http://www.cnr.it/ontology/cnr/individuo/prodotto/ID29632
Thermal history of ALH84001 meteorite by Fe2+-Mg ordering in orthopyroxene. (Articolo in rivista)
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- Label
- Thermal history of ALH84001 meteorite by Fe2+-Mg ordering in orthopyroxene. (Articolo in rivista) (literal)
- Anno
- 2007-01-01T00:00:00+01:00 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
- 10.1111/j.1945-5100.2007.tb00531.x (literal)
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- Domeneghetti M.C.; Fioretti A.M.; Cámara F.; Molin G.; Tazzoli V. (literal)
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- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroFascicolo
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- 1. Univ Pavia, Dipartimento Sci Terra, I-27100 Pavia, Italy
2. CNR, IGG Unita Padova, I-35137 Padua, Italy
3. CNR, IGG Unita Pavia, I-27100 Pavia, Italy
4. Univ Padua, Dipartimento Min & Petrol, I-35137 Padua, Italy (literal)
- Titolo
- Thermal history of ALH84001 meteorite by Fe2+-Mg ordering in orthopyroxene. (literal)
- Abstract
- -A single orthopyroxene crystal from the Martian meteorite Allan Hills (ALH) 84001 was
studied by X-ray diffraction (XRD) and electron microprobe analysis (EMPA) to retrieve information
about its thermal history. Both sets of data were used to measure the Fe2+-Mg order degree between
the M1 and M2 sites expressed by the distribution coefficient kD. The 529 ± 30 °C closure temperature
(Tc) of the Fe2+-Mg ordering process of ALH 84001 orthopyroxene (Fs28) was calculated using
Stimpfl (2005a, 2005b) lnkD versus 1/T equation obtained for intermediate iron sample. At this Tc, the
orthopyroxene cooling rate, calculated by Ganguly's (1982) numerical method, was 0.1 °C/day. This
study puts new constraints on the last high-temperature thermal episode recorded by orthopyroxene.
With reference to the geological history (Treiman 1998), we ascribe this episode to the I3 event, and
we interpret the Tc of 529 °C as a lower limit for this impact heating. Our data confirm that
experimentally defined physical conditions for the formation of magnetite from decomposition of
carbonates took place on the Martian surface during event I3. (literal)
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