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Blomidon Formation : ウィキペディア英語版 | Blomidon Formation
The Blomidon Formation is a unit of Upper Triassic (Norian–Rhaetian) sedimentary rocks, which outcrops in Nova Scotia. At outcrop they reach a maximum thickness of 365m, but up to 1168m has been proven from well data and a thickness of up to 2500m has been inferred from seismic reflection data. It overlies the mainly Carnian Wolfville Formation and underlies the North Mountain Basalt. The type section is exposed between Cape Blomidon () and Paddy Island (). ==References==
抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)』 ■ウィキペディアで「Blomidon Formation」の詳細全文を読む
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