-100 km southeast of Governador Valadares where it stretches about 110 km from SW to NE.

The district includes more than 205 pegmatites that have been mined.

Over 50 minerals have been found in the district, including much gem-quality tourmaline, aquamarine, morganite, and kunzite besides industrial materials such as K-feldspar, albite, mica, and beryl ore.

Many of the pegmatites are rich in phosphates, including the primary triphylite and montebrasite, and more than a dozen secondary phosphates for which the district is best known, most notably brazilianite and variscite.

The district is also known for red rubellite and multi-color elbaite including blue-caps.

Today the Conselheiro Pena pegmatites are mined mostly for industrial feldspar (mainly microcline), plus minerals for collectors.

Tectonically, the Conselheiro Pena Pegmatite District lies within the Araçuaí Orogen, a structurally complex crustal segment created when two microcontinents collided during the Brasiliano Orogeny to form a portion of the southern supercontinent of Gondwana.

Two-mica granites of the Urucum suite were generated during that orogeny at ca. 582 Ma, and pegmatites evolved by fractional crystallization from those.

Most pegmatite bodies in the district are tabular or lenticular, but a few are tear-drop shaped.

The pegmatites solidified at a temperature of about 600 degrees C and under pressures of 4-5 kbar, corresponding to depths of 12-15 km (Nalini et al., 2015).

They intruded mostly along steeply-dipping strike-slip shear zones in the metamorphics of the Rio Doce Group.

These rocks include sillimanite-staurolite-garnet-mica schist with interbedded marble, metawackes, and metaquartzites that were originally marine sedimentary rocks deposited in a narrow seaway that once separated the two colliding microcontinents.

NK, rev. December 2017

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


17 valid minerals.

Rock Types Recorded

Note: data is currently VERY limited. Please bear with us while we work towards adding this information!

Select Rock List Type

Alphabetical List Tree Diagram

Detailed Mineral List:

β“˜ Albite
Formula: Na(AlSi3O8)
β“˜ 'Apatite'
Formula: Ca5(PO4)3(Cl/F/OH)
β“˜ Beraunite
Formula: Fe3+6(PO4)4O(OH)4 · 6H2O
β“˜ Bermanite
Formula: Mn2+Mn3+2(PO4)2(OH)2 · 4H2O
β“˜ Borocookeite
Formula: (LiAl4◻)[BSi3O10](OH)8
References:
β“˜ Brazilianite
Formula: NaAl3(PO4)2(OH)4
β“˜ Cookeite
Formula: (LiAl4◻)[AlSi3O10](OH)8
β“˜ Euclase
Formula: BeAl(SiO4)(OH)
β“˜ Hureaulite
Formula: Mn2+5(PO3OH)2(PO4)2 · 4H2O
β“˜ Laueite
Formula: Mn2+Fe3+2(PO4)2(OH)2 · 8H2O
β“˜ Muscovite
Formula: KAl2(AlSi3O10)(OH)2
β“˜ Phosphosiderite
Formula: FePO4 · 2H2O
β“˜ Rockbridgeite
Formula: Fe2+Fe3+4(PO4)3(OH)5
β“˜ Siderite
Formula: FeCO3
β“˜ Stewartite
Formula: Mn2+Fe3+2(PO4)2(OH)2 · 8H2O
β“˜ Strengite
Formula: FePO4 · 2H2O
β“˜ Strunzite
Formula: Mn2+Fe3+2(PO4)2(OH)2 · 6H2O
β“˜ Titanite ?
Formula: CaTi(SiO4)O
β“˜ 'Tourmaline'
Formula: AD3G6 (T6O18)(BO3)3X3Z

