翻訳と辞書 Words near each other ・ 1848 in Norway ・ 1848 in paleontology ・ 1848 in philosophy ・ 1848 in poetry ・ 1848 in rail transport ・ 1848 in science ・ 1848 in Scotland ・ 1848 in South Africa ・ 1848 in Spain ・ 1848 in sports ・ 1848 in Sweden ・ 1848 in Switzerland ・ 1848 in the United Kingdom ・ 1848 in the United States ・ 1848 in Wales ・ 1848 Marlborough earthquake ・ 1848 Naval Air Squadron ・ 1848 Tampa Bay hurricane ・ 1848 Whig National Convention ・ 1848–49 massacres in Transylvania ・ 1849 ・ 1849 Baden Revolution ・ 1849 English cricket season ・ 1849 Grand National ・ 1849 in archaeology ・ 1849 in architecture ・ 1849 in art ・ 1849 in Australia ・ 1849 in birding and ornithology ・ 1849 in Canada 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 1848 Marlborough earthquake ： ウィキペディア英語版 1848 Marlborough earthquake The 1848 Marlborough earthquake is the name associated with a severe earthquake which occurred at 1:40 a.m. on 16 October 1848 and whose epicenter was in the Marlborough region of the South Island of New Zealand. In Wellington the shaking lasted for about two minutes and caused widespread damage, especially to brick- or stone- built structures. Most of the buildings damaged in the earthquake were rebuilt in wood and this contributed to the relatively low level of damage and loss of life in the more powerful Wairarapa earthquake that hit Wellington seven years later. ==Tectonic setting== New Zealand lies along the boundary between the Australian and Pacific Plates. In the South Island most of the relative displacement between these plates is taken up along a single dextral (right lateral) strike-slip fault with a major reverse component, the Alpine Fault. In the North Island, the displacement is mainly taken up along the Kermadec subduction zone, although the remaining dextral strike-slip component of the relative plate motion is accommodated by the North Island Fault System (NIFS).〔(Mouslopoulou,V., Nicol,A., Little, T.A. & Walsh, J.J. 2007. Terminations of large strike-slip faults: an alternative model from New Zealand. In: Cunningham, W. D. & Mann, P (eds).Tectonics of Strike-Slip Restraining and Releasing Bends. Geological Society of London, Special Publication, 290; p. 387–415. )〕 A group of dextral strike-slip structures, known as the Marlborough Fault System, transfer displacement between the mainly transform and convergent type plate boundaries in a complex zone at the northern end of South Island.〔(Van Dissen, R. & Yeats, R.S. 1991. Hope Fault, Jordan Thrust, and uplift of the Seaward Kaikoura Range, New Zealand. Geology, 19, 393–396 ).〕 The earthquake occurred on the Awatere Fault which is part of the Marlborough Fault System.〔(Grapes, R., Little, T. & Downes, G. 1998. Rupturing of the Awatere Fault during the 1848 October 16 Marlborough earthquake, New Zealand: historical and present day evidence, New Zealand Journal of Geology & Geophysics, 1998, Vol. 41: 387–399 )〕 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「1848 Marlborough earthquake」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.