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1.
依据最新的辽宁及其邻近地区地壳上地幔三维地震波速结构，并考虑地质构造、断裂以及地壳深部的构造环境等因素，建立研究区的三维地质模型；结合震源机制解与原地应力测量资料，分析区域现代地应力场特征，确定了研究区的边界约束和动力边界条件．在以上基础上，采用线弹性介质模型进行研究区三维构造应力场的有限元数值模拟，探讨研究区地壳应力场的基本特征．对比分析表明，本区地壳内应力场的三维有限元数值模拟结果与已发生的地震有着较好的对应关系，并指出了值得注意的有潜在发震可能的地震危险区． 相似文献
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ＮｕｍｅｒｉｃａｌｓｉｍｕｌａｔｉｏｎｏｆｔｈｅｃｒｕｓｔａｌｓｔｒｅｓｆｉｅｌｄｂｙｕｓｉｎｇｄａｔａｏｆｄｅｐｇｅｏｐｈｙｓｉｃａｌｅｘｐｌｏｒａｔｉｏｎｉｎｔｈｅｎｏｒｔｈｅｒｎｐａｒｔｏｆＮｏｒｔｈＣｈｉｎａＣＨＡＮＧＱＵＡＮＬＩＵ（刘... 相似文献
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Three dimensional tectonic stress field in North China 总被引：3，自引：0，他引：3
IntroductionThecrusttectonicstressfieldisoneofthekeyproblemsofgeodynamics,itsmaincontentsareaprobingintospatialdistributionanddynamicevaluationofcrusttectonicstressfield,thentracingtheevolutionprocessofcrusttectonicmovement,learningcontemporarycrusttectoniceventanditsmechanism,thuspredictingthefuturedevelopmentlawoftectonicmovement.Intheendof1970s,aseriesofpaperswerepublishedattheinternationalconferenceonMagnitudeofDeviatoricStressesintheEarth'SCrustandUppermostMantle.Theygavethebriefoutlin… 相似文献
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Based on the studies of earthquake activity, tectonic movement, crustal shortening rate, fault activity, local stress field and historical characteristics of strong earthquake activities in Xinjiang, we divide the south part of Xinjiang into 4 seismotectonic zones, namely, the eastern segment of south Tianshan seismic belt, the Kalpin block, the Kashi-Wuqia junction zone, and the west Kunlun Mountains seismic belt. Using earthquake catalogues from Xinjiang since 1900, and on the basis of integrity analysis of earthquake records in different magnitude ranges, the seismicity state of different seismotectonic zones is analyzed quantificationally by calculating the mean value of annual strain energy release, annual rate of earthquakes with different lower limits of magnitude, b-value, and the parameter m of accelerating strain release model. The characteristic indexes of seismicity state for each of the seismic tectonic zones are then determined, which provide a quantitative basis for earthquake tendency analysis and judgment. 相似文献
