中国与美国西部平均构造剪应力值的比较          下载免费PDF全文

陈培善  白彤霞  李保昆 《地震学报》2002,24(5):479-486

提出了一种估计一个地区平均构造剪应力值的方法．用这种方法，选取哈佛大学公布的1977～1999年共15 993次地震的矩张量数据，估计了美国西部19个地区、中国和邻区43个地区(每个地区为1010范围)的平均环境剪应力值．结果表明，美国西部南加州西部海域和南加州应力最高，达13.7和12.0 MPa，然后向北、向南和向东逐渐递减，但最小也达8.7 MPa，是最高值的63%．中国新疆西北部地区和西藏察隅地区应力水平最高，达17.2和12.9 MPa，比美国高．中国的华北、云南、四川、台湾和美国南加州的应力水平差不多．中国南北地震带的应力水平为13 MPa左右，比南加州略高．两个重要地区的平均剪应力值分布图，提供了地学的基本数据．这些结果可为研究地震活动的大背景提供依据，对研究强地面运动参数(如峰值加速度及反应谱等)的衰减关系也是有用的．   相似文献   

Effective stress analyses of liquefaction-induced deformation in river dikes   总被引：3，自引：0，他引：3  

O. Ozutsumi  S. Sawada  S. Iai  Y. Takeshima  W. Sugiyama  T. Shimazu 《Soil Dynamics and Earthquake Engineering》2002,22(9-12):1075-1082

A series of effective stress analyses is carried out on the seismic performance of river dikes based on the case histories during the 1993 Hokkaido-Nansei-oki and 1995 Hyogoken-Nambu earthquakes in Japan. Seven case histories selected for the analyses involve a crest settlement ranging from none to 2.7 m in the dikes 3–6 m high with evidence of liquefaction at foundation soil. The effective stress model used is based on a multiple shear mechanism and was developed by one of the authors. The soil parameters are evaluated based on the site investigation and laboratory test results. The results of the analyses are basically consistent with the observed performance of the river dikes. In particular, the effective stress model shows a reasonable capability to reproduce the varying degree of settlements depending on the geotechnical conditions of foundation soils beneath the dikes. The analyses also indicate that the effect of a cohesive soil layer mixed with the liquefiable sand layers beneath the dikes can be a primary factor for reducing the liquefaction-induced deformation of dikes.  相似文献   

Shallow seismicity, stress distribution and crustal deformation pattern in the Andaman-West Sunda arc and Andaman Sea, northeastern Indian Ocean     

M. Radha Krishna  T.D. Sanu 《Journal of Seismology》2002,6(1):25-41

Shallow seismicity and available source mechanisms in the Andaman–westSunda arc and Andaman sea region suggest distinct variation in stressdistribution pattern both along and across the arc in the overriding plate.Seismotectonic regionalisation indicates that the region could be dividedinto eight broad seismogenic sources of relatively homogeneousdeformation. Crustal deformation rates have been determined for each oneof these sources based on the summation of moment tensors. The analysisshowed that the entire fore arc region is dominated by compressive stresseswith compression in a mean direction of N23^°, and the rates ofseismic deformation velocities in this belt decrease northward from 5.2± 0.65 mm/yr near Nias island off Sumatra and 1.12 ±0.13 mm/yr near Great Nicobar islands to as much as 0.4 ±0.04 mm/yr north of 8^°N along Andaman–Nicobar islandsregion. The deformation velocities indicate, extension of 0.83 ±0.05 mm/yr along N343^° and compression of 0.19 ±0.01 mm/yr along N73^° in the Andaman back arc spreadingregion, extension of 0.18 ± 0.01 mm/yr along N125^° andcompression of 0.16 ± 0.01 mm/yr along N35^° in NicobarDeep and west Andaman fault zone, compression of 0.84 ±0.12 mm/yr N341^° and extension of 0.77 ± 0.11 mm/yralong N72^° within the transverse tectonic zone in the Andamantrench, N-S compression of 3.19 ± 0.29 mm/yr and an E-Wextension of 1.24 ± 0.11 mm/yr in the Semangko fault zone ofnorth Sumatra. The vertical deformation suggests crustal thinning in theAndaman sea and crustal thickening in the fore arc and Semangko faultzones. The apparent stresses calculated for all major events range between0.1–10 bars and the values increase with increasing seismic moment.However, the apparent stress estimates neither indicate any significantvariation with faulting type nor display any variation across the arc, incontrast to the general observation that the fore arc thrust events showhigher stress levels in the shallow subduction zones. It is inferred that theoblique plate convergence, partial subduction of 90^°E Ridge innorth below the Andaman trench and the active back arc spreading are themain contributing factors for the observed stress field within the overridingplate in this region.  相似文献   

