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Patrimonio meteorite, Patrimônio, Minas Gerais, Brazili
Regional Level Types
Patrimonio meteoriteMeteorite Fall Location
PatrimônioMunicipality
Minas GeraisState
BrazilCountry

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Key
Latitude & Longitude (WGS84):
19° 31' 59'' South , 48° 34' 0'' West
Latitude & Longitude (decimal):
Meteorite Class:
Meteoritical Society Class:
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Prata19,896 (2012)45.1km
Conceição das Alagoas16,152 (2012)46.3km


Ordinary chondrite (L6)
Fall, 6 August 1950; 2.12 kg, small shower

After detonations at least 20 small stones fell in the village of Patrimônio. The interior of examined specimens are characterized by sparse & usually poorly defined chondrules of various textures largely intergrown with the recrystallized matrix. Chondrules have apparent diameters within a 0.3-1.8 mm range (mean 1.2 mm). Rare instances of devitrified glass are still present in some chondrules. Mineralogically the meteorite consists primarily of olivine, orthopyroxene, and albitic plagioclase accompanied by minor troilite and Fe-Ni metal. Accessory chromite, diopside, and merrillite are also present. Total iron (Fe 21.5 wt%) and major silicate composition [olivine (Fa25), orthopyroxene (Fs20.7)] are characteristic of the L-chondrite geochemical group. Textures, mineralogical equilibration, and lack of primary glass are all consistent with the L6 petrologic type.

The L (relatively low in total iron) ordinary chondrites represent approximately 40% of the witnessed and properly classified meteorite falls. Approximately 70% of the group are classified as petrologic type L6. Patrimonio is one of the 4 Brazilian and 271 worldwide falls which have been classified exactly as 'L6' chondrites (as of June 2016). The main mass has been kept at the Museu Nacional-Universidade (Rio de Janeiro), but a number of very small samples are traded on the internet.

Spelling of meteorite names: Patrimonio meteorite vs. Patrimônio village.

During the past two decades the use of diacritical markers and other language-specific spelling conventions has become common in the recognized official (and unique) names of newly recovered meteorites. However, to prevent confusion official names and their spellings for older meteorites are seldom altered once an official meteorite name has been designated.

Select Mineral List Type

Standard Detailed Strunz Dana Chemical Elements

Mineral List


4 valid minerals.

Meteorite/Rock Types Recorded

Note: this is a very new system on mindat.org and 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:

'Albite-Anorthite Series'
Description: Composition of Plagioclase (An11.3Ab82.1Or6.8)
Reference: Gomes, C.B. & Keil, K. (1980) Brazilian Stony Meteorites: University of New Mexico Press: Albuquerque. pp. 162.
Chromite
Formula: Fe2+Cr3+2O4
Reference: Gomes, C.B. & Keil, K. (1980) Brazilian Stony Meteorites: University of New Mexico Press: Albuquerque. pp. 162.
Diopside
Formula: CaMgSi2O6
Description: Composition of Diopside (Fs8.5En47.6Or6.6) according to Gomes & Keil (1980).
Reference: Gomes, C.B. & Keil, K. (1980) Brazilian Stony Meteorites: University of New Mexico Press: Albuquerque. pp. 162.
'Fayalite-Forsterite Series'
Description: Olivine (Fa24.8) Range Fa~24.0-25.4 reported by Gomes & Keil,1980. Also, Fa25 reported by Mason,1963.
Reference: Mason, B. (1963) Olivine in ordinary chondrites. Geochimica et Cosmochimica Acta 27(9): 1011-1023. (Sept 1963).; Gomes, C.B. & Keil, K. (1980) Brazilian Stony Meteorites: University of New Mexico Press: Albuquerque. pp. 162.
Merrillite
Formula: Ca9NaMg(PO4)7
Reference: Gomes, C.B. & Keil, K. (1980) Brazilian Stony Meteorites: University of New Mexico Press: Albuquerque. pp. 162.
'Meteoritic Iron'
Reference: Gomes, C.B. & Keil, K. (1980) Brazilian Stony Meteorites: University of New Mexico Press: Albuquerque. pp. 162.
'Orthopyroxene Subgroup'
Reference: Gomes, C.B. & Keil, K. (1980) Brazilian Stony Meteorites: University of New Mexico Press: Albuquerque. pp. 162.
Troilite
Formula: FeS
Reference: Gomes, C.B. & Keil, K. (1980) Brazilian Stony Meteorites: University of New Mexico Press: Albuquerque. pp. 162.

List of minerals arranged by Strunz 10th Edition classification

Group 2 - Sulphides and Sulfosalts
Troilite2.CC.10FeS
Group 4 - Oxides and Hydroxides
Chromite4.BB.05Fe2+Cr3+2O4
Group 8 - Phosphates, Arsenates and Vanadates
Merrillite8.AC.45Ca9NaMg(PO4)7
Group 9 - Silicates
Diopside9.DA.15CaMgSi2O6
Unclassified Minerals, Rocks, etc.
'Albite-Anorthite Series'-
'Fayalite-Forsterite Series'-
'Meteoritic Iron'-
'Orthopyroxene Subgroup'-

List of minerals arranged by Dana 8th Edition classification

Group 2 - SULFIDES
AmXp, with m:p = 1:1
Troilite2.8.9.1FeS
Group 7 - MULTIPLE OXIDES
AB2X4
Chromite7.2.3.3Fe2+Cr3+2O4
Group 38 - ANHYDROUS NORMAL PHOSPHATES, ARSENATES, AND VANADATES
(AB)3(XO4)2
Merrillite38.3.4.4Ca9NaMg(PO4)7
Group 65 - INOSILICATES Single-Width,Unbranched Chains,(W=1)
Single-Width Unbranched Chains, W=1 with chains P=2
Diopside65.1.3a.1CaMgSi2O6
Unclassified Minerals, Mixtures, etc.
'Albite-Anorthite Series'-
'Fayalite-Forsterite Series'-
'Meteoritic Iron'-
'Orthopyroxene Subgroup'-

List of minerals for each chemical element

OOxygen
O ChromiteFe2+Cr23+O4
O DiopsideCaMgSi2O6
O MerrilliteCa9NaMg(PO4)7
NaSodium
Na MerrilliteCa9NaMg(PO4)7
MgMagnesium
Mg DiopsideCaMgSi2O6
Mg MerrilliteCa9NaMg(PO4)7
SiSilicon
Si DiopsideCaMgSi2O6
PPhosphorus
P MerrilliteCa9NaMg(PO4)7
SSulfur
S TroiliteFeS
CaCalcium
Ca DiopsideCaMgSi2O6
Ca MerrilliteCa9NaMg(PO4)7
CrChromium
Cr ChromiteFe2+Cr23+O4
FeIron
Fe ChromiteFe2+Cr23+O4
Fe TroiliteFeS

References

Sort by

Year (asc) Year (desc) Author (A-Z) Author (Z-A)
Krinov, E. L. - Editor (1958) The Meteoritical Bulletin, No. 8. Moscow.
Mason, B. (1963) Olivine in ordinary chondrites. Geochimica et Cosmochimica Acta 27(9): 1011-1023. (Sept 1963).
Gomes, C.B. & Keil, K. (1980) Brazilian Stony Meteorites: University of New Mexico Press: Albuquerque. pp. 162.
Grady, M.M (2000). Catalogue of Meteorites (5/e). Cambridge University Press: Cambridge; New York; Oakleigh; Madrid; Cape Town. 689 pages.

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