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A cone sheet is a type of high-level igneo … A cone sheet is a type of high-level igneous intrusion of subvolcanic rock, found in partly eroded central volcanic complexes. Cone sheets are relatively thin inclined sheets, generally just a few metres thick, with the geometry of a downward-pointing cone. Viewed from above, their outcrop is typically circular to elliptical. They were originally described from the Ardnamurchan, Mull and other central complexes of the British Tertiary Volcanic Province (now recognised as part of the North Atlantic Igneous Province).t of the North Atlantic Igneous Province).
, 錐狀岩板（英語：cone sheet）是一種淺成岩的火成岩侵入體，常出露在部分被侵蝕的火山雜岩中心。錐狀岩板是由較薄的傾斜岩板構成，通常只有幾米厚，形狀如同向下指向的圓錐體。 從空中看，它們通常是圓形到橢圓形。 最初被命名是在英國第三紀火山省 Ardnamurchan、Mull 和其他在中央的複合體。
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錐狀岩板（英語：cone sheet）是一種淺成岩的火成岩侵入體，常出露在部分被侵蝕的火山雜岩中心。錐狀岩板是由較薄的傾斜岩板構成，通常只有幾米厚，形狀如同向下指向的圓錐體。 從空中看，它們通常是圓形到橢圓形。 最初被命名是在英國第三紀火山省 Ardnamurchan、Mull 和其他在中央的複合體。
, A cone sheet is a type of high-level igneo … A cone sheet is a type of high-level igneous intrusion of subvolcanic rock, found in partly eroded central volcanic complexes. Cone sheets are relatively thin inclined sheets, generally just a few metres thick, with the geometry of a downward-pointing cone. Viewed from above, their outcrop is typically circular to elliptical. They were originally described from the Ardnamurchan, Mull and other central complexes of the British Tertiary Volcanic Province (now recognised as part of the North Atlantic Igneous Province).t of the North Atlantic Igneous Province).
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錐狀岩板
, Cone sheet
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