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EXACT SOLUTIONS OF NEAR CRACK LINE FIELDS FOR MODE I CRACK UNDER PLANE STRESS CONDITION IN AN ELASTIC-PERFECTLY PLASTIC SOLID 被引量:1
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作者 易志坚 王士杰 《Applied Mathematics and Mechanics(English Edition)》 SCIE EI 1996年第4期351-358,共8页
The near crack line analysis method has been used in the present paper,The classical small scale yielding conditions have been completely abandoned in the analyses and one inappropriate matching condition used to be u... The near crack line analysis method has been used in the present paper,The classical small scale yielding conditions have been completely abandoned in the analyses and one inappropriate matching condition used to be used at the elasticplastic boundary has been corrected.The reasonable solution of the plastic stresses near the crack line region has been established.By matching the plastic stresses with the exact elastic stresses at the elastic-plastic boundary,the plastic stresses the length of the plastic zone and the unit normal vector of the elastic-plastic boundary near the crock line region have been obtained for a mode I crack under uniaxial tension,as well as a mode I crack under biaxial tension,which shows that for both conditions the plastic stress componentsσy, and σsy.he length of the plastic zone and the unit normal vector of the elastic-plastic boundary are quite the same while the plastic stress σs is different. 展开更多
关键词 mode I plane stress crack crack line field plastic zone elastic zone
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ANISOTROPIC PLASTIC FIELDS AT A RAPIDLY PROPAGATING PLANE-STRESS CRACK-TIP
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作者 林拜松 《Applied Mathematics and Mechanics(English Edition)》 SCIE EI 1993年第1期27-40,共14页
Under the condition that all the stress components at a crack-tip are the functions of 0 only, making use of the equations of steady-state motion. Hill anisotropic yield condition and stress-strain relations, we obtai... Under the condition that all the stress components at a crack-tip are the functions of 0 only, making use of the equations of steady-state motion. Hill anisotropic yield condition and stress-strain relations, we obtain the general solution of anisotropic plastic field at a rapidly propagating plane-stress crack-tip. Applying this general solution to four particular cases of anisotropy, the general solutions of these four particular cases are derived. Finally, we give the anisotropic plastic field at the rapidly propagating plane-stress mode I crack-tip in the case of X=Y=Z 展开更多
关键词 anisotropic plastic field CRACK-TIP plane-stress
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The Plane Stress Crack-Tip Field for an Incompressible Rubber Material
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作者 高玉臣 石志飞 《Applied Mathematics and Mechanics(English Edition)》 SCIE EI 1994年第5期499-506,共8页
