TY - JOUR
T1 - Pressure-temperature-time path of a metapelite from Mefjell, Sør Rondane Mountains, East Antarctica
AU - Tsubokawa, Yumiko
AU - Ishikawa, Masahiro
AU - Kawakami, Tetsuo
AU - Hokada, Tomokazu
AU - Satish-Kumar, M.
AU - Tsuchiya, Noriyoshi
AU - Grantham, Geoffrey H.
PY - 2017/4/1
Y1 - 2017/4/1
N2 - A metapelite preserving prograde and retrograde zoning in garnet from Mefjell, southern Sør Rondane Mountains (SRM), East Antarctica is described in detail and U-Th-Pb geochronological data are presented. Garnet, sillimanite, staurolite and biotite are in textural equilibrium in the matrix. The garnet shows three distinct compositional zones comprising core, mantle and rim. From core to the mantle, the spessartine content represents a bell-shaped profile. From mantle to the rim, spessartine content increases and pyrope decreases. Kyanite is present as tiny inclusions in the garnet core. The core also contains aggregates of sillimanite with radial cracks around them, interpreted to have resulted from the inversion of kyanite. The prograde P-T path recorded in the garnet is heating to approximately 700 °C at 5.6 kbar with a slight increase in pressure. U-Th-Pb dating of monazite grains yields a large range of age distribution between 700 and 540 Ma. The inferred prograde metamorphism of the metapelite sample in this study might be related to subduction and/or tectonic loading explained by a collision tectonic model of the SRM (Osanai et al., 2013).
AB - A metapelite preserving prograde and retrograde zoning in garnet from Mefjell, southern Sør Rondane Mountains (SRM), East Antarctica is described in detail and U-Th-Pb geochronological data are presented. Garnet, sillimanite, staurolite and biotite are in textural equilibrium in the matrix. The garnet shows three distinct compositional zones comprising core, mantle and rim. From core to the mantle, the spessartine content represents a bell-shaped profile. From mantle to the rim, spessartine content increases and pyrope decreases. Kyanite is present as tiny inclusions in the garnet core. The core also contains aggregates of sillimanite with radial cracks around them, interpreted to have resulted from the inversion of kyanite. The prograde P-T path recorded in the garnet is heating to approximately 700 °C at 5.6 kbar with a slight increase in pressure. U-Th-Pb dating of monazite grains yields a large range of age distribution between 700 and 540 Ma. The inferred prograde metamorphism of the metapelite sample in this study might be related to subduction and/or tectonic loading explained by a collision tectonic model of the SRM (Osanai et al., 2013).
KW - East Antarctica
KW - Pressure and temperature conditions
KW - Prograde zoning
KW - Sør Rondane Mountains
UR - http://www.scopus.com/inward/record.url?scp=85018934943&partnerID=8YFLogxK
U2 - 10.2465/jmps.160919
DO - 10.2465/jmps.160919
M3 - Article
AN - SCOPUS:85018934943
SN - 1345-6296
VL - 112
SP - 77
EP - 87
JO - Journal of Mineralogical and Petrological Sciences
JF - Journal of Mineralogical and Petrological Sciences
IS - 2
ER -