Details

Autor(en) / Beteiligte

• Shaw, R. K.
• Arima, M.

Titel

Retrograde pressure-temperature path for spinel-bearing metapelites in Rayagada, Eastern Ghats, India

Ist Teil von

• Mineralogy and petrology, 1997-01, Vol.60 (1-2), p.41-59

Ort / Verlag

Wien: Springer Nature B.V

Erscheinungsjahr

1997

Quelle

Springer journals

Beschreibungen/Notizen

• Two assemblages have been identified in spinel-bearing metapelites from Rayagada, in the Eastern Ghats Belt, India: the first, an iron-rich assemblage, is characterized by iron-rich spinel and garnet; the second, iron-poor assemblage, by iron-poor spinel and garnet, together with cordierite and hematite. Garnet and sillimanite coronas around spinel show elongation parallel to the dominant fabric in the iron-rich assemblage but not in the iron-poor one. Both textures suggest the corona forming retrograde reaction spl + qtz = grt + sil. The P-T conditions for these corona-forming reactions are estimated at 950°C and 8.7-9.0 kbar for the iron-rich, and 800°C and 8 kbar for the iron-poor assemblage. Thermobarometric results and observed phase relations, using the model system FeO-MgO-Al^sub 2^O^sub 3^-SiO^sub 2^ (FMAS) indicate near-isobaric cooling from 950° to 800°C and subsequent decompression from 8 to 6.5 kbar. The corona-forming event in the iron-rich assemblage has been correlated with the dominant second phase of deformation (D2), but that in the iron-poor assemblage apparently postdates D^sub 2^.[PUBLICATION ABSTRACT]