翻訳と辞書 Words near each other ・ Thin Wires in the Voice ・ Thin-film bulk acoustic resonator ・ Thin-film composite membrane ・ Thin-film diode ・ Thin-film drug delivery ・ Thin-film interference ・ Thin-film memory ・ Thin-film optics ・ Thin-film solar cell ・ Thin-film thickness monitor ・ Thin-film transistor ・ Thin-film-transistor liquid-crystal display ・ Thin-layer chromatography ・ Thin-le-Moutier ・ Thin-shell structure ・ Thin-skinned deformation ・ Thin-slicing ・ Thin-wall injection molding ・ Thina ・ Thinadhoo ・ Thinadhoo (Gaafu Dhaalu Atoll) ・ Thinadhoo (Vaavu Atoll) ・ Thinai ・ Thinaia ・ Thinakaran ・ Thinakkural ・ Thinali ・ Thinan-malkia ・ ThinBasic ・ Thinbaw 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 Thin-skinned deformation ： ウィキペディア英語版 Thin-skinned deformation Thin-skinned deformation is a style of deformation in plate tectonics at a convergent boundary which occurs with shallow thrust faults that only involves cover rocks (typically sedimentary rocks), and not deeper basement rocks.〔Davidson et al., 1997, Exploring Earth, An Introduction to Physical Geology, ISBN 0-13-463936-7〕 The thin-skinned style of deformation is typical of many fold and thrust belts developed in the foreland of a collisional zone or back arc of a continental volcanic arc. This is particularly the case where a good basal decollement exists, usually in a weaker layer like a shale, evaporite, or a zone of high pore fluid pressure.〔(Hatcher, R.D. 2007. Confirmation of Thin-skinned Thrust Faulting in Foreland Fold-Thrust Belts and Its Impact on Hydrocarbon Exploration: Bally, Gordy, and Stewart, Bulletin of Canadian Petroleum Geology, 1966. First in the AAPG History of Petroleum Geology Series on Papers Having a Major Impact on Petroleum Geology: A contribution of the AAPG History of Petroleum Geology Committee )〕 This was first described in Rocky Mountains of the United States, as part of the Sevier Orogeny. In the rock record, this will increase the influence of more surficial rocks, which usually includes sedimentary rocks. Typically, you will see repeated sections of the same rock over and over as thrust faults, coming up from the decollement, stack the same layer on top of itself. The sediments that are created by this type of deformation are typically lithic sandstones. ==See also== *Thick-skinned deformation *Fold and thrust belts 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「Thin-skinned deformation」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.