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 5 - Nitrates and Carbonates
β“˜Siderite5.AB.05FeCO3
Group 8 - Phosphates, Arsenates and Vanadates
β“˜Rockbridgeite8.BC.10Fe2+Fe3+4(PO4)3(OH)5
β“˜Brazilianite8.BK.05NaAl3(PO4)2(OH)4
β“˜Hureaulite8.CB.10Mn2+5(PO3OH)2(PO4)2 Β· 4H2O
β“˜Phosphosiderite8.CD.05FePO4 Β· 2H2O
β“˜Strengite8.CD.10FePO4 Β· 2H2O
β“˜Bermanite8.DC.20Mn2+Mn3+2(PO4)2(OH)2 Β· 4H2O
β“˜Strunzite8.DC.25Mn2+Fe3+2(PO4)2(OH)2 Β· 6H2O
β“˜Beraunite8.DC.27Fe3+6(PO4)4O(OH)4 Β· 6H2O
β“˜Laueite8.DC.30Mn2+Fe3+2(PO4)2(OH)2 Β· 8H2O
β“˜Stewartite8.DC.30Mn2+Fe3+2(PO4)2(OH)2 Β· 8H2O
Group 9 - Silicates
β“˜Euclase9.AE.10BeAl(SiO4)(OH)
β“˜Titanite ?9.AG.15CaTi(SiO4)O
β“˜Muscovite9.EC.15KAl2(AlSi3O10)(OH)2
β“˜Borocookeite9.EC.55(LiAl4β—»)[BSi3O10](OH)8
β“˜Cookeite9.EC.55(LiAl4β—»)[AlSi3O10](OH)8
β“˜Albite9.FA.35Na(AlSi3O8)
Unclassified
β“˜'Tourmaline'-AD3G6 (T6O18)(BO3)3X3Z
β“˜'Apatite'-Ca5(PO4)3(Cl/F/OH)

