HORIZONTAL LITHOSPHERE COMPRESSION AND SUBDUCTION - CONSTRAINTS PROVIDED BY PHYSICAL MODELING

NCU Institutional Repository > 地球科學學院 > 地球物理研究所 > 期刊論文 > Item 987654321/27617

jsp.display-item.identifier=請使用永久網址來引用或連結此文件: http://ir.lib.ncu.edu.tw/handle/987654321/27617

题名:	HORIZONTAL LITHOSPHERE COMPRESSION AND SUBDUCTION - CONSTRAINTS PROVIDED BY PHYSICAL MODELING
作者:	SHEMENDA,AI
贡献者:	地球物理研究所
关键词:	INTRAPLATE DEFORMATION;OCEANIC LITHOSPHERE;INDIAN-OCEAN;PLATE;TECTONICS;SEISMICITY;JUNCTION;TRENCH;BASIN;AREA
日期:	1992
上传时间:	2010-06-29 18:42:02 (UTC+8)
出版者:	中央大學
摘要:	Physical modeling of the subduction is performed with a two-layered mantle model (elastico-plastic lithosphere and low-viscosity asthenosphere) and is governed by the criteria of similarity. Compression of the lithosphere in the area of a passive continental margin has been shown to produce a buckling instability in the oceanic plate with wavelengths of 200 km on the average. Later, a localization of deformation occurs in sagging at some distance from the margin where a strongly dislocated linear ridge is formed due to the thrusting. The plate then experiences a failure along the inclined zone, and subduction starts. The inner trench slope which forms therefore has a scraped structure and include a block of crushed and dislocated oceanic crust and sediments in the lower section. If there is an old inclined fault striking across the compression of an oceanic lithosphere, it is on that fault that a subduction zone is initiated. The inner trench slope has then a different structure and forms, due to normal faulting, in the frontal part of the overriding plate. The formation of a subduction zone requires a compression that is smaller than that in the preceding case by a factor of 2 or 3. The subducting plate experiences an elastico-plastic bending and (under specific conditions) thrusting along the zone, dipping from under the overriding plate oceanward and crossing the entire lithosphere. The best agreement between generalized relief in subduction zone in the model and nature is achieved when a shear yield limit tau(s) = 1.3 x 10(8) Pa, modulus of elasticity E about a few times 10(11) Pa, and a thickness H = 60 km, are adopted for the real lithosphere.
關聯:	JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
显示于类别:	[地球物理研究所] 期刊論文

文件中的档案:

档案	描述	大小	格式	浏览次数
index.html		0Kb	HTML	1178	检视/开启

在NCUIR中所有的数据项都受到原著作权保护.

社群 sharing

数据加载中.....