山东海阳断裂东石兰沟段晚更新世以来地表断错特征与最大潜在地震估计   总被引：7，自引：2，他引：7       下载免费PDF全文

周本刚  冉勇康  环文林  冉洪流 《地震地质》2002,24(2):159-166

海阳断裂是胶东半岛NE向牟平 -即墨断裂带东部一条规模较大的断裂 ,尽管晚更新世以来该断裂的地表断错活动总体上已基本停息 ,但东石兰沟段在晚更新世晚期以来仍有断错地表的活动。最后一次断错地表的活动发生在距今 3 7～ 1 2万年 ,但接近 1 2万年。地表破裂长度约6 5km ,活动段长度 8km。地表断错以走滑活动为主 ,可见最大倾滑位移 0 2m ;根据断层擦痕侧伏角推测最大水平位移 1 13m。最后一次断错地表的活动若以距今 1 2万年计算 ,则最大平均倾滑速率为 0 0 17mm/a ;最大平均右旋走滑速率为 0 0 94mm/a。野外观测到该活动段的断错活动表现为突发断错 ,根据地震地表破裂参数、活动段长度与地震的关系 ,估计其最大潜在地震为 6 级  相似文献   

基于高温高压岩石破裂实验结果对中强地震前震中附近区域部分地震学现象的初步解释   总被引：6，自引：1，他引：6       下载免费PDF全文

蒋海昆  张流  周永胜  侯海峰  晁文海 《地震工程学报》2002,24(2):113-122

依据高温高压岩石破裂实验结果并结合理论分析，对 附近区域不同深度温压条件下岩石变形破坏性质及破坏失稳的力学行为进行了研究，在一次应力加载循环中，发生破坏的部位随时间具有向深部下迁的趋势。考虑到深度温压条件下岩石的渐进式破坏行为及突发失稳，对主震前震中附近区域小地震活动的增强、平静、活化等现象，以及b值等时间序列参数变化的可能机理进行初步探讨，并简单讨论了两类平静和两类b值变化的可能原因。  相似文献   

Stresses and strains in a twisted subduction zone—Fiordland, New Zealand     

Martin Reyners  Russell Robinson  Aasha Pancha  Peter McGinty 《Geophysical Journal International》2002,148(3):637-648

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Synfolding remagnetization and deformation: results from Palaeozoic sedimentary rocks in West Virginia     

Michael T. Lewchuk  Mark Evans  R. Douglas Elmore 《Geophysical Journal International》2003,152(2):266-279

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Three-dimensional elastic earthquake modelling based on integrated seismological and InSAR data: the M_w= 7.2 Nuweiba earthquake, gulf of Elat/Aqaba 1995 November     

G. Shamir  G. Baer  A. Hofstetter 《Geophysical Journal International》2003,154(3):731-744

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Average strain rate in the Italian crust inferred from a permanent GPS network – II. Strain rate versus seismicity and structural geology     

Alessandro Caporali  Silvana Martin  Matteo Massironi 《Geophysical Journal International》2003,155(1):254-268

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Microclimate, freezing tolerance, and cold acclimation along an elevation gradient for seedlings of the Great Basin Desert shrub, Artemisia tridentata     

Michael E. Loik  Sean P.Redar 《Journal of Arid Environments》2003,54(4):769-782

Vegetation, microclimate, seedling frequency, freezing tolerance, and cold acclimation were compared for seedlings of Artemisia tridentata collected from 1775, 2175, and 2575 m elevation in the eastern Sierra Nevada, California. Data were used to test the hypothesis that ecotypic differences in stress physiology are important for seedling survival along gradients from desert to montane ecosystems. The vegetation canopy cover and A. tridentata seedling frequency were greatest at 2575 m, compared to 1775 and 2175 m. Snow cover ameliorated temperatures near the soil surface for part of the winter and depth varied across elevations. Freezing tolerance was compared for seedlings maintained in growth chambers at day/night air temperatures of 25°C/15°C. The temperature at which electrolyte leakage and Photosystem II function (F_V/F_M) from leaves were half-maximum was approximately −13·5°C for leaves of seedlings from all three elevations. Shifting day/night air temperatures from 25°C/15°C to 15°C/5°C initiated about 1·5° of acclimation by plants from all three altitudes, with seedlings from the highest elevation exhibiting the greatest acclimation change. Measurements of ambient air and canopy temperatures at the three elevations indicated that wintertime average low temperatures were consistent with the measured degree of freezing tolerance. At small spatial scales used in this study, pollen and seed dispersal between study sites may have precluded resolution of ecotypic differences. Patterns of freezing tolerance and cold acclimation may depend on a combination of mesoclimate and microclimate temperatures, canopy cover, snow depth, and snow melt patterns.  相似文献