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Shelburne dike
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Shelburne dike : ウィキペディア英語版
Shelburne dike

The Shelburne dike, also known as the Great Dike, is a large northeast trending Mesozoic diabase dike in southeastern Nova Scotia, Canada. It is long, although some evidence suggests it extends a further to the northeast to Sambro Island. The dike might have fed volcanoes in the Triassic period when the landscape was rifting apart during the breakup of supercontinent Pangaea.〔(T2.6 The Triassic Basalts and Continental Rifting )〕〔(The Shelburne dike, an early Mesozoic diabase dike in Nova Scotia: mineralogy, chemistry, and regional significance:1 Discussion )〕
==See also==

*Volcanism of Canada
*Volcanism of Eastern 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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