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Salal Creek Pluton : ウィキペディア英語版 | Salal Creek Pluton The Salal Creek Pluton, also called the Salal Creek stock, is a small circular eight-million-year-old intrusion with an area of . It contains 52 dikes composed of basalt and was probably formed or less below the Earth's surface.〔(Salal Creek Molybdenum Property )〕 It forms part of the Pemberton Volcanic Belt, a geological formation that formed as a result of subduction zone volcanism in the Canadian Cascade Arc. ==See also==
*Volcanism of Western Canada
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「Salal Creek Pluton」の詳細全文を読む
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