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Salal Creek Pluton
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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)
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