Brownfield (1937) meteorite, Terry County, Texas, USAi
| Regional Level Types | |
|---|---|
| Brownfield (1937) meteorite | Meteorite Fall Location |
| Terry County | County |
| Texas | State |
| USA | Country |
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Latitude & Longitude (WGS84):
33° 13' 0'' North , 102° 10' 59'' West
Latitude & Longitude (decimal):
Meteorite Class:
Meteoritical Society Class:
Köppen climate type:
Nearest Settlements:
| Place | Population | Distance |
|---|---|---|
| Brownfield | 9,736 (2017) | 9.3km |
| Meadow | 593 (2011) | 13.6km |
| Ropesville | 439 (2017) | 22.0km |
| New Home | 341 (2017) | 28.0km |
| Wellman | 203 (2011) | 29.5km |
Ordinary chondrite, unequilibrated (H3.7; S1; W3)
Found, 1937; 40.96 kg
After two stones had been found in 1937, five additional associated stones had been recovered by 1971. Inspections reveal distinct chondrules and chondrule fragments, and xenoliths within a complex matrix. Compositionally, bulk iron contents (26 wt% Fe), the nearly equilibrated olivine (Fa18.5,ave.), and the more variable pyroxenes are characteristic of the unequilibrated H chondrites. Mineralogically, the meteorite consists primarily of dominant olivine and pyroxene with minor troilite, and Fe-Ni metal. Pyroxene in chondrules is variable and usually clinopyroxene, but is often mantled by more Ca-rich phases. In a few porphyritic [POP] and radial pyroxene [RP] chondrules, clinoenstatite (sensu strictu, En>90) is found. Accessory chromite, ilmenite, feldspar and other very minor phases are also reported in the chondrules and/or matrix. Taenite, if present, is apparently quite sparse — perhaps due to extensive weathering (weathering grade W3). Secondary goethite and magnetite are among the more prominent terrestrial weatherates reported by Ramdohr (1973). Ar, Kr, and Xe gases appear to include residues of the early solar nebula. A cosmic ray exposure (CRE) age of ~30.4 Ma and a terrestrial age of 21 ka have also been reported.
The H group of ordinary chondrites constitute roughly 35-40% of all recovered meteorites with over 20,000 recovered by early 2017. However, only 75 meteorites have been classified as exactly 'H3.7' [as of January 2017]. Brownfield (1937) is the second-most massive member of this small meteoritic subtype. Only the 200 kg Dimmitt L3.7 chondrite (another Texas stone) is more massive.
What's in a name? Harvey Nininger and his son-in-law, Glenn Huss, were instrumental in recovering several meteoritic stones from Terry County. After confusion in some instances, it became clear that the Brownfield (iron), Brownfield (1964), and Brownfield (c) meteorites [IID, H5, OC, resp.] represented an additional two or three individual falls.
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsMineral List
12 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:
| ⓘ Augite Formula: (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| ⓘ 'Chrome-Spinel (of Dana)' |
| ⓘ Chromite Formula: Fe2+Cr3+2O4 |
| ⓘ Clinoenstatite Formula: MgSiO3 Description: Most abundant pyroxene in chondrule pyroxenes. |
| ⓘ 'Clinopyroxene Subgroup' |
| ⓘ 'Fayalite-Forsterite Series' Description: Average olivine (Fa18,4) in Rubin, 1990, and (Fa18.5) reported by Hutchison in Grady, 2000, are virtually identical. References: |
| ⓘ 'Feldspar Group' Description: Orthoclase component approaches 20 mol% in some chondrules. |
| ⓘ 'Glass' |
| ⓘ Goethite Formula: Fe3+O(OH) |
| ⓘ Ilmenite Formula: Fe2+TiO3 |
| ⓘ Magnetite Formula: Fe2+Fe3+2O4 Description: In this instance, secondary (e.g., a terrestrial weatherate). |
| ⓘ Native Copper Formula: Cu |
| ⓘ Native Iron Formula: Fe |
| ⓘ Native Iron var. Kamacite Formula: (Fe,Ni) Description: Kamacite can be as Ni-poor as 2 wt%. |
| ⓘ 'Orthopyroxene Subgroup' |
| ⓘ Pentlandite Formula: (NixFey)Σ9S8 |
| ⓘ Pigeonite Formula: (CaxMgyFez)(Mgy1Fez1)Si2O6 Description: Pigeonite as discontinuous chondritic rims. |
| ⓘ 'Plagioclase' Formula: (Na,Ca)[(Si,Al)AlSi2]O8 Description: Albitic and anorthitic components quite variable with orthoclase component as small as 2 mol% in some chondrules. |
| ⓘ 'Pyroxene Group' Formula: ADSi2O6 Description: Pyroxenes include, minimally, augite, clinoenstatite [sensu strictu], clinopyroxene (mostly 'clinobronzite'), orthopyroxene and pigeonite. |