The crack-tip field under plane stress condition for an incompressible rubbermaterial ̄[1] is investigated by. the use of the fully nonlinear equilibrium theory. It isfound thai the crack-tip field is composed of two ... The crack-tip field under plane stress condition for an incompressible rubbermaterial ̄[1] is investigated by. the use of the fully nonlinear equilibrium theory. It isfound thai the crack-tip field is composed of two shrink sectors and one expansion se-ctor. At the crack-tip, stress and strain possess the singularity of R ̄(-1) and R ̄(-1n), respec-tively, (R is the distance to the crack-tip before deformation, n is the material const-ant). When the crack-tip is approached, the thickness of the sheet shrinks to zerowith the order of R ̄(1.4n). The results obtained in this paper are consistent with that ob-tained in [8] when s→∞ . 展开更多
关键词 incompressible material plane stress condition crack-tip field fully nonlinear equilibrium theory
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SUPPLEMENTARY STUDY ON ANISOTROPIC PLASTIC STRESS FIELDS AT A STATIONARY PLANE-STRESS CRACK-TIP
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作者 林拜松 《Applied Mathematics and Mechanics(English Edition)》 SCIE EI 1993年第5期429-436,共8页
Under the hypothesis that all the perfectly plastic stress components at a orach tip are the functions of θ only, making use of yield conditions and equilibrium equations. we derive the generally analytical expressio... Under the hypothesis that all the perfectly plastic stress components at a orach tip are the functions of θ only, making use of yield conditions and equilibrium equations. we derive the generally analytical expressions of the perfectly plastic stress field at a crack tip. Applying these generally analytical expressions to the concrete cracks, the analytical expressions of perfectly plastic stress fields at the tips of Mode Ⅰ Mode Ⅱ, Mode Ⅲ and Mixed Mode Ⅰ-Ⅱ cracks are obtained. 展开更多
关键词 plane-stress CRACK-TIP anisotropic plastic stress field general expression
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EFFECT OF THE POISSON RATIO ON THE PERFECTLY PLASTIC STRESS FIELD AT A STATIONARY PLANE-STRAIN CRACK TIP
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作者 林拜松 《Applied Mathematics and Mechanics(English Edition)》 SCIE EI 1992年第3期289-295,共7页
Under the condition that all the perfectly plastic stress components at a crack tip are the functions of ? only, making use of equilibrium equations and Von-Mises yield condition containing Poisson ratio, in this pape... Under the condition that all the perfectly plastic stress components at a crack tip are the functions of ? only, making use of equilibrium equations and Von-Mises yield condition containing Poisson ratio, in this paper, we derive the generally analytical expressions of perfectly plastic stress field at a stationary plane-strain crack tip. Applying these generally analytical expressions to the concrete cracks, the analytical expressions of perfectly plastic stress fields at the stationary tips of Mode I, Mode II and Mixed-Mode I-II plane-strain cracks are obtained. These analytical expressions contain Poisson ratio. 展开更多
关键词 Poisson ratio plane-STRAIN stationary crack-tip perfectly-plastic stress fields generally analytical expression
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Effect of Rotation, Magnetic Field and Initial Stresses on Propagation of Plane Waves in Transversely Isotropic Dissipative Half Space
