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โ‡ฑ Narellan meteorite, Camden County, New South Wales, Australia


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Narellan meteorite, Camden County, New South Wales, Australiai
Regional Level Types
Narellan meteoriteMeteorite Fall Location
Camden CountyCounty
New South WalesState
AustraliaCountry

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Latitude & Longitude (WGS84):
34ยฐ 2' 59'' South , 150ยฐ 41' 29'' East
Latitude & Longitude (decimal):
Kรถppen climate type:
Nearest Settlements:
PlacePopulationDistance
Elderslie4,252 (2018)2.1km
Brownlow Hill379 (2012)2.9km
Camden South4,343 (2015)3.7km
Narellan7,350 (2018)3.8km
Cobbitty1,162 (2015)4.0km
Nearest Clubs:
Local clubs are the best way to get access to collecting localities
ClubLocationDistance
Campbelltown and Districts Lapidary ClubIngleburn, New South Wales17km
Fairfield & Districts Gemstone ClubWakeley, New South Wales28km
Nepean District Lapidary Club IncSt Marys, New South Wales32km
Bankstown and Districts Lapidary Club IncBankstown, New South Wales34km
Rooty Hill and District Lapidary ClubRooty Hill , New South Wales34km
Mindat Locality ID:
294605
Long-form identifier:
mindat:1:2:294605:7
GUID (UUID V4):
0


Ordinary chondrite (L6)
Fell, 8 April 1928, 17:15 hrs; 367.5 g

A small stone fell and was recovered. Olivine (Fa25.3) and low Ca-orthopyroxene (Fs21.4) compositions are characteristic of the L-chondrite geochemical group. Mineralogically the meteorite consists primarily of olivine and orthopyroxene accompanied by minor albitic plagioclase, troilite, and Fe-Ni metal. Accessory chromite and other minor opaques (copper, ilmenite and isocubanite) have also been reported. Chemical analysis suggests that other mineral phases may also be present. However, in the mid 20th century such phases would not always have been readily detected โ€” even with larger meteorites โ€” using the destructive wet-chemical techniques used in decades following the meteorite's fall. Chromite aggregates appear to be the product of pre-terrestrial shock. A Pb,Th:He gas release age of 3.21 Ga is probably another indication of at least one major post-formational collision.

The L-group of ordinary chondrites (relatively low in total iron) are the largest group of classified witnessed meteorite falls and account for ~45% of all well-classified meteorite falls. The L6 petrologic type account for ~ 70% of the group. 272 meteorite falls are currently classified exactly as 'L6' chondrites [June 2017].

189 g, approximately half of the original mass, has been kept at the Australian Museum in Sydney.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


7 valid minerals.

Meteorite/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:

โ“˜ Chromite
Formula: Fe2+Cr3+2O4
Description: Shock-produced chromite aggregates present.
โ“˜ 'Fayalite-Forsterite Series'
Description: Olivine composition [Fa25.3] @Mason,1974,
โ“˜ Ilmenite
Formula: Fe2+TiO3
โ“˜ Isocubanite
Formula: CuFe2S3
โ“˜ Native Copper
Formula: Cu
โ“˜ Native Iron
Formula: Fe
โ“˜ Native Iron var. Kamacite
Formula: (Fe,Ni)
โ“˜ 'Orthopyroxene Subgroup'
Description: Orthopyroxene composition [Fs21.4] @Mason,1974.
โ“˜ 'Plagioclase'
Formula: (Na,Ca)[(Si,Al)AlSi2]O8
โ“˜ Taenite
Formula: (Fe,Ni)
โ“˜ Troilite
Formula: FeS

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
โ“˜Native Copper1.AA.05Cu
โ“˜Native Iron1.AE.05Fe
โ“˜var. Kamacite1.AE.05(Fe,Ni)
โ“˜Taenite1.AE.10(Fe,Ni)
Group 2 - Sulphides and Sulfosalts
โ“˜Isocubanite2.CB.55bCuFe2S3
โ“˜Troilite2.CC.10FeS
Group 4 - Oxides and Hydroxides
โ“˜Chromite4.BB.05Fe2+Cr3+2O4
โ“˜Ilmenite4.CB.05Fe2+TiO3
Unclassified
โ“˜'Fayalite-Forsterite Series'-
โ“˜'Plagioclase'-(Na,Ca)[(Si,Al)AlSi2]O8
โ“˜'Orthopyroxene Subgroup'-

List of minerals for each chemical element

OOxygen
Oโ“˜ ChromiteFe2+Cr23+O4
Oโ“˜ IlmeniteFe2+TiO3
Oโ“˜ Fayalite-Forsterite Series
Oโ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
NaSodium
Naโ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
MgMagnesium
Mgโ“˜ Fayalite-Forsterite Series
AlAluminium
Alโ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
SiSilicon
Siโ“˜ Fayalite-Forsterite Series
Siโ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
SSulfur
Sโ“˜ IsocubaniteCuFe2S3
Sโ“˜ TroiliteFeS
CaCalcium
Caโ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
TiTitanium
Tiโ“˜ IlmeniteFe2+TiO3
CrChromium
Crโ“˜ ChromiteFe2+Cr23+O4
FeIron
Feโ“˜ ChromiteFe2+Cr23+O4
Feโ“˜ IlmeniteFe2+TiO3
Feโ“˜ Native IronFe
Feโ“˜ IsocubaniteCuFe2S3
Feโ“˜ Native Iron var. Kamacite(Fe,Ni)
Feโ“˜ Taenite(Fe,Ni)
Feโ“˜ TroiliteFeS
Feโ“˜ Fayalite-Forsterite Series
NiNickel
Niโ“˜ Native Iron var. Kamacite(Fe,Ni)
Niโ“˜ Taenite(Fe,Ni)
CuCopper
Cuโ“˜ Native CopperCu
Cuโ“˜ IsocubaniteCuFe2S3

Other Regions, Features and Areas containing this locality

Australia
Australian 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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