Amphibolite to granulite transition in aluminous greywackes from the Sierra de Comechingones, Córdoba, Argentina

OTAMENDI, J.E., PATIÑO DOUCE, A.E. Y DEMICHELIS, A.H

JOURNAL OF METAMORPHIC GEOLOGY

WILEY-BLACKWELL PUBLISHING, INC

Año: 1999 vol. 17 p. 415 - 434

0263-4929

We discuss upper-amphibolite- to granulite-facies, early Paleozoic metamorphism and partial melting of aluminous greywackes from the Sierra de Comechingones, SE Sierras Pampeanas of Central Argentina. Consistent pressure-temperature estimates, obtained from equilibria involving Al and Ti exchange components in biotite and from more traditional thermobarometric equilibria, suggest that peak metamorphism of the exposed section took place at an essentially constant pressure of 7 - 8 kbar, and at temperatures ranging from 650 ºC to 950 ºC. Mineral compositions record an initial decompression, after peak metamorphism, of  ~ 1.5 kbar, that was accompanied by a cooling of ~100 ºC. Upper-amphibolite-facies gneisses consist of the assemblage Qtz + Pl + Bt + Grt + Rt / Ilm. The transition to the granulite facies is marked by the simultaneous appearance of the assemblage Kfs + Sil and of migmatitic structures, suggesting that the amphibolite-to-granulite transition in the Sierra de Comechingones corresponds to the beginning of melting. Rocks with structural and / or chemical manifestations of partial melting range from metatexites, to diatexites, to melt-depleted granulites, consisting of the assemblage Grt + Crd + Pl + Qtz + Ilm ± Ath. The melting stage overlapped at least partially with decompression, as suggested by the occurrence of cordierite, in both the migmatites and the residual granulites, of two distinct textural types:  idiomorphic porphyroblasts (probably representing peritectic cordierite) and garnet-rimming coronas. Metapelitic rocks are unknown in the Sierra de Comechingones. Therefore, it appears most likely that the Al-rich residual assemblages found in the migmatites and residual granulites was formed by partial-melting of muscovite- and sillimanite-undersaturated metagreywackes.We propose a mechanism for this that relies on the subsolidus stabilization of garnet and the ensuing changes in the octahedral Al content of biotite with pressure and temperature.