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Okhotsk-Chukotka Volcanic Belt : ウィキペディア英語版 | Okhotsk-Chukotka Volcanic Belt The Okhotsk-Chukotka Volcanic Belt (OCVB) is a Cretaceous volcanic belt in northeastern Eurasia. It is one of the largest subduction-zone related volcanic provinces in the world, stretching some 3200 km and comprising about 2 million km3 of volcanic and plutonic material. The volcanism within the volcanic belt was related to the subduction of the ancient Kula Plate, which moved in a northward direction about 55 million years ago. ==References==
*(New 40Ar/39Ar ages of Cretaceous continental volcanics from central Chukotka: implications for initiation and duration of volcanism within northern part of the Okhotsk Chukotka Volcanic Belt (northeastern Eurasia) ), by V. O. Ispolatov, P. L. Tikhomirov, M. Heizler, and I. Yu. Cherepanova.
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「Okhotsk-Chukotka Volcanic Belt」の詳細全文を読む
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