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作者 Sushant Shekhar Imtiyaz A. Parvez 《Applied Mathematics》 2013年第8期107-113,共7页
The problem regarding the reflection of plane waves in a transversely isotropic dissipative medium is considered, in which we are studying about the reflection of incidence waves in initially stressed dissipative half... The problem regarding the reflection of plane waves in a transversely isotropic dissipative medium is considered, in which we are studying about the reflection of incidence waves in initially stressed dissipative half space. After solving the governing equations, we find the two complex quasi-P (qP) and quasi-SV (qSV) waves. The occurrence of reflected waves is studied to calculate the reflection coefficient and the energy partition of incidence wave at the plane boundary of the dissipative medium. Numerical example is considered for the reflection coefficient and the partition of incident energy, in which we study about the effect of rotation, initial stresses and magnetic field. 展开更多
关键词 Magnetic field Initial stress ROTATION REFLECTION of plane WAVES REFLECTION COEFFICIENTS Energy Ratios
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Three dimensional K-Tz stress fields around the embedded center elliptical crack front in elastic plates 被引量:2
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作者 Junhua Zhao Wanlin Guo Chongmin She Bo Meng 《Acta Mechanica Sinica》 SCIE EI CAS CSCD 2006年第2期148-155,共8页
Through detailed three-dimensional (3D) finite element (FE) calculations, the out-of-plane constraints Tz along embedded center-elliptical cracks in mode I elastic plates are studied. The distributions of Tz are o... Through detailed three-dimensional (3D) finite element (FE) calculations, the out-of-plane constraints Tz along embedded center-elliptical cracks in mode I elastic plates are studied. The distributions of Tz are obtained near the crack front with aspect ratios (a/c) of 0.2, 0.4, 0.5, 0.6, 0.8 and 1.0. Tz decreases from an approximate value of Poisson ratio v at the crack tip to zero with increasing normalized radial distances (r/a) in the normal plane of the crack front line, and increases gradually when the elliptical parameter angle φ changes from 0° to 90°at the same r/a. With a/c rising to 1.0, Tz is getting nearly independent of φ and is only related to r/a. Based on the present FE calculations for Tz, empirical formulas for Tz are obtained to describe the 3D distribution of Tz for embedded center-elliptical cracks using the least squares method in the range of 0.2 ≤ a/c ≤ 1.0. These Tz results together with the corresponding stress intensity factor K are well suitable for the analysis of the 3D embedded centerelliptical crack from field, and a two-parameter K-Tz principle is proposed. 展开更多
关键词 Three-dimensional finite element Out-of-plane constraint Tz Embedded elliptical crack stress intensity factor T-stress stress field
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MODE Ⅰ AND MODE Ⅱ CRACK TIP ASYMPTOTIC FIELDS WITH STRAIN GRADIENT EFFECTS 被引量:1
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作者 陈少华 王自强 《Acta Mechanica Sinica》 SCIE EI CAS CSCD 2001年第3期269-280,共12页
