1.

図書

図書
J. Reddy
出版情報: [U.S.] : McGraw-Hill Education, c2015
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2.

図書

図書
O.C. Zienkiewicz, R.L. Taylor, P. Nithiarasu
出版情報: Oxford : Butterworth-Heinemann, 2014
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3.

電子ブック

EB
Jian-Ming Jin
出版情報: Hoboken, N.J. : Wiley, c2014
オンライン: https://elib.maruzen.co.jp/elib/html/BookDetail/Id/3000097439
4.

図書

図書
O.C. Zienkiewicz, R.L. Taylor, J.Z. Zhu
出版情報: Oxford ; Tokyo : Butterworth-Heinemann, 2013
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5.

図書

図書
Soheil Mohammadi
出版情報: Chichester, West Sussex : John Wiley & Sons, 2012
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6.

電子ブック

EB
Nam-Ho Kim, Bhavani V. Sankar
出版情報: New York : J. Wiley, c2009
オンライン: https://elib.maruzen.co.jp/elib/html/BookDetail/Id/3000065304
7.

図書

図書
O.C. Zienkiewicz, R.L. Taylor, J.Z. Zhu
出版情報: Amsterdam ; Oxford ; Tokyo : Elsevier Butterworth-Heinemann, 2005
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8.

論文(リポジトリ)

論文(リポジトリ)
Howladar, M. Farhad ; Hayashi, Daigoro ; 林, 大五郎
出版情報: 情報地質 = Geological data processing (Geoinformatics).  15  pp.207-219,  2004-12-25.  日本情報地質学会
URL: http://hdl.handle.net/20.500.12000/2949
概要: The Himalayan mountain system developed from the powerful earth movements which occurred as the Indian plate pressed aga inst the Eurasian continental plate. A series of elastic finite element models are presented to examine the development of major thrusts (MCT, MBT and MFT) in the central Himalaya. Balanced geologic profiles of the central Himalaya which are modified from Johnson's profiles (2002) are used for the purpose under plane strain condition. The convergent rate of India has changed 10 cm/a at 40 Ma, 5 cm/a at 20 Ma and 2 cm/a at 10 Ma. Results show that the horizontal compressive stress σ_1 leads to the development of thrust faults in the Ththys Himalaya, Higher Himalaya, Lesser Himalaya, Sub-Himalaya and incipient zones of MCT, MBT and MFT. Especially, the thrust faults are highly concentrated within the whole area of the incipient zones, which influenced the formation of MCT, MBT and MFT at their early stage.<br />大規模な地殻の運動によって出現したヒマラヤ山系はインドプレートとユーラシア大陸プレートとの衝突によりもたらされた.ここに取り上げた一連の弾性有限要素モデルは中央ヒマラヤの主要スラスト(MCT,MBT,MFT)の発達過程を表している.Johnson(2002)によって作成された中央ヒマラヤのバランス地質断面図を多少修正したものを平面ひずみの条件のもとで使用した.インドプレートの速度を40Maでは10cm/年,20Maでは5cm/年,10Maでは2cm/年に設定した.シミュレーションの結果,水平圧縮応力σ_1はテーチスヒマラヤ,高ヒマラヤ,低ヒマラヤ,サブヒマラヤ,そしてMCT,MBT,MFTの萌芽地帯にスラストを生じさせた.特に将来MCT,MBT,MFTとなる萌芽地帯全体でのスラストの発生する領域の占める割合は高い. 続きを見る
9.

図書

図書
Victor N. Kaliakin
出版情報: New York : Marcel Dekker, 2002
シリーズ名: Civil and environmental engineering ; 9
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10.

論文(リポジトリ)

論文(リポジトリ)
Tsutsui, Shigeaki ; 筒井, 茂明
出版情報: 琉球大学工学部紀要.  pp.9-35,  2001-03.  琉球大学工学部
URL: http://hdl.handle.net/20.500.12000/2221
概要: The CATWAVES is a package of Fortran programs, based on the finite element method, for linear and nonlinear wave analyses in unbounded coastal domains. This package consists of three procedures: (I) the finite element mesh generation routines for preprocessing, (II) the finite element analysis routines of wave motion and (III) the graphics routines for post-processing. The model equation of wave motion implemented in CATWAVES is a variant of the mild-slope equation and combines the linear dispersion with weak nonlinearity. The boundary conditions applicable to the model are wave reflection along the shorelines and the boundary of coastal structures, discontinuous changes in water depth, such as occur in reef coasts, and the radiation condition at infinity. Initially, the CATWAVES imposes, on the user, preparation of two data files for the mesh generation routine, i.e., bathymetric and finite element mesh data. After preparation of these data, the system successively creates the input/output data files and leads to the final results together with high-quality graphics. 続きを見る