翻訳と辞書 Words near each other ・ Cariboo Mountains ・ Cariboo Mountains Provincial Park ・ Cariboo North ・ Cariboo Plateau ・ Cariboo Prospector ・ Cariboo Regional District ・ Cariboo River ・ Cariboo River Provincial Park ・ Cariboo Road ・ Cariboo Runaway ・ Cariboo South ・ Cariboo-Chilcotin ・ Cariboo-Chilcotin (provincial electoral district) ・ Cariboo—Chilcotin ・ Caribbean lanternshark ・ Caribbean large igneous province ・ Caribbean Law Institute ・ Caribbean Legion ・ Caribbean Link for Guiding ・ Caribbean literature ・ Caribbean Lowlands ・ Caribbean martin ・ Caribbean Media Corporation ・ Caribbean Medical University ・ Caribbean monk seal ・ Caribbean Moon ・ Caribbean Motel ・ Caribbean music in Canada ・ Caribbean music in the United Kingdom ・ Caribbean National Forest Act of 2005 Dictionary Lists mini英和辞書 mini和英辞書 Webster 1913 Latin-English FOLDOC Wikipedia English ウィキペディア

翻訳と辞書　辞書検索 [ 開発暫定版 ] スポンサード リンク Caribbean large igneous province ： ウィキペディア英語版 Caribbean large igneous province The Caribbean large igneous province (CLIP) consists of a major flood basalt, which created this large igneous province (LIP). It is the source of the current large eastern Pacific oceanic plateau, of which the Caribbean-Colombian oceanic plateau is the tectonized remnant. The deeper levels of the plateau have been exposed on its margins at the North and South American plates. The volcanism took place between 139 and 69 million years ago, with the majority of activity appearing to lie between 95 and 88 Ma. The plateau volume has been estimated as on the order of 4 x 106 km³. It has been linked to the Galápagos hotspot.〔; 〕 ==Proto-Caribbean Seaway== Divergence between the North American and South American Plates began to create oceanic crust off Colombia's Pacific coast by the end of the Jurassic (150 Ma). This divergence, which continued until at least 66 Ma, first resulted in a "proto-Caribbean spreading ridge" between these plates flanked by a perpendicular transform zone on its the Pacific side. By 135–130 Ma, the subduction of the Farallon Plate had begun along this transform zone, effectively modifying it into a subduction zone and beginning the creation of the Great Caribbean Arch. This arch was formed around 120-115 Ma but must have been intersected by the Caribbean spreading ridge until 66 Ma. Hence, the Farallon Plate fed the spreading zone and later became the Caribbean Plate. 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「Caribbean large igneous province」の詳細全文を読む スポンサード リンク 翻訳と辞書 : 翻訳のためのインターネットリソース Copyright(C) kotoba.ne.jp 1997-2016. All Rights Reserved.