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211.
华北地区的共轭地震构造带 总被引:10,自引:3,他引:10
本文采用小地震活动图象和4.0级(Ms)以上地震震源机制资料的构造分析方法,得到一幅华北地区震源构造在地面的投影分布图,它显示4条NNE-NE向和1条NWW-NW向地震构造带交切成的共轭剪切构造格架。每条地震构造带又由一系列共轭剪切构造组成。由发生在带内的5个大震序列共轭破裂特征发现,共轭地震构造的孕震与控震作用是地震构造带形成的机制。 相似文献
212.
F. Amini 《Soil Dynamics and Earthquake Engineering》1995,14(6):439-443
Two types of clayey soils, a kaolinite and a bentonite, were tested using a resonant column apparatus under random excitation conditions. The concept of root mean square (rms) strain was utilized for the purpose of strain calculations during random loading. The conventional estimator of the transfer function was used for random vibration analysis. The effect of confinement duration (at a constant pressure) on dynamic soil properties, namely damping and shear modulus, was evaluated. The results indicate that for both cohesive soils, the effect of time was less pronounced during random vibration than sinusoidal loading at the same rms strain. This effect is however more pronounced when the peak shearing strain of sinusoidal loading is considered. Furthermore, time effects were more pronounced at low strain levels than at high strain levels. 相似文献
213.
Yoichiro Fujii 《Pure and Applied Geophysics》1995,144(1):19-37
In order to study characteristics of horizontal crustal strains, we divide the Japanese Islands into 14 tectonic provinces
consistent with the suggestion given byMatsuda (1990). We calculate frequency distribution of strain rates using the results of the Precise Control Survey initiated by
the Geographical Survey Institute in 1973. This survey is a revision of old first- and second-order triangulation networks
by trilateration. The principal axes and principal strains inside all the geodetic triangles are deduced from the comparison
of the old triangulation and the new trilateration networks. The maximum shear strain rates are calculated by dividing the
accumulated strains with the time intervals. The frequency distribution of strain rates is counted for each tectonic province
and for the entire Japanese Islands.
It is proved that the maximum shear strain rate with highest frequency ranges from 0.10–0.15 microstrain/a for 4409 data in
the Japanese Islands. The mean value of the strain rates throughout the Japanese Islands is deduced to be 0.18 microstrain/a.
We also calculated a mean value of strain rates for each tectonic province. Comparison is made between mean geodetic strain
rates in the provinces and Quaternary strain rates estimated by geomorphic data. It is found that 0.3–0.4 microstrain/a of
the highest order strain rate is now prevailing in the Izu province, the south Fossa-Magna collision zone, and some special
provinces along the eastern part of the Japan Sea coast. 相似文献
214.
对华北地区韧性剪切带几种代表上、中、下地壳深度的糜棱岩及其围岩在高温高压条件下进行纵波速度测定及各向异性研究.对实验样品的纵波速度测定得到以下结果:1.沿糜棱岩面理方向的纵波速度大于与面理垂直方向的纵波速度,差值为0.15-0.30km/s,各向异性为3%-5%;2.糜棱岩的纵波速度低于其围岩的纵波速度,差值为0.10-0.45km/s;3.中地壳角闪岩相糜棱岩的纵波速度各向异性高于上地壳绿片岩相糜棱岩和下地壳麻粒岩相糜棱岩的各向异性;4.地震波速各向异性与糜棱岩矿物优选定向有关. 相似文献
215.
BEDSHEARINEVOLVINGSCOURATACYLINDER:ATHEORETICALAPPROACHSubhasishDEY1andSrijibK.KAR2Abstract:Thetemporalvariationofshearstress... 相似文献
216.
217.
内蒙古东五分子地区韧性剪切变质作用的特征 总被引:6,自引:0,他引:6
东五分子地区花岗-绿岩地体经受了三种类型变质作用的改造。韧性剪切带不仅控制了区域变质岩组合的分布,而且也导致其变质作用的强度出现了逆转序列。根据岩石的结构、碎斑含量及矿物成分,韧性剪切变质岩划分为三类,其共同特点是具有碎斑结构。其变形结构分为单矿物型及组合型。同一块韧性剪切变质岩由处在单变平衡的一组矿物组成。根据岩石变形及重结晶的特点,结合其产状,确定出两种不同类型韧性剪切变质带。共生矿物对的研究证明它们形成于地壳不同深度及温度、压力条件。本区的金矿化、运移、沉淀与韧性剪切变质带紧密相关。 相似文献
218.
B. Stimpson 《Geotechnical and Geological Engineering》1987,5(3):299-305
Summary The shear stiffness of a grouted, rock bolt intersecting a discontinuity controls the amount of shear movement that can occur for a given shear force. In this paper an analytical model is developed for estimating the shear stiffness of a single bolt as a function of bolt inclination, hole and bolt diameter, bolt, grout and rock Young's moduli, and aperture (opening) across the discontinuity, and sensitivity studies conducted to determine the most significant of these variables as predicted by the model. 相似文献
219.
Further Studies Of Atmospheric Turbulence In Layers Near The Surface: Scaling The Tke Budget Above The Roughness Sublayer 总被引:2,自引:0,他引:2
The second of two experimental studies of the TKE budget conducted on sites of different roughness is described, and results are compared. The first took place within a shallow layer above a small field of mostly bare, cultivated soil; the second was carried out above a roughness sublayer of significant depth on an extensive plain of tall dry grass. Budget terms observed in the second study were scaled with a modified u which compensated for effects of an unusually large stress gradient and ensured that the m functions would be collinear. By showing that the modification becomes negligible in smaller gradients, it is demonstrated that in normal conditions, budgets observed above significant roughness sublayers should be normalized by scaling in terms of the unreduced Reynolds stress at the sublayer's upper surface. This procedure is shown to be consistent with the expectation that TKE budgets in layers near the surface all scale in fundamentally the same way.Other findings include: (1) the fact that most m functions previously reported are not quite collinear is attributed to a type of overspeeding known to affect three-cup anemometers; (2) revised m functions, collinear and largely free of the effects of overspeeding, are determined from a well-established characteristic of the linear m relation for the stable case; (3) data that define collinear m functions can also be represented with single hyperbolic curves; (4) dissipation is found to be 10 to 15% too small to balance total TKE production in unstable and neutral conditions and to decrease with increasing z/L in thestable regime; and (5) new relations for based on the observed behaviour of the dissipation deficit provide an improved closure for the set of equations that express the budget terms as functions of m and z/L. 相似文献
220.
具有悠久历史的石结构是砌体结构的重要组成部分,本文作者经广泛调研和试验分析:(1)提出以石粉为集料对石砌体进行抗震加固,寓环保与防灾于一体;(2)给出新型浆体配比和复合砂浆的强度等级,阐述加固技术和方法,建立灌浆石砌体抗震抗剪强度公式;(3)阐明抗震验算方法,提出基于模糊随机可靠理论的可靠性分析方法。 相似文献