The strain gradient effect becomes significant when the size of frac- ture process zone around a crack tip is comparable to the intrinsic material length l, typically of the order of microns. Using the new strain grad... The strain gradient effect becomes significant when the size of frac- ture process zone around a crack tip is comparable to the intrinsic material length l, typically of the order of microns. Using the new strain gradient deformation theory given by Chen and Wang, the asymptotic fields near a crack tip in an elastic-plastic material with strain gradient effects are investigated. It is established that the dom- inant strain field is irrotational. For mode Ⅰ plane stress crack tip asymptotic field, the stress asymptotic field and the couple stress asymptotic field can not exist si- multaneously. In the stress dominated asymptotic field, the angular distributions of stresses are consistent with the classical plane stress HRR field; In the couple stress dominated asymptotic field, the angular distributions of couple stresses are consistent with that obtained by Huang et al. For mode Ⅱ plane stress and plane strain crack tip asymptotic fields, only the stress-dominated asymptotic fields exist. The couple stress asymptotic field is less singular than the stress asymptotic fields. The stress asymptotic fields are the same as mode Ⅱ plane stress and plane strain HRR fields, respectively. The increase in stresses is not observed in strain gradient plasticity for mode Ⅰ and mode Ⅱ, because the present theory is based only on the rotational gradi- ent of deformation and the crack tip asymptotic fields are irrotational and dominated by the stretching gradient. 展开更多
关键词 strain gradient effect crack tip asymptotic field plane stress plane strain
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Stress value in 2003 Dayao Ms6.1 earthquake source region
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作者 Xiaofeng Xu Yongge Wan Huilin Wang 《Earthquake Science》 CSCD 2011年第4期343-350,共8页
The Ms6.2 Dayao, Yunnan, earthquake occurred on July 21, 2003, followed by a major Ms6.1 earthquake about 88 days later in the same region. Hypocenters of the two earthquakes are almost in the same place. Based on the... The Ms6.2 Dayao, Yunnan, earthquake occurred on July 21, 2003, followed by a major Ms6.1 earthquake about 88 days later in the same region. Hypocenters of the two earthquakes are almost in the same place. Based on the P wave first motion polarities of the two aftershock sequences recorded by temporary stations, we have studied the stress field in the aftershock zone and obtained the two stress field directions in Dayao region using the new version of PKU_Grid^Test Software provided by Chunquan Yu. Assuming that the rotation of the stress field is caused by the second main shock, we estimated the crustal stress value in the focal region by using the stress value calculation method proposed by Yongge Wan. The estimated maximum, intermediate and minimum principal stresses are 166.3 MPa, 158.7 MPa and 151 MPa, respectively, before the second main shock. The normal and shear stresses projected on the fault plane of the second main shock before it occurred are 