Allan Hills A77230 meteorite, Allan Hills, Victoria Land, Eastern Antarctica, Antarcticai
Regional Level Types | |
---|---|
Allan Hills A77230 meteorite | Meteorite Fall Location |
Allan Hills | Group of Hills |
Victoria Land | Region |
Eastern Antarctica | Region |
Antarctica | Continent |
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Latitude & Longitude (WGS84):
74° 43' South , 159° 40' East
Latitude & Longitude (decimal):
Locality type:
Meteorite Class:
Meteoritical Society Class:
KΓΆppen climate type:
Other/historical names associated with this locality:
ALHA77230; ALH 77230
Ordinary Chondrite (L4; S2; W4)
Find,1977; 2.4773 kg
Allan Hills A77230 (ALHA77230) was a nearly complete moderate-sized, weathered meteoritic stone recovered by the joint US-Japanese Antarctic Meteorite program. In thin sections distinct chondrules and chondrule fragments are tightly packed within a medium-grained matrix. Olivine and pyroxene chondrules (mean diameters 0.3-2.0 mm) are present with barred and porphyritic olivine (BO,PO) and radial pyroxene (RP) chondrule types the most prominent. Two populations of chondrules can be distinguished β prominent spherical chondrules with a glassy mesostasis and other less defined chondrules partially integrated with the surrounding matrix. Average composition of olivine (Fa23) [and pyroxene (Fs~18)] is indicative of the L chondrite group. Partial integration of chondrules and matrix and the mild disequilibrium of olivine (Fa22-25) and the more marked disequilibrium of pyroxene disequilibrium (Fs18β29) account for the L4 petrologic type designation. Formal definition of L4 chondrites would normally indicate an absence of primary glass. In this instance, apparently, the petrologic type 4 designation represents a characterization of the overall status for what is an oddly heterogeneous aggregate. Troilite and lesser amounts of Fe-Ni metal appear in pooled, interstitial metal-troilite aggregates. Weathering grade (W4) is based upon the presence of significant rust in fissures and limonite staining.
A few studies have been published which have been more focused on reconstructing the thermal history of ALHA77230 (along with other chondrites) rather than reporting on its mineralogy per se. A somewhat tentative K-Ar age of ~3.4 Ga suggests that ALHA77230 has experienced at least one major disruption since it original aggregation and, presumably, before it was ejected into an earth-crossing orbit.
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsMineral List
4 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 DiagramDetailed Mineral List:
β 'Clinopyroxene Subgroup' Description: Clinopyroxene, often twinned, appears to be the primary Ca-poor pyroxene. Reference: Meteorite Working Group (1978) Antarctic meteorite Newsletter: Johnson Space Center, Houston. (Nov 1978).; Tsuchiyama, A., Fujita, T. & Morimoto, N. (1988). Fe-Mg Heterogeneity in the low-Ca Pyroxenes during metamorphism of the Ordinary Chondrites. Proc. NIPR Symposium Antarct. Meteorites 1, 173-174. |
β Diopside Formula: CaMgSi2O6 Description: 1 grain of diopsidic composition reported by Tsuchiyama et al. (1988). Reference: Tsuchiyama, A., Fujita, T. & Morimoto, N. (1988). Fe-Mg Heterogeneity in the low-Ca Pyroxenes during metamorphism of the Ordinary Chondrites. Proc. NIPR Symposium Antarct. Meteorites 1, 173-174. |
β 'Fayalite-Forsterite Series' Reference: Meteorite Working Group (1978) Antarctic meteorite Newsletter: Johnson Space Center, Houston. (Nov 1978).; Horii, Y., Fujii, N. & Takeda, H. (1990) Hardness analysis of metallic particles in ordinary chondrites. Fourteenth Symposium on Antarctic Meteorites. Proceedings of the NIPR Symposium, No. 3: 254-263.; Grady, M.M., Pratesi, G. & Moggi-Cecchi, V. (2015) Atlas of Meteorites. Cambridge University Press: Cambridge, United Kingdom. 373 pages. |
β 'Glass' Reference: Grady, M.M., Pratesi, G. & Moggi-Cecchi, V. (2015) Atlas of Meteorites. Cambridge University Press: Cambridge, United Kingdom. 373 pages. |
β Iron Formula: Fe Reference: Nagahara, N. (1980) Petrology of Equilibrated Chondrites: Metamorphism and Thermal History. Memoirs of National Institute of Polar Research, Special Issue 12: 32-49. |
β Iron var. Kamacite Formula: (Fe,Ni) Reference: Nagahara, N. (1980) Petrology of Equilibrated Chondrites: Metamorphism and Thermal History. Memoirs of National Institute of Polar Research, Special Issue 12: 32-49. |
β 'Limonite' Reference: Meteorite Working Group (1978) Antarctic meteorite Newsletter: Johnson Space Center, Houston. (Nov 1978).; Grady, M.M., Pratesi, G. & Moggi-Cecchi, V. (2015) Atlas of Meteorites. Cambridge University Press: Cambridge, United Kingdom. 373 pages. |
