Help mindat.org|Log In|Register|
Home PageMindat NewsThe Mindat ManualHistory of MindatCopyright StatusManagement TeamContact UsAdvertise on Mindat
Donate to MindatSponsor a PageSponsored PagesTop Available PagesMindat AdvertisersAdvertise on Mindat
Minerals by PropertiesMinerals by ChemistryAdvanced Locality SearchRandom MineralSearch by minIDLocalities Near MeSearch ArticlesSearch GlossaryMore Search Options
Search For:
Mineral Name:
Locality Name:
Keyword(s):
 
The Mindat ManualAdd a New PhotoRate PhotosLocality Edit ReportCoordinate Completion ReportAdd Glossary Item
StatisticsThe ElementsMember ListBooks & MagazinesMineral Shows & EventsThe Mindat DirectoryHow to Link to MindatDevice Settings
Photo SearchPhoto GalleriesNew Photos TodayNew Photos YesterdayMembers' Photo GalleriesPast Photo of the Day Gallery

Sapucaia mine (Proberil mine), Sapucaia do Norte, Galiléia, Minas Gerais, Brazil

This page is currently not sponsored. Click here to sponsor this page.
 
Latitude & Longitude (WGS84): 18° 54' 2'' South , 41° 29' 3'' West
Latitude & Longitude (decimal): -18.90083,-41.48444
Köppen climate type:Aw : Tropical savanna, wet


The Sapucaia mine is approximately 60 km due east of Governador Valadares, and 16 km ENE of Galiléia. It lies within the Conselheiro Pena Pegmatite District of the Eastern Brazilian Pegmatite Province. Mining began in the early part of the 20th century, but the time of greatest activity was during the Second World War when the mine produced industrial beryl and muscovite. It still produces feldspar and rare minerals for collectors.

The Sapucaia Pegmatite intrudes garnet-staurolite-muscovite-biotite schists of the São Tomé Formation (Rio Doce Group) and sericite quartzites of the Crenaque Group, all of Neoproterozoic age. The pegmatite forms a lenticular body elongated in a NW-SE direction and dips at about 70 degrees to the NE. Weathering processes and the introduction of metasomatic fluids led to the formation of many secondary phosphates. The pegmatite is lithium-rich and is the type locality for eight minerals, all of them phosphates. Among collectors, the mine is best-known for the phosphates (especially iron-rich ones) and rose quartz. It is NOT known for any tourmaline group mineral or any variety of beryl or spodumene.

(Modified by NK, September 2016.)

Mineral List

Albite

var: Cleavelandite

Almandine

Althausite

Arrojadite-(PbFe) (TL)

Arsenopyrite

Augelite

Autunite

Barbosalite (TL)

Beraunite

Berlinite

Bermanite

Beryl

var: Heliodor

'Biotite'

Cacoxenite

Chamosite

Childrenite

'Clays'

'Columbite-Tantalite'

Crandallite

Cryptomelane

Cyrilovite

Dufrénite

Elbaite

Eleonorite

Eosphorite

Faheyite (TL)

Fairfieldite

Ferrisicklerite

Fluorapatite

Frondelite (TL)

'Frondelite-Rockbridgeite Series'

'Garnet'

Gayite

Goethite

Gordonite

Greifensteinite

'Gummite'

Hematite

Heterosite

Hureaulite

Hydroxylherderite

Jahnsite-(CaMnFe)

'Jahnsite Group'

'Jahnsite-(MnMnMg)'

Johnsomervilleite

Kaolinite

Kidwellite

Laueite

Leucophosphite

'Limonite'

Lipscombite (TL)

Lithiophorite

Löllingite

Ludlamite

Magnetite

Messelite

Metaswitzerite

Metavivianite

'Meurigite'

Meurigite-K

Microcline

Mitridatite

Monazite-(Ce)

Montebrasite

Montmorillonite

Moraesite (TL)

Muscovite

Natrodufrénite

Nontronite

Opal

var: Opal-AN

Paravauxite

Pharmacosiderite

Phosphosiderite

Phosphuranylite

Pyrite

Quartz

var: Chalcedony

var: Smoky Quartz

Robertsite

Rockbridgeite

Roscherite

Ruifrancoite (TL)

Rutherfordine

Sabugalite

Saléeite

Schorl

Scorodite

Serrabrancaite

Siderite

Sphalerite

Spodumene

Strengite

Strunzite

Tapiolite-(Fe)

Tavorite (TL)

'Tourmaline'

Triphylite

Variscite

Vivianite

Wardite

Wavellite

Whiteite-(CaMnMg)

'Whiteite Group' ?

