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Ungava magmatic event : ウィキペディア英語版 | Ungava magmatic event
The Ungava magmatic event was a widespread magmatic event that began about 2.22 billion years ago during the Proterozoic Eon. == Extent == With an area of , the Ungava magmatic event consists of a large igneous province.〔(2000 Ma large mafic magmatic events )〕 Magmatic features that were formed during the Ungava magmatic event include the Klotz, Maguire and Senneterre dikes of Quebec and the Nipissing sills of Ontario.
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「Ungava magmatic event」の詳細全文を読む
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