Felsite-nanogranite inclusions and three Al 2 SiO 5 polymorphs in the same garnet in ultrahigh-temperature granulites from Rundvågshetta, Lützow-Holm Complex, East Antarctica

Yoshikuni Hiroi, Tomokazu Hokada, Mutsumi Kato, Ayahiko Yanagi, Tatsuro Adachi, Yasuhito Osanai, Yoichi Motoyoshi, Kazuyuki Shiraishi

Research output: Contribution to journalArticle

Abstract

Ultrahigh-temperature (UHT) granulites characterized by the parageneses of sapphirine + quartz and orthopyroxene + sillimanite + garnet + quartz are found in Rundvågshetta, Lützow-Holm Complex (LHC), East Antarctica. In this study, we report previously undocumented features of the UHT pelitic granulites, including the presence of felsite-nanogranite inclusions (FNIs), which are interpreted to have formed by the supercooling of melt inclusions in garnet, and the presence of three Al 2 SiO 5 polymorphs within the same garnet porphyroblast. Whereas sillimanite is present as inclusions in garnet and in the matrix, kyanite occurs as inclusions in garnet and andalusite appears in FNIs. Porphyroblastic garnet is compositionally zoned with Mg-rich cores surrounded by Fe- and Mn-rich rims, indicating homogenization and later modification of Fe, Mg, and Mn. Ca contents oscillate from core to rim, which may be a remnant of growth zoning and suggests compression before high- temperature decompression. Integration of these new data with those previously documented leads to the inference of a rapid change in pressure-temperature conditions during regional UHT metamorphism in the late Neoproterozoic to early Paleozoic Gondwana-forming collisional orogen. Locally occurring intimate intergrowths of kyanite/sillimanite + sapphirine + garnet ± quartz in garnet may be a breakdown product of Mg-rich staurolite and thus may be a link between high-pressure and UHT metamorphism.

Original languageEnglish
Pages (from-to)60-78
Number of pages19
JournalJournal of Mineralogical and Petrological Sciences
Volume114
Issue number2
DOIs
Publication statusPublished - Apr 1 2019

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felsite
Antarctic regions
garnets
garnet
inclusions
sillimanite
temperature
ultrahigh temperature metamorphism
sapphirine
quartz
kyanite
rims
supercooling
porphyroblast
andalusite
staurolite
Antarctica
melt inclusion
pressure reduction
regional metamorphism

All Science Journal Classification (ASJC) codes

  • Geophysics
  • Geology

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Felsite-nanogranite inclusions and three Al 2 SiO 5 polymorphs in the same garnet in ultrahigh-temperature granulites from Rundvågshetta, Lützow-Holm Complex, East Antarctica . / Hiroi, Yoshikuni; Hokada, Tomokazu; Kato, Mutsumi; Yanagi, Ayahiko; Adachi, Tatsuro; Osanai, Yasuhito; Motoyoshi, Yoichi; Shiraishi, Kazuyuki.

In: Journal of Mineralogical and Petrological Sciences, Vol. 114, No. 2, 01.04.2019, p. 60-78.

Research output: Contribution to journalArticle

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AU - Hiroi, Yoshikuni

AU - Hokada, Tomokazu

AU - Kato, Mutsumi

AU - Yanagi, Ayahiko

AU - Adachi, Tatsuro

AU - Osanai, Yasuhito

AU - Motoyoshi, Yoichi

AU - Shiraishi, Kazuyuki

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