Cambrian granulite to upper amphibolite facies metamorphism of post-797 Ma sediments in Madagascar

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概要

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• The CHIME monazite and xenotime ages were determined for two paragneisses from Madagascar. The biotite-sillimanite-cordierite-quartz-microcline-plagioclase schist at Ihosy in southern Madagascar contains core-mantle monazite grains as well as chronologically unzoned ones. The unzoned monazite grains (8 of 11 analyzed grains) give a CHIME age of 527±15 Ma. Two zoned grains show core ages of 1640±180 and 797±75 Ma with mantles of 550±50 and 535±10 Ma, respectively. The kyanite- and corundum-bearing cordierite-sillimanite-muscovite-biotite-plagioclase-quartz gneiss at Maevatanana in northwestern Madagascar contains both monazite and xenotime. Monazite and xenotime grains are chronologically uniform, and give CHIME ages of 534±10 and 530±32 Ma, respectively. These chronological data suggest that the high-grade paragneisses in Madagascar, if not all, formed through a single thermal event at ca. 530 Ma from post-797 Ma sediments. This metamorphism can be linked to the continental collision that resulted in Gondwana supercontinent.

• 名古屋大学の論文

著者

• Suzuki Kazuhiro

  Department of Earth and Environmental Sciences, Nagoya University

• Yogo Setsuo

  Department Of Earth And Planetary Sciences Graduate School Of Science Nagoya University

• Ito Masahiro

  School Of Science And Engineering Waseda University:kagami Memorial Laboratory For Materials Science

• Ito Masahiro

  Department Of Applied Chemistry Faculty Of Engineering Osaka University

• Ito Masahiro

  School Of Informatics And Sciences Nagoya University

• SUZUKI Kazuhiro

  School of Informatics and Sciences, Nagoya University

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