β 'Plagioclase' Formula: (Na,Ca)[(Si,Al)AlSi2]O8 Reference: Horii, Y., Fujii, N. & Takeda, H. (1990) Hardness analysis of metallic particles in ordinary chondrites. Fourteenth Symposium on Antarctic Meteorites. Proceedings of the NIPR Symposium, No. 3: 254-263. |
β 'Pyroxene Group' Formula: ADSi2O6 Reference: Meteorite Working Group (1978) Antarctic meteorite Newsletter: Johnson Space Center, Houston. (Nov 1978).; Horii, Y., Fujii, N. & Takeda, H. (1990) Hardness analysis of metallic particles in ordinary chondrites. Fourteenth Symposium on Antarctic Meteorites. Proceedings of the NIPR Symposium, No. 3: 254-263.; Grady, M.M., Pratesi, G. & Moggi-Cecchi, V. (2015) Atlas of Meteorites. Cambridge University Press: Cambridge, United Kingdom. 373 pages. |
β Taenite Formula: (Fe,Ni) Description: Ni-rich phase is mostly in the Ni 40%-45% range. Reference: Nagahara, N. (1980) Petrology of Equilibrated Chondrites: Metamorphism and Thermal History. Memoirs of National Institute of Polar Research, Special Issue 12: 32-49. |
β Troilite Formula: FeS Reference: Meteorite Working Group (1978) Antarctic meteorite Newsletter: Johnson Space Center, Houston. (Nov 1978).; Grady, M.M., Pratesi, G. & Moggi-Cecchi, V. (2015) Atlas of Meteorites. Cambridge University Press: Cambridge, United Kingdom. 373 pages. |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
Group 1 - Elements | |||
---|---|---|---|
β | Iron | 1.AE.05 | Fe |
β | var. Kamacite | 1.AE.05 | (Fe,Ni) |
β | Taenite | 1.AE.10 | (Fe,Ni) |
Group 2 - Sulphides and Sulfosalts | |||
β | Troilite | 2.CC.10 | FeS |
Group 9 - Silicates | |||
β | Diopside | 9.DA.15 | CaMgSi2O6 |
Unclassified Minerals, Rocks, etc. | |||
β | 'Clinopyroxene Subgroup' | - | |
β | 'Fayalite-Forsterite Series' | - | |
β | 'Glass' | - | |
β | 'Limonite' | - | |
β | 'Plagioclase' | - | (Na,Ca)[(Si,Al)AlSi2]O8 |
β | 'Pyroxene Group' | - | ADSi2O6 |
List of minerals for each chemical element
O | Oxygen | |
---|---|---|
O | β Pyroxene Group | ADSi2O6 |
O | β Diopside | CaMgSi2O6 |
O | β Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
Na | Sodium | |
Na | β Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
Mg | Magnesium | |
Mg | β Diopside | CaMgSi2O6 |
Al | Aluminium | |
Al | β Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
Si | Silicon | |
Si | β Pyroxene Group | ADSi2O6 |
Si | β Diopside | CaMgSi2O6 |
Si | β Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
S | Sulfur | |
S | β Troilite | FeS |
Ca | Calcium | |
Ca | β Diopside | CaMgSi2O6 |
Ca | β Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
Fe | Iron | |
Fe | β Troilite | FeS |
Fe | β Iron var. Kamacite | (Fe,Ni) |
Fe | β Taenite | (Fe,Ni) |
Fe | β Iron | Fe |
Ni | Nickel | |
Ni | β Iron var. Kamacite | (Fe,Ni) |
Ni | β Taenite | (Fe,Ni) |
References
Sort by
Year (asc) Year (desc) Author (A-Z) Author (Z-A)Meteorite Working Group (1978) Antarctic meteorite Newsletter: Johnson Space Center, Houston. (Nov 1978).
Nagahara, N. (1980) Petrology of Equilibrated Chondrites: Metamorphism and Thermal History. Memoirs of National Institute of Polar Research, Special Issue 12: 32-49.
Stephan, T. & Jessberger, E.K. (1978) Ar-40/Ar-39 ages of types 3 and 4, L and H chondrites from Antarctica: Meteoritics 23 (4):373-377. (Dec 1988).
Tsuchiyama, A., Fujita, T. & Morimoto, N. (1988). Fe-Mg Heterogeneity in the low-Ca Pyroxenes during metamorphism of the Ordinary Chondrites. Proc. NIPR Symposium Antarct. Meteorites 1, 173-174.
Horii, Y., Fujii, N. & Takeda, H. (1990) Hardness analysis of metallic particles in ordinary chondrites. Fourteenth Symposium on Antarctic Meteorites. Proceedings of the NIPR Symposium, No. 3: 254-263
Grossman, J.N. (1994). The Meteoritical Bulletin, No. 76: Meteoritics 29(1): 100-143. (Jan 1994).
Grady, M.M., Pratesi, G. & Moggi-Cecchi, V. (2015) Atlas of Meteorites. Cambridge University Press: Cambridge, United Kingdom. 373 pages.
External Links
http://www.lpi.usra.edu/meteor/metbull.php - MeteoriticalBulletinDatabase
http://www.lpi.usra.edu/meteor/metbull.php?code=1541 -ALHA77230@MetBullDatabase
http://ci.nii.ac.jp/els/110000029861.pdf?id=ART0000355554&type=pdf&lang=en&host=cinii&order_no=&ppv_type=0&lang_sw=&no=1468941067&cp= -Heterogeneity in pyroxenes
http://ci.nii.ac.jp/naid/110000009333/ -Nagahara(1980)
http://www.lpi.usra.edu/meteor/metbull.php?code=1541 -ALHA77230@MetBullDatabase
http://ci.nii.ac.jp/els/110000029861.pdf?id=ART0000355554&type=pdf&lang=en&host=cinii&order_no=&ppv_type=0&lang_sw=&no=1468941067&cp= -Heterogeneity in pyroxenes
http://ci.nii.ac.jp/naid/110000009333/ -Nagahara(1980)
Other Regions, Features and Areas containing this locality
Antarctic MeteoritesGroup of Meteorite Fall Locations
Antarctic PlateTectonic Plate
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