List of minerals for each chemical element

HHydrogen
Hβ“˜ BerauniteFe63+(PO4)4O(OH)4 · 6H2O
Hβ“˜ BermaniteMn2+Mn23+(PO4)2(OH)2 · 4H2O
Hβ“˜ BrazilianiteNaAl3(PO4)2(OH)4
Hβ“˜ Cookeite(LiAl4◻)[AlSi3O10](OH)8
Hβ“˜ EuclaseBeAl(SiO4)(OH)
Hβ“˜ HureauliteMn52+(PO3OH)2(PO4)2 · 4H2O
Hβ“˜ LaueiteMn2+Fe23+(PO4)2(OH)2 · 8H2O
Hβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Hβ“˜ PhosphosideriteFePO4 · 2H2O
Hβ“˜ RockbridgeiteFe2+Fe43+(PO4)3(OH)5
Hβ“˜ StewartiteMn2+Fe23+(PO4)2(OH)2 · 8H2O
Hβ“˜ StrengiteFePO4 · 2H2O
Hβ“˜ StrunziteMn2+Fe23+(PO4)2(OH)2 · 6H2O
Hβ“˜ Borocookeite(LiAl4◻)[BSi3O10](OH)8
Hβ“˜ ApatiteCa5(PO4)3(Cl/F/OH)
LiLithium
Liβ“˜ Cookeite(LiAl4◻)[AlSi3O10](OH)8
Liβ“˜ Borocookeite(LiAl4◻)[BSi3O10](OH)8
BeBeryllium
Beβ“˜ EuclaseBeAl(SiO4)(OH)
BBoron
Bβ“˜ TourmalineAD3G6 (T6O18)(BO3)3X3Z
Bβ“˜ Borocookeite(LiAl4◻)[BSi3O10](OH)8
CCarbon
Cβ“˜ SideriteFeCO3
OOxygen
Oβ“˜ AlbiteNa(AlSi3O8)
Oβ“˜ BerauniteFe63+(PO4)4O(OH)4 · 6H2O
Oβ“˜ BermaniteMn2+Mn23+(PO4)2(OH)2 · 4H2O
Oβ“˜ BrazilianiteNaAl3(PO4)2(OH)4
Oβ“˜ Cookeite(LiAl4◻)[AlSi3O10](OH)8
Oβ“˜ EuclaseBeAl(SiO4)(OH)
Oβ“˜ HureauliteMn52+(PO3OH)2(PO4)2 · 4H2O
Oβ“˜ LaueiteMn2+Fe23+(PO4)2(OH)2 · 8H2O
Oβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Oβ“˜ PhosphosideriteFePO4 · 2H2O
Oβ“˜ RockbridgeiteFe2+Fe43+(PO4)3(OH)5
Oβ“˜ SideriteFeCO3
Oβ“˜ StewartiteMn2+Fe23+(PO4)2(OH)2 · 8H2O
Oβ“˜ StrengiteFePO4 · 2H2O
Oβ“˜ StrunziteMn2+Fe23+(PO4)2(OH)2 · 6H2O
Oβ“˜ TitaniteCaTi(SiO4)O
Oβ“˜ TourmalineAD3G6 (T6O18)(BO3)3X3Z
Oβ“˜ Borocookeite(LiAl4◻)[BSi3O10](OH)8
Oβ“˜ ApatiteCa5(PO4)3(Cl/F/OH)
FFluorine
Fβ“˜ ApatiteCa5(PO4)3(Cl/F/OH)
NaSodium
Naβ“˜ AlbiteNa(AlSi3O8)
Naβ“˜ BrazilianiteNaAl3(PO4)2(OH)4
AlAluminium
Alβ“˜ AlbiteNa(AlSi3O8)
Alβ“˜ BrazilianiteNaAl3(PO4)2(OH)4
Alβ“˜ Cookeite(LiAl4◻)[AlSi3O10](OH)8
Alβ“˜ EuclaseBeAl(SiO4)(OH)
Alβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Alβ“˜ Borocookeite(LiAl4◻)[BSi3O10](OH)8
SiSilicon
Siβ“˜ AlbiteNa(AlSi3O8)
Siβ“˜ Cookeite(LiAl4◻)[AlSi3O10](OH)8
Siβ“˜ EuclaseBeAl(SiO4)(OH)
Siβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Siβ“˜ TitaniteCaTi(SiO4)O
Siβ“˜ Borocookeite(LiAl4◻)[BSi3O10](OH)8
PPhosphorus
Pβ“˜ BerauniteFe63+(PO4)4O(OH)4 · 6H2O
Pβ“˜ BermaniteMn2+Mn23+(PO4)2(OH)2 · 4H2O
Pβ“˜ BrazilianiteNaAl3(PO4)2(OH)4
Pβ“˜ HureauliteMn52+(PO3OH)2(PO4)2 · 4H2O
Pβ“˜ LaueiteMn2+Fe23+(PO4)2(OH)2 · 8H2O
Pβ“˜ PhosphosideriteFePO4 · 2H2O
Pβ“˜ RockbridgeiteFe2+Fe43+(PO4)3(OH)5
Pβ“˜ StewartiteMn2+Fe23+(PO4)2(OH)2 · 8H2O
Pβ“˜ StrengiteFePO4 · 2H2O
Pβ“˜ StrunziteMn2+Fe23+(PO4)2(OH)2 · 6H2O
Pβ“˜ ApatiteCa5(PO4)3(Cl/F/OH)
ClChlorine
Clβ“˜ ApatiteCa5(PO4)3(Cl/F/OH)
KPotassium
Kβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
CaCalcium
Caβ“˜ TitaniteCaTi(SiO4)O
Caβ“˜ ApatiteCa5(PO4)3(Cl/F/OH)
TiTitanium
Tiβ“˜ TitaniteCaTi(SiO4)O
MnManganese
Mnβ“˜ BermaniteMn2+Mn23+(PO4)2(OH)2 · 4H2O
Mnβ“˜ HureauliteMn52+(PO3OH)2(PO4)2 · 4H2O
Mnβ“˜ LaueiteMn2+Fe23+(PO4)2(OH)2 · 8H2O
Mnβ“˜ StewartiteMn2+Fe23+(PO4)2(OH)2 · 8H2O
Mnβ“˜ StrunziteMn2+Fe23+(PO4)2(OH)2 · 6H2O
FeIron
Feβ“˜ BerauniteFe63+(PO4)4O(OH)4 · 6H2O
Feβ“˜ LaueiteMn2+Fe23+(PO4)2(OH)2 · 8H2O
Feβ“˜ PhosphosideriteFePO4 · 2H2O
Feβ“˜ RockbridgeiteFe2+Fe43+(PO4)3(OH)5
Feβ“˜ SideriteFeCO3
Feβ“˜ StewartiteMn2+Fe23+(PO4)2(OH)2 · 8H2O
Feβ“˜ StrengiteFePO4 · 2H2O
Feβ“˜ StrunziteMn2+Fe23+(PO4)2(OH)2 · 6H2O

Other Regions, Features and Areas containing this locality

South AmericaContinent
South America PlateTectonic Plate

This page contains all mineral locality references listed on mindat.org. This does not claim to be a complete list. If you know of more minerals from this site, please register so you can add to our database. This locality information is for reference purposes only. You should never attempt to visit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holders for access and that you are aware of all safety precautions necessary.

References

 
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