| ⓘ Spinel Formula: MgAl2O4 |
| ⓘ Troilite Formula: FeS References: |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 1 - Elements | |||
|---|---|---|---|
| ⓘ | Native Copper | 1.AA.05 | Cu |
| ⓘ | Native Iron | 1.AE.05 | Fe |
| ⓘ | var. Kamacite | 1.AE.05 | (Fe,Ni) |
| Group 2 - Sulphides and Sulfosalts | |||
| ⓘ | Pentlandite | 2.BB.15 | (NixFey)Σ9S8 |
| ⓘ | Troilite | 2.CC.10 | FeS |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Goethite | 4.00. | Fe3+O(OH) |
| ⓘ | Chromite | 4.BB.05 | Fe2+Cr3+2O4 |
| ⓘ | Magnetite | 4.BB.05 | Fe2+Fe3+2O4 |
| ⓘ | Spinel | 4.BB.05 | MgAl2O4 |
| ⓘ | Ilmenite | 4.CB.05 | Fe2+TiO3 |
| Group 9 - Silicates | |||
| ⓘ | Clinoenstatite | 9.DA.10 | MgSiO3 |
| ⓘ | Pigeonite | 9.DA.10 | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| ⓘ | Augite | 9.DA.15 | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| Unclassified | |||
| ⓘ | 'Feldspar Group' | - | |
| ⓘ | 'Clinopyroxene Subgroup' | - | |
| ⓘ | 'Fayalite-Forsterite Series' | - | |
| ⓘ | 'Plagioclase' | - | (Na,Ca)[(Si,Al)AlSi2]O8 |
| ⓘ | 'Pyroxene Group' | - | ADSi2O6 |
| ⓘ | 'Chrome-Spinel (of Dana)' | - | |
| ⓘ | 'Orthopyroxene Subgroup' | - | |
| ⓘ | 'Glass' | - | |
List of minerals for each chemical element
| H | Hydrogen | |
|---|---|---|
| H | ⓘ Goethite | Fe3+O(OH) |
| O | Oxygen | |
| O | ⓘ Augite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| O | ⓘ Chromite | Fe2+Cr23+O4 |
| O | ⓘ Clinoenstatite | MgSiO3 |
| O | ⓘ Goethite | Fe3+O(OH) |
| O | ⓘ Ilmenite | Fe2+TiO3 |
| O | ⓘ Magnetite | Fe2+Fe23+O4 |
| O | ⓘ Pigeonite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| O | ⓘ Spinel | MgAl2O4 |
| O | ⓘ Fayalite-Forsterite Series | |
| O | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| O | ⓘ Pyroxene Group | ADSi2O6 |
| Na | Sodium | |
| Na | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Mg | Magnesium | |
| Mg | ⓘ Augite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| Mg | ⓘ Clinoenstatite | MgSiO3 |
| Mg | ⓘ Pigeonite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| Mg | ⓘ Spinel | MgAl2O4 |
| Mg | ⓘ Fayalite-Forsterite Series | |
| Al | Aluminium | |
| Al | ⓘ Spinel | MgAl2O4 |
| Al | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Si | Silicon | |
| Si | ⓘ Augite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| Si | ⓘ Clinoenstatite | MgSiO3 |
| Si | ⓘ Pigeonite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| Si | ⓘ Fayalite-Forsterite Series | |
| Si | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Si | ⓘ Pyroxene Group | ADSi2O6 |
| S | Sulfur | |
| S | ⓘ Pentlandite | (NixFey)Σ9S8 |
| S | ⓘ Troilite | FeS |
| Ca | Calcium | |
| Ca | ⓘ Augite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| Ca | ⓘ Pigeonite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| Ca | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Ti | Titanium | |
| Ti | ⓘ Ilmenite | Fe2+TiO3 |
| Cr | Chromium | |
| Cr | ⓘ Chromite | Fe2+Cr23+O4 |
| Fe | Iron | |
| Fe | ⓘ Augite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| Fe | ⓘ Chromite | Fe2+Cr23+O4 |
| Fe | ⓘ Goethite | Fe3+O(OH) |
| Fe | ⓘ Ilmenite | Fe2+TiO3 |
| Fe | ⓘ Native Iron | Fe |
| Fe | ⓘ Native Iron var. Kamacite | (Fe,Ni) |
| Fe | ⓘ Magnetite | Fe2+Fe23+O4 |
| Fe | ⓘ Pentlandite | (NixFey)Σ9S8 |
| Fe | ⓘ Pigeonite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| Fe | ⓘ Troilite | FeS |
| Fe | ⓘ Fayalite-Forsterite Series | |
| Ni | Nickel | |
| Ni | ⓘ Native Iron var. Kamacite | (Fe,Ni) |
| Ni | ⓘ Pentlandite | (NixFey)Σ9S8 |
| Cu | Copper | |
| Cu | ⓘ Native Copper | Cu |
Other Regions, Features and Areas containing this locality
North AmericaContinent
North America PlateTectonic Plate
- Granite-Rhyolite ProvinceMagmatic Province
- Permian BasinBasin
- Shawnee DomainDomain
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References
Bunch, T.E., Keil, Klaus, Snetsinger, K.G. (1967) Chromite composition in relation to chemistry and texture of ordinary chondrites. Geochimica et Cosmochimica Acta, 31 (10). 1569-1582 doi:10.1016/0016-7037(67)90105-6
Snetsinger, Kenneth G., Keil, Klaus (1969) Ilmenite in ordinary Chondrites. American Mineralogist, 54 (5-6) 780-786