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本文通过对航磁异常资料进行向上解析延拓、垂向不同阶导数及磁性体边界确定新方法等处理，并结合地震震中分布对鄂尔多斯块体及邻区不同深度场源磁异常特征加以分析研究.结果表明，鄂尔多斯块体虽具有整体刚性的特征，但其内部也存在非均质性；块体东缘的华北克拉通地区经后期改造，产生近SN向的基底软弱带；青藏高原地壳缩短增厚的同时，其东北缘下地壳韧性物质分别沿秦岭、祁连两个软弱带向周缘塑性流动，而且青藏高原巨大的NE向挤压应力造成鄂尔多斯块体逆时针旋转；鄂尔多斯块体及其边界多样化的构造特征反映了不同刚性程度的地质体在外部不同应力作用下产生了显著差异的地质构造形态，这种构造形态具有继承性和叠加性. 相似文献
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大连及其邻区存在金州、庄河、大洋河等多条区域活动构造带,历史上中强地震较活跃,并有破坏怀地震发生。本文依据区域地质构造,地震活动性,地壳应力场待方面资料,讨论了该地区地震地质背景及区域构造与华北统一应力场的一致性,并据此指出了本区未来可能发生地震及应重点加强监视的地区。 相似文献
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Introduction Sichuan-Yunnan region is a major area with frequent strong earthquakes in Chinese mainland, especially the middle-southern segment of South-North Seismic Zone, where many strong earth-quakes occurred in history. In the past 30 years, Sichuan-Yunnan region has two seismically active periods: one is from Tonghai earthquake in 1970 to Longling-Songpan earthquake in 1976, the other is from Lancang earthquake in 1988 to now. During this two periods, the M=7.7 Tonghai, M=7.1 Dagua… 相似文献
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喜马拉雅构造带及其临近区域是印度板块与欧亚大陆板块挤压碰撞的前缘地带.本文利用GPS实测速度场与震源机制解数据分别计算了研究区域现今地壳岩石圈表面的GPS应变场及岩石圈内部的主应力分布,研究了印度板块持续挤压作用下板块边界带地壳岩石圈现今地壳形变的空间分布特征.结果显示,南北向的剧烈挤压变形与东西向的拉伸变形是现今青藏高原南缘地壳岩石圈的主要变形特征.其中南北向的地壳挤压变形主要集中在主前缘冲断带与雅鲁藏布江缝合带之间.东西方向上,南北走向的亚东—谷露断裂是区域地壳东西向伸展变形的重要分界断裂.75°E是研究区域地壳形变的另一条显著不连续边界,其西侧地壳主压应变强度低、方向弥散且最大主压应力方向一致性较差,而东侧地壳主压应变方向与主压应力方向以及地壳水平运动速度场方向均具有较好的一致性.布格重力异常的小波多尺度辨析结果显示该分界带与循喜马拉雅西构造结楔入欧亚大陆的印度板块密切相关. 相似文献
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本文基于SKUA-GOCAD三维建模软件平台的构造-地层实体建模流程，通过整合研究区大量地质、地球物理资料和数据利用地质时间域坐标系转换和离散光滑插值（DSI）技术，并结合非定量化的地质基础利用地质网格功能建立了郯庐断裂带江苏段新生界的三维地质构造模型，该模型包括地表、第四系底部、新近系底部和基岩顶部等四个层面的地层模型和断层模型。该模型定量化地给出了研究区第四系、新近系底界的三维结构和特征，并刻画了主要活动断裂的三维空间分布，通过该模型可以更直观地显示研究区新生代地层单元和断裂的变化规律，对深入分析活动断裂带的沉积与构造具有重要的意义。 相似文献
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11.
针对川滇地区，在大量搜集、总结前人资料和结果的基础上，建立了包括上地壳、下地壳(两层)、上地幔等4层结构的三维有限元模型. 通过反复调试，确定了其边界条件，并且计算了川滇地区背景应力场、断层蠕动产生的应力场和强震触发的应力场，以及它们的动态变化. 结果表明:后续地震大多发生在前面地震引发的库仑破裂应力正值区，前一地震对后续地震有一定的触发作用，强震是在较高的应力背景下成组发生的. 这对判断、识别地震异常，提高地震预测水平有着很大的意义. 相似文献
12.
中国大陆地壳应变能密度年变化率图像与强震活动关系的初步探讨 总被引：5，自引：0，他引：5
以现代构造应力场和地壳运动的观测结果为约束条件,利用有限元方法计算了中国大陆地壳应变能密度年变化率,三维有限元模型采用粘弹性本构关系,包含了中国大陆主要活动断裂带,在青藏高原考虑了因高海拔地势蓄集的附加重力势能和地壳山根浮力作用。 相似文献
13.
