Jonzac meteorite, Saint-Simon-de-Bordes, Jonzac, Charente-Maritime, Nouvelle-Aquitaine, Francei
Regional Level Types | |
---|---|
Jonzac meteorite | Meteorite Fall Location |
Saint-Simon-de-Bordes | Commune |
Jonzac | Arrondissement |
Charente-Maritime | Department |
Nouvelle-Aquitaine | Region |
France | Country |
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Latitude & Longitude (WGS84):
45° 25' 59'' North , 0° 27' 0'' West
Latitude & Longitude (decimal):
Meteorite Class:
Meteoritical Society Class:
Köppen climate type:
Nearest Settlements:
Place | Population | Distance |
---|---|---|
Saint-Germain-de-Lusignan | 1,179 (2016) | 2.1km |
Jonzac | 4,524 (2016) | 2.3km |
Saint-Martial-de-Vitaterne | 387 (2016) | 3.3km |
Saint-Hilaire-du-Bois | 302 (2016) | 4.0km |
Saint-Simon-de-Bordes | 666 (2016) | 4.2km |
Mindat Locality ID:
259727
Long-form identifier:
mindat:1:2:259727:3
GUID (UUID V4):
814af88f-a9dc-4a5f-830d-5ea875c743b7
Other/historical names associated with this locality:
Poitou-Charentes
Fall, 13 Jun 1819; 5 kg
Eucrite, monomict
Soon after sunrise a fireball was seen, detonations were heard, and a shower of stones were said to have fallen with 2 stones (3 kg & 2 kg) being recovered for study. Today, Juvinas is recognized as the second of 34 witnessed eucrite falls. Like most eucrites, Juvinas is compositionally dominated by brecciated intergrowths of pyroxene (mostly pigeonite) and variable, somewhat anorthitic plagioclase. Other phases appear to be quite minor as they receive only tangential mention in most references cited here. Minor zircon has received special attention, however, as it appears to provide the most reliable indicator of the original formation epoch of the Juvinas mineralogical assemblages ~4.55 billion years ago (Pb-Pb dating).
Less than 1.5 kg of the original ~5 kg remains in scientific repositories, but enough material is extant to be used in occasional geochemical and chronological studies. After original formation of the Juvinas parent body, Pu-Xe, Lu-Hf, & Pb-Pb ages all suggest that important metamorphic disturbance -- probably impact(s) — occurred ~ 300 million years later. (Cf. Dietderich, et al., 2013). This chronology is consistent with similar ages contributing to an emerging consensus within the planetary science community that most Eucrites (and related Howardites and Diogenites) are fragments of the asteroid Vesta.
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsMineral List
6 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:
ⓘ Anorthite Formula: Ca(Al2Si2O8) Description: Anorthite (with associated Bytownite) account for approximately 33% of the meteorite |
ⓘ Ilmenite Formula: Fe2+TiO3 |
ⓘ Pigeonite Formula: (CaxMgyFez)(Mgy1Fez1)Si2O6 |
ⓘ 'Plagioclase' Formula: (Na,Ca)[(Si,Al)AlSi2]O8 References: |
ⓘ 'Pyroxene Group' Formula: ADSi2O6 Description: Pigeonite appears to be dominant, but the pyroxenes range from Wo2Fs65En34—Wo47Fs21En29. The Ca-rich values are consistent only with diopside, augite, or -perhaps- ferroaugite. References: |
ⓘ Quartz Formula: SiO2 |
ⓘ Troilite Formula: FeS Description: Farrington discusses both troilite and pyrrhotite, but as he suggests that the FeS is both non-magnetic and stoichiometric it seems clear he has observed troilite. |
ⓘ Zircon Formula: Zr(SiO4) References: |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
Group 2 - Sulphides and Sulfosalts | |||
---|---|---|---|
ⓘ | Troilite | 2.CC.10 | FeS |
Group 4 - Oxides and Hydroxides | |||
ⓘ | Ilmenite | 4.CB.05 | Fe2+TiO3 |
ⓘ | Quartz | 4.DA.05 | SiO2 |
Group 9 - Silicates | |||
ⓘ | Zircon | 9.AD.30 | Zr(SiO4) |
ⓘ | Pigeonite | 9.DA.10 | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
ⓘ | Anorthite | 9.FA.35 | Ca(Al2Si2O8) |
Unclassified | |||
ⓘ | 'Plagioclase' | - | (Na,Ca)[(Si,Al)AlSi2]O8 |
ⓘ | 'Pyroxene Group' | - | ADSi2O6 |
List of minerals for each chemical element
O | Oxygen | |
---|---|---|
O | ⓘ Anorthite | Ca(Al2Si2O8) |
O | ⓘ Ilmenite | Fe2+TiO3 |
O | ⓘ Pigeonite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
O | ⓘ Quartz | SiO2 |
O | ⓘ Zircon | Zr(SiO4) |
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 | ⓘ Pigeonite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
Al | Aluminium | |
Al | ⓘ Anorthite | Ca(Al2Si2O8) |
Al | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
Si | Silicon | |
Si | ⓘ Anorthite | Ca(Al2Si2O8) |
Si | ⓘ Pigeonite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
Si | ⓘ Quartz | SiO2 |
Si | ⓘ Zircon | Zr(SiO4) |
Si | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
Si | ⓘ Pyroxene Group | ADSi2O6 |
S | Sulfur | |
S | ⓘ Troilite | FeS |
Ca | Calcium | |
Ca | ⓘ Anorthite | Ca(Al2Si2O8) |
Ca | ⓘ Pigeonite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
Ca | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
Ti | Titanium | |
Ti | ⓘ Ilmenite | Fe2+TiO3 |
Fe | Iron | |
Fe | ⓘ Ilmenite | Fe2+TiO3 |
Fe | ⓘ Pigeonite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
Fe | ⓘ Troilite | FeS |
Zr | Zirconium | |
Zr | ⓘ Zircon | Zr(SiO4) |
Other Regions, Features and Areas containing this locality
Eurasian PlateTectonic Plate
EuropeContinent
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