Last Updated:2025/12/04

In the rock sample, calcio-olivine formed distinct, pale grains that confirmed a high-calcium silicate composition.

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In the rock sample, calcio-olivine formed distinct, pale grains that confirmed a high-calcium silicate composition.

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岩石試料では、カルシウム・オリビンが明瞭な淡色の粒子として形成され、高カルシウムの珪酸塩組成が確認された。

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