—Measurements indicate that stress magnitudes in the crust are normally limited by the frictional equilibrium on pre-existing, optimally oriented faults. Fault zones where these limitations are frequently reached are referred to as seismic zones. Fault zones in the crust concentrate stresses because their material properties are different from those of the host rock. Most fault zones are spatially relatively stable structures, however the associated seismicity in these zones is quite variable in space and time. Here we propose that this variability is attributable to stress-concentration zones that migrate and expand through the fault zone. We suggest that following a large earthquake and the associated stress relaxation, shear stresses of a magnitude sufficient to produce earthquakes occur only in those small parts of the seismic zone that, because of material properties and boundary conditions, encourage concentration of shear stress. During the earthquake cycle, the conditions for seismogenic fault slip migrate from these stress-concentration regions throughout the entire seismic zone. Thus, while the stress-concentration regions continue to produce small slips and small earthquakes throughout the seismic cycle, the conditions for slip and earthquakes are gradually reached in larger parts of, and eventually the whole, seismogenic layer of the seismic zone. Prior to the propagation of an earthquake fracture that gives rise to a large earthquake, the stress conditions in the zone along the whole potential rupture plane must be essentially similar. This follows because if they were not, then, on entering crustal parts where the state of stress was unfavourable to this type of faulting, the fault propagation would be arrested. The proposed necessary homogenisation of the stress field in a seismic zone as a precursor to large earthquakes implies that by monitoring the state of stress in a seismic zone, its large earthquakes may possibly be forecasted. We test the model on data from Iceland and demonstrate that it broadly explains the historical, as well as the current, patterns of seismogenic faulting in the South Iceland Seismic Zone. 相似文献
14.
Geng Lumin Zhang Guomin Shi YaolinCenter for Analysis Prediction Beijing China Graduate School Academia Sinica Beijing China 《中国地震研究》1995,(3)
The "field" and "source" are two important branches in seismology and earthquake research.In this paper,we use a computer model to study the relation between the field and the source in earthquake activity.In our modeling,a network of nonlinear elements is used to simulate seismic activity of seismic zones in a seismotectonic block.Constant strain rate is enforced on the boundary of the model,cyclic seismic activity,quasi-periodic variation of stress field intensity,and strain energy are observed with high and low fluctuations.There is a main seismicity area in seismic cycles,and the main seismicity area shows the spatial migration during different seismic cycles.If the precursory area is related to high element stress,it is found that the development of precursors in our model is quite complicated.No certain relation between the precursors and earthquakes has been discovered.Anomalies show different characteristics in the seismic quiet period and active period.All of the seismic zones in the system hav 相似文献
15.
新疆南部构造区带与地震活动状态研究 总被引：3，自引：0，他引：3
以地震活动为主线并依据新疆地质构造运动、地壳缩短速率、断裂活动、局部应力场及历史强地震活动特征等的研究,将新疆南部地区初步划分为南天山东段、柯坪块体、喀什—乌恰交汇区及西昆仑地震带4个地震构造区带。利用新疆1900年以来的地震记录,在不同强度地震记录完整性分析的基础上,通过计算上述各构造区带年应变能释放均值、折合震级、不同震级下限的地震年发生率、b值和应变加速释放模型参数m值等参数,对各构造区带中地震活动状态进行了定量分析,进而提取了各构造区带地震活动状态的特征指标,为地震趋势分析和判定提供了定量的依据。 相似文献
16.
本文对泉州市区域地壳结构、地质构造、构造应力场和地震活动性进行了综合分析。结果表明,泉州市在第四纪中更新世之前位于环太平洋中、新生代构造一岩浆活动带中,地壳运动频繁而又强烈,地质构造复杂;现代处于菲律宾海板块对欧亚板块挤压形成的“台湾动力触角”影响区,但区内的断裂不具全新世活动性,新构造运动不强烈,有史以来未见≥5．0级地震记载,属于地壳相对稳定区,未来遭遇6．0级地震的危险性不大,其地震破坏性影响主要来自周边孕震区,特别是东部海域,与“台湾动力触角”的作用和滨海断裂带的活动有关。 相似文献
17.
本文以构造应力场观测结果、 岩石圈流变特性为约束, 采用摩擦接触单元反映断裂带空间分段特征, 以最接近真实地下环境的非线性黏弹性材料为模型的本构关系, 建立包括安宁河—则木河—小江断裂带的三维有限元模型, 模拟在速度边界条件和重力势能等动力因素共同作用下的断裂带应力分布特性. 研究结果表明, 模拟得到的断裂带现今构造应力场与地震活动有明显的对应关系, 应力比较集中的区域, 如石棉、 西昌、 巧家、 东川附近, 极有可能是未来的地震危险区域. 相似文献
18.