157.3 MPa, 7.4 MPa, and are 158.8 MPa, 0.2 MPa after it occurred, respectively. The perturbed input parameters experiments attest the stability of the solution. The result shows that the preseismic shear stress is larger than the post-seismic one, and their difference corresponds to the stress drop approximately. The estimated compressive stress level is very high, but the differential stress is low. The result is helpful for friction coefficient estimation, plate motion simulation and related studies. 展开更多
关键词 composite fault plane solution stress field stress magnitude 2003 Dayao twin earthquake
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PLANE PROBLEMS OF A FINITE DISC CONTAINING AN INTERNAL CRACK
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作者 尹昌言 祖承德 《Applied Mathematics and Mechanics(English Edition)》 SCIE EI 1990年第10期921-930,共10页
Using complex variable methods in elasticity, this paper deals with the plane problems ot a finite disc containing an internal linear crack at any position under general loads, obtains the general forms of Complex str... Using complex variable methods in elasticity, this paper deals with the plane problems ot a finite disc containing an internal linear crack at any position under general loads, obtains the general forms of Complex stress functions and stress-intensity tactors expressed in terms of series, and to these problems disiusses three sposial cases,i.e.the cases of the crack under a uniform pressure, a uniform shear stress and the use of the dise rotating uniformly. In these cases the approximate formulas calcidating the stress-intensity factors are also presented. The calculated results shun that for the middle and.small orachs situated inside the disc and not near the external boundary,these approximate formulas give good or better approximation. 展开更多
关键词 plane problem disc containing a crack stress-intensity factor stress field displacement Held
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盖州青石岭震群断层面参数的确定及构造应力场特征研究
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作者 戴盈磊 张文静 +2 位作者 惠杨 底欣欣 杨晓东 《防灾减灾学报》 2024年第1期1-8,共8页
根据之前学者的双差定位结果,使用Fit_Fault软件包计算盖州青石岭震群发震断层面走向为114.30°,倾角74.67°。收集2001年至2011年辽宁地区的震源机制解资料,采用全局网格搜索算法,反演该地区的构造应力场,其主压应力轴为NEE向... 根据之前学者的双差定位结果,使用Fit_Fault软件包计算盖州青石岭震群发震断层面走向为114.30°,倾角74.67°。收集2001年至2011年辽宁地区的震源机制解资料,采用全局网格搜索算法,反演该地区的构造应力场,其主压应力轴为NEE向,主张应力轴为NNW向,整体呈现拉张的应力状态。并据此确定出青石岭震群发震断层的滑动角是35.49°,为左旋走滑性质。模拟在辽宁地区构造应力体系下各种产状的断层面上可产生的相对剪应力和相对正应力分布情况,发现该震群发震断层面上的相对剪应力和相对正应力分别为0.513和0.576。分析认为盖州青石岭震群是一处地质薄弱带,背景构造应力场在其最近一期的活动中未起主导作用。 展开更多
关键词 青石岭震群 断层面参数 震源机制解 应力场 辽宁地区
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2020年唐山古冶M_(S)5.1地震发震构造及应力触发研究
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作者 靳志同 周明月 +2 位作者 白梓明 刘佳璐 余海琳 《地震地磁观测与研究》 2024年第6期2-13,共12页
2020年7月12日唐山古冶发生M_(S)5.1地震,对其发震断层几何形状和滑动性质,以及后续余震的应力触发进行研究,主要得到以下结论:①发震构造:基于收集的古冶震源区地震精定位结果,使用改进的模糊聚类分析方法,计算得到断层的几何形状和断... 2020年7月12日唐山古冶发生M_(S)5.1地震,对其发震断层几何形状和滑动性质,以及后续余震的应力触发进行研究,主要得到以下结论:①发震构造:基于收集的古冶震源区地震精定位结果,使用改进的模糊聚类分析方法,计算得到断层的几何形状和断层空间分布,其中断层走向为230.2°,倾角为86.2°;基于震源机制得到该地区构造应力场,并将构造应力场投影到发震断层面上,得到该地震发震断层滑动角,数值为-177.2°。②应力触发:基于经验公式,得到该地震破裂模型,其断层长为3.9 m,宽为4.4 m,断层滑动量为1.9 cm;基于破裂模型和PSGRN/PSCMP软件包,计算该地震对M_(S)4.3余震和其他余震的应力触发,结果显示:不同深度上的主震对余震的应力触发不同,其中,主震在12 km深度上对余震的应力触发比例最高;在计算主震对M_(S)4.3余震的应力触发时,发现其位于主震引起的库仑应力变化为正的区域,表明该地震受到M_(S)5.1地震的触发作用。本研究结果对研究和了解唐山震源区地震断层的发震构造以及地震危险性具有一定意义。 展开更多