Whiteite-(MnFeMg)

Whiteite-(MnMnMg)

Whitmoreite

Xanthoxenite

Xenotime-(Y)

Zanazziite

Zircon


96 valid minerals. 8 (TL) - type locality of valid minerals.

Regional Geology

This geological map and associated information on rock units at or nearby to the coordinates given for this locality is based on relatively small scale geological maps provided by various national Geological Surveys. This does not necessarily represent the complete geology at this locality but it gives a background for the region in which it is found.

Click on geological units on the map for more information. Click here to view full-screen map on Macrostrat.org

Neoproterozoic
541 - 1000 Ma



ID: 1383569
Neoproterozoic plutonic rocks

Age: Neoproterozoic (541 - 1000 Ma)

Comments: Deep-seated to high-level intrusions are included. Many charnockites, anorthosites, and large ophiolites, classified as plutons, are distinguished in the database using the SIGNIF item. Ophiolites were classified as plutons, even where remnants may be extrusive and/or sedimentary.

Lithology: Plutonic rocks

Reference: Geological Survey of Canada. Generalized geological map of the world and linked databases. doi:10.4095/195142. Open File 2915d. [18]

Data and map coding provided by Macrostrat.org, used under Creative Commons Attribution 4.0 License



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

Lindberg, M. L. (1949) Frondelite and the frondelite-rockbridgeite series. American Mineralogist. 34, 541-549.

Lindberg & Murata (1953) Faheyite, a new phosphate mineral from the Sapucaia pegmatite mine, Minas Gerais, Brazil. American Mineralogist. 38, 263-270, 349.

Science (1954) 119: 739.

Lindberg, M.L. and Pecora, W.T. (1955) Tavorite and barbosalite, two new phosphate minerals from Minas Gerais, Brazil. American Mineralogist 40, 952-966.

Rocks & Minerals: 62: 318.

Rocks & Minerals: 63: 44 & 139.

Mineralogical Record: 21: 97.

Cassedanne, J.P. & Baptista, A. (1999) Famous Mineral Localities: The Sapucaia Pegmatite Minas Gerais, Brazil. Mineralogical Record, 30: 347-360 + 365.

Herminio, Jr., A. N., Bilal, E., and Neves, J. M. (2000) Syn-collisional peraluminous magmatism in the Rio Doce region: mineralogy, geochemistry and isotopic data of the Neoproterozoic Urucum Suite (Eastern Minas Gerais State, Brazil): Revista Brasileira de Geociências, v. 30, p. 120-125.

Chopin, C., Oberti, R., Cámara, F. (2006) The arrojadite enigma: II. Compositional space, new members and nomenclature of the group. American Mineralogist, 91, 1260-1270 [with discussion and analysis of arrojadite-(PbFe) from Sapucaia].

Atencio, K., Chukanov, N. V., Coutinho, J. M.V., Menezes Filho, L.A.D., Dubinchuk, V. T. & Möckel, S. (2007) Ruifrancoite, a new Fe3+-dominant monoclinic member of the roscherite group from Galileia, Minas Gerais, Brazil. Canadian Mineralogist. 45, 1263-1273.

Pedrosa-Soares, A., Chaves, M., and Scholz, R. (2009) Eastern Brazilian Pegmatite Province: 4th International Symposium on Granitic Pegmatites, Field Trip Guide, p. 1-28. (pdf on-line at http://www.researchgate.net/publication/234037120_Eastern_Brazilian_Pegmatite_Province).

Baijot, M., Hatert, F. & Philippo, S. (2012) Mineralogy and geochemistry of phosphates and silicates in the Sapucaia pegmatite, Minas Gerais, Brazil: Genetic implications. Canadian Mineralogist. 50, 1531-1554.

Mineral and/or Locality  
Mindat.org is an outreach project of the Hudson Institute of Mineralogy, a 501(c)(3) not-for-profit organization.
Copyright © mindat.org and the Hudson Institute of Mineralogy 1993-2017, except where stated. Mindat.org relies on the contributions of thousands of members and supporters.
Privacy Policy - Terms & Conditions - Contact Us Current server date and time: October 23, 2017 18:13:24 Page generated: October 17, 2017 17:29:18
Go to top of page