Ｒｅｓｅａｒｃｈｏｎｔｅｍｐｏｒａｌａｎｄｓｐａｔｉａｌｄｉｓｔｒｉｂｕ┐ｔｉｏｎ,ｅｖｏｌｕｔｉｏｎａｒｙｃｈａｒａｃｔｅｒａｎｄｍｅｃｈａｎｉｓｍｏｆｃｒｕｓｔａｌｄｅｆｏｒｍａｔｉｏｎｆｉｅｌｄｂｅｆｏｒｅａｎｄａｆｔｅｒｔｈｅＴａｎｇｓｈａｎ... 相似文献
19.
Chen Hua-ran Chen Lian-wang Ma Hong-sheng Li Yi-qun Zhang Jie-qing He Qiao-yun Wang Jian-guo 《地震学报(英文版)》2004,17(6):625-634
Based on the latest achievement about activities of geological structure, a 3-D finite-element model containing four layers
of upper crust, lower crust (two layers) and upper mantle is established in the paper. By repeated tests and revisions, the
boundary conditions of the model are determined. And then the background stress field, the stress field caused by fault creep
and the stress field triggered by strong earthquake in Sichuan-Yunnan region, as well as their dynamic variations are calculated.
The results indicate that the latter earthquake often occurs in the area with positive Coulomb rupture stress change associated
with the former one, the former earthquake has a triggering effect on the latter one to a certain extent, and strong earthquake
often occur in groups under the background of high stress, which is of great significance for distinguishing seismic anomalies,
as well as for improving the level of earthquake prediction.
Foundation item: State Key Basic Research Project (G1998040702) and Key Project of State Science and Technology during the tenth Five-year
Plan (2001BA601B02-01-03). 相似文献
20.
利用1999—2007期和2009—2013期中国大陆GPS速度场数据,采用DEFNODE负位错反演程序估算了川滇菱形块体东边界——鲜水河—安宁河—则木河—小江断裂带在汶川地震前后的断层闭锁程度和滑动亏损空间分布动态变化特征,讨论了汶川地震对该断裂系统的影响范围和程度,并结合b值空间分布和地震破裂时-空结果分析了断裂系统的强震危险段.结果表明,汶川地震前鲜水河断裂最南端为完全闭锁(闭锁深度25km),中南段地表以下10~15km深度为强闭锁状态,中北段基本处于蠕滑状态;安宁河断裂最南端闭锁很弱,其余位置闭锁深度为10~15km;则木河断裂除最南端闭锁较弱以外,其余位置基本为完全闭锁;小江断裂在巧家以南、东川以南、宜良附近、华宁以北等四处位置闭锁较弱,其余位置为强闭锁.10年尺度的GPS速度场反演所得断层闭锁程度所指示的强震危险段,主要为鲜水河断裂道孚—八美段、安宁河断裂中段、则木河断裂中北段、小江断裂北段东川附近、小江断裂南段华宁—建水段,该结果与地质尺度的断层地震空区和30年尺度的b值空间分布所指示的危险段落具有一致性.汶川地震后断裂带远、近场速度分布和块体运动状态发生变化,这种区域地壳运动调整使得负位错模型反演得到的断裂带闭锁情况发生一定变化.汶川地震前后川滇菱形块体东边界平行断层滑动亏损速率均为左旋走滑亏损,且在安宁河断裂北端、则木河断裂中北段滑动亏损速率最大;除鲜水河断裂中南段与最南端和小江断裂东川附近以外,其余断裂震后滑动亏损速率均有所增加.垂直断层滑动亏损速率既有拉张亏损也有挤压亏损,且鲜水河断裂最南端由震前挤压转变为震后拉张,其余断裂除了安宁河断裂和小江断裂中段与最北端存在挤压滑动亏损速率外均为拉张速率. 相似文献