关键词 古冶M_(S)5.1地震 断层面拟合 应力场 应力触发
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福建仙游震群的应力场及其成因分析
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作者 余海琳 万永革 +2 位作者 崔华伟 王晓山 黄少华 《地震学报》 CSCD 北大核心 2024年第4期600-619,共20页
利用双差定位法对2010年8月1日至2014年12月31日福建仙游地区中国地震台网中心记录到的地震群进行重定位,并采用P波初动的方法求解出该震群的159个震源机制解,显示该震群的震源机制解结果与背景构造应力场表现明显不一致。为了进一步探... 利用双差定位法对2010年8月1日至2014年12月31日福建仙游地区中国地震台网中心记录到的地震群进行重定位,并采用P波初动的方法求解出该震群的159个震源机制解,显示该震群的震源机制解结果与背景构造应力场表现明显不一致。为了进一步探究差异性存在的原因,将得到的震群震源机制解结果分区域和分深度求解应力场,结果显示:金钟水库的东南部附近应力方向更远离背景构造应力方向,并且应力形因子小于0.5,中间轴呈现为拉张应力;随着深度的增加,应力场的方向也更接近背景构造应力场的方向。此外,根据前人研究推断该区域应力方向发生偏转是由于太平洋板块在深部的低角度俯冲挤压导致浅部张开,应力呈现为东西向拉张所致。在上述两原因的共同作用下,使得经震源机制解反演出的应力场结果与背景应力场差别较大。 展开更多
关键词 双差定位 断层面拟合 震源机制解 应力场
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复杂应力场中圆形隧洞偏应力场分布规律 被引量:1
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作者 安学旭 郭新天 +1 位作者 赵力将 黄荣宾 《科技和产业》 2024年第13期122-132,共11页
为了厘清深部圆形中导洞(设置于双向隧洞中间)围岩偏应力分布问题,结合岩石力学与摩尔-库仑屈服准则,推导平面三向应力场中圆形隧洞围岩主偏应力与塑性区半径解析解,研究不同工况下圆形隧洞围岩主偏应力的分布规律及塑性区边界处主偏应... 为了厘清深部圆形中导洞(设置于双向隧洞中间)围岩偏应力分布问题,结合岩石力学与摩尔-库仑屈服准则,推导平面三向应力场中圆形隧洞围岩主偏应力与塑性区半径解析解,研究不同工况下圆形隧洞围岩主偏应力的分布规律及塑性区边界处主偏应力的几何形态分布特征。结果表明:当隧洞所处的斜向应力场为竖向应力场0.5~1.0倍时,随着斜向应力场水平方位角α_(1)=α_(2)增加,径向1.0倍隧洞半径范围内顶底主偏应力在快速降低,腰部主偏应力在快速增加,径向1.0倍隧洞半径范围外隧洞围岩主偏应力先小幅下降后又逐渐增大,最终在围岩深部趋于某定值;隧洞围岩主偏应力对其塑性区形态分布影响显著,当斜向应力场水平方位角α_(1)=α_(2)为30°时,围岩塑性区形态分布较优,为圆形或椭圆形。 展开更多
关键词 平面三向应力场 围岩偏应力场 理论解析 塑性区形态特征
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从震源机制中准确识别发震断层面对重构应力场的意义
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作者 李振月 万永革 +1 位作者 郭祥云 刘瑞丰 《地球物理学报》 SCIE EI CAS CSCD 北大核心 2024年第7期2612-2624,共13页
基于震源机制的应力场反演,需要从震源机制的两个节面中准确地识别出发震断层面,然后通过拟合发震断层面的滑动方向获得应力场.然而,目前的技术和方法不能保证能够从所有的震源机制中准确地识别出发震断层面.因此,用于应力场反演的断层... 基于震源机制的应力场反演,需要从震源机制的两个节面中准确地识别出发震断层面,然后通过拟合发震断层面的滑动方向获得应力场.然而,目前的技术和方法不能保证能够从所有的震源机制中准确地识别出发震断层面.因此,用于应力场反演的断层数据中会参入小部分辅助断层面,这部分假断层的存在会造成重构的应力场与实际应力场产生多大程度的偏离?本文通过合成实验揭示出,从部分震源机制中错误地选择断层面可能会造成重构的应力场方向和主应力相对大小(R)与实际产生较大偏离,重构应力场的偏离程度主要与实际的应力R值、错误选择断层面的震源机制所占的比例以及震源机制中包含的噪声大小这三个因素有关.当实际的应力R值为中间值附近时,只有准确地选择断层面才能准确地重构R值,当实际的应力R值较小时,准确地选择断层面有助于准确地重构应力方向,故准确地从震源机制中选择断层面可以保证在不同的背景应力场下都能准确地重构应力场方向和R值,这对于根据重构的应力场合理解释构造运动具有重要意义. 展开更多
关键词 震源机制 重构应力场 识别发震断层面 主应力相对大小
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2024年1月23日新疆阿克苏地区乌什县M S7.1地震对周围断层的应力影响及对余震的触发作用
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作者 宋泽尧 万永革 +2 位作者 关兆萱 顾培苑 王润妍 《地震工程学报》 CSCD 北大核心 2024年第4期982-991,共10页
为研究2024年新疆阿克苏地区乌什县M S7.1大震对周边区域应力的影响,基于美国地质调查局(USGS)给出的主震破裂模型,计算此次地震对周边地区产生的同震位移场及应变场,结果发现:体应变在震源西北侧呈现拉张,东南侧呈现挤压;面应变的分布... 为研究2024年新疆阿克苏地区乌什县M S7.1大震对周边区域应力的影响,基于美国地质调查局(USGS)给出的主震破裂模型,计算此次地震对周边地区产生的同震位移场及应变场,结果发现:体应变在震源西北侧呈现拉张,东南侧呈现挤压;面应变的分布与体应变的形态基本相似。为研究该地震对余震的触发情况,首先需要确定接收断层的断层面参数,对中国地震台网发布的2024年1月23日到2024年4月10日的余震震源机制节面聚类分析,得到两簇结果,选择标准差较小的二簇节面进行平均,得到走向为243.91°,倾角为64.97°;将乌什地震震源区的构造应力场投影到该发震断层上,得到滑动角为61.02°。将这些参数作为余震接收断层的断层面参数,同样基于USGS给出的主震断层破裂模型,计算主震产生的静态库仑应力,研究发现:区内库仑应力均超过0.01 MPa阈值,且库仑破裂应力最大值达0.3 MPa,大多数余震处于库仑应力变化的高值区;表明主震产生的静态库仑应力促进了余震的发生。为研究该地震发生对周围断层的影响,根据前人给出的周边断层的几何和滑动特性,计算在周边断裂上沿滑动方向上的库仑破裂应力变化,研究发现:本次地震对迈丹—沙依拉姆断裂库仑应力最大增加量达到0.22 MPa,喀拉铁克断裂、衣木干他乌断裂、塔塔埃尔塔格断裂、奥兹格尔他乌断裂、柯坪断裂的库仑应力变化并不明显,迈丹—沙依拉姆断裂库仑应力增加最大,应注意该断层的地震活动性。 展开更多
