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石基

5 件の記事

The smooth texture of this basaltic volcanic bomb is aphanitic.

アファナイト(潜晶質岩)の特性と火成岩の分類

アファナイト潜晶質火成岩火山岩
IUGS classification of aphanitic extrusive igneous rocks to their relative alkali (Na2O + K2O) and silica (SiO2) weight contents. Blue area is roughly where alkaline rocks plot; yellow area where subalkaline rocks plot. Original source: *Le Maitre, R.W. (ed.); 1989: A classification of igneous rocks and glossary of terms, Blackwell Science, Oxford.

火山岩(噴出岩)の形成プロセスと多様な岩石タイプ

火山岩噴出岩マグマ斑晶
Porphyritic texture in a granite. This is an intrusive porphyritic rock. The white, square feldspar phenocrysts are much larger than crystals in the surrounding matrix; eastern Sierra Nevada, Rock Creek Canyon, California.

斑状組織(ポルフィリティック)とは?火成岩の結晶サイズが異なる理由を解説

斑状組織ポルフィリティック斑晶石基
Granites often have large feldspathic phenocrysts. This granite, from the Swiss side of the Mont Blanc massif, has large white phenocrysts of plagioclase (that have trapezoid shapes when cut through). 1 euro coin (diameter 2.3 cm) for scale.

斑晶(Phenocryst)とは?火成岩の組織から読み解くマグマの履歴

斑晶火成岩斑状組織マグマ
IUGS classification of aphanitic extrusive igneous rocks to their relative alkali (Na2O + K2O) and silica (SiO2) weight contents. Blue area is roughly where alkaline rocks plot; yellow area where subalkaline rocks plot. Original source: *Le Maitre, R.W. (ed.); 1989: A classification of igneous rocks and glossary of terms, Blackwell Science, Oxford.

火山岩(噴出岩)の形成プロセスと多様な組織・種類

噴出岩火山岩マグマ斑晶