关键词 2024年乌什县M S7.1地震 发震断层面 位移场 应变场 静态库仑应力
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微动磨损形貌与接触应力场耦合机制仿真分析
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作者 韩怡茗 李欣 +1 位作者 刘乐强 杨建伟 《机床与液压》 北大核心 2024年第19期135-140,共6页
微动磨损是影响机械关键结构的主要失效形式。为研究磨损形貌和应力场的演化过程及耦合机制,利用ABAQUS软件建立柱面/平面有限元接触模型,并基于Archard磨损公式对微动磨损形貌与接触应力场演化过程进行仿真,进一步对微动磨损过程中磨... 微动磨损是影响机械关键结构的主要失效形式。为研究磨损形貌和应力场的演化过程及耦合机制,利用ABAQUS软件建立柱面/平面有限元接触模型,并基于Archard磨损公式对微动磨损形貌与接触应力场演化过程进行仿真,进一步对微动磨损过程中磨损形貌和应力场的耦合机制进行分析。仿真结果表明:局部滑移下,磨损形貌呈“W”形,随着循环次数增加,接触宽度和磨损深度略有增加,接触区最大正应力和切应力略有增大;全局滑移下,磨损形貌呈“U”形,随着循环次数增加,磨损形貌显著变宽、变深,接触区正应力和切应力的应力场分布逐渐变宽变扁。 展开更多
关键词 微动磨损 接触应力场 耦合机制 柱面/平面 Archard模型
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High Order Asymptotic Field for Plane Stress Crack Problem
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作者 李松涛 王自强 《Science China Mathematics》 SCIE 1993年第9期1073-1083,共11页
This paper presents an exact analysis for high order asymptotic field of theplane stress crack problem.It has been shown that the second order asymptotic field is notan independent eigen field and should be matched wi... This paper presents an exact analysis for high order asymptotic field of theplane stress crack problem.It has been shown that the second order asymptotic field is notan independent eigen field and should be matched with the elastic strain term of the firstorder asymptotic field.The second order stress field ahead of the crack tip is quite smallcompared with the first order stress field.The stress field ahead of crack tip is character-ized by the HRR field.Hence the J integral can be used as a criterion for crack initiation. 展开更多
关键词 plane stress high order ASYMPTOTIC field J INTEGRAL elasto-plastieity
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日本海—鄂霍次克海下俯冲带的应力状态及其深部形变 被引量:12
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作者 臧绍先 吴忠良 宁杰远 《地球物理学报》 SCIE EI CAS CSCD 北大核心 1992年第5期560-573,共14页
通过地震分布及地震机制解所反映的日本海—鄂霍次克海俯冲带的形态及应力状态,研究了俯冲带深部形变及650km间断面的穿透问题.日本海Benioff带较直,连续性较好;鄂霍次克海Benioff带弯度稍大,220—320km深度之间地震很少.两俯冲带在浅... 通过地震分布及地震机制解所反映的日本海—鄂霍次克海俯冲带的形态及应力状态,研究了俯冲带深部形变及650km间断面的穿透问题.日本海Benioff带较直,连续性较好;鄂霍次克海Benioff带弯度稍大,220—320km深度之间地震很少.两俯冲带在浅部及深部地震密集,100—200km深度之间有双地震层.应力状态随深度变化,200km深度以下P,T轴方向相对集中,P轴接近俯冲方向,在约100—200km深度附近,P,T轴均接近俯冲方向.观测和理论地震图拟合分析表明,地震断层面走向接近俯冲带走向,断裂的结果使俯冲带在深部倾角变小. 展开更多
关键词 俯冲带 震源机制 应力场 形变 地震
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江西永平铜矿火烧岗岩体中流体包裹体面研究 被引量:5
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作者 吕赟珊 朱筱婷 +1 位作者 蔡逸涛 解国爱 《南京大学学报(自然科学版)》 CSCD 北大核心 2012年第3期316-327,共12页
江西永平铜矿区的火烧岗岩体是燕山早期侵入的似斑状黑云母花岗岩,这一时期的岩浆热液活动对该区的成矿有重要意义.通过对花岗岩中流体包裹体面(FIP)的研究,可以揭示火烧岗岩体在侵位冷缺过程中受到的区域应力场变化及受应力控制的流体... 江西永平铜矿区的火烧岗岩体是燕山早期侵入的似斑状黑云母花岗岩,这一时期的岩浆热液活动对该区的成矿有重要意义.通过对花岗岩中流体包裹体面(FIP)的研究,可以揭示火烧岗岩体在侵位冷缺过程中受到的区域应力场变化及受应力控制的流体运移和演化特征.流体包裹体面产状数据显示,火烧岗岩体中FIP主要发育NEE向和NW向两个优势方位,且两组方向FIP的倾角近于直立,其中NEE向FIP的形成早于NW向,推断火烧岗岩体在侵位过程中先后受到NNW向的水平拉张构造应力场和NW向的挤压构造应力场.相对应的构造事件为古太平洋板块向华南板块之下俯冲造成大陆腹地发生从局部拉张到挤压的构造转换.显微测温数据表明,两期FIP中的流体包裹体主要类型都为NaCl-H2O-CO2(N2)包裹体,少部分为NaCl-H2O包裹体,流体演化的总体趋势为早期高温度、高盐度、低密度型流体向晚期低温度、低盐度、高密度型流体演化. 展开更多
关键词 火烧岗岩体 流体包裹体面 构造应力场 永平铜矿
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