青藏高原西部及邻区构造应力场反演和断层滑动趋势分析     

杨颖  解朝娣  徐彦  相传芳  刘本玉 《大地测量与地球动力学》2022,42(7):694-699

基于Global CMT提供的1976-01-01~2015-12-31期间1 255个M_W≥3.5地震的震源机制解,利用FMSI方法对青藏高原西部及邻区（新疆西部地区）应力场进行反演,得到区域应力场特征,并分析西昆仑断裂带及阿尔金断裂带的断层滑动趋势。结果表明,青藏高原西部及邻区的最大主压应力轴σ1整体呈NNE-SSW向,自西向东顺时针旋转;最小主压应力轴σ3整体呈NWW-SEE向。最大主压应力轴σ1倾角大小约为5°~9°,说明该地区的构造应力场以水平运动为主。西昆仑断裂带及阿尔金断裂带具有较强的滑动趋势（T_s≥0.5）,说明西昆仑断裂带及阿尔金断裂带未来失稳滑动的可能性较大。  相似文献   

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陈连旺  詹自敏 《大地测量与地球动力学》2011,31(6):1-5

?????????????????????????????????????ó???????????????????????仯??????1???????????仯????????????????NNW-SSE??????????3~9 kPa a^-1???????????仯???????????????NEE-SWW??????????1~6 kPa a^-1?????????????????????????????????????￡?2???????????仯????????????????NNW????????????????,??????????????????????????????????仯???????????????NEE????????λ?????????????????????仯????????????????????????????????????????????п????????Щ???????????????????3?????????????????????????????????з???????????-???ε???????????????????6 kPa a^-1?????-?????ε???????????????????5 kPa a^-1???????κ??????媲????ε????????????????????3~4 kPa a^-1??  相似文献   

鲁北平原深层地下水基本特征与水环境问题          下载免费PDF全文

刘桂仪 《山东国土资源》2001,17(5):43-47

鲁北平原因超量开采地下水而引发了诸多水环境问题.本文对其分布规律和演化趋势进行了分析,并提出了对策建议.  相似文献   

麻痹性贝毒对肝脏和肾脏氧化损伤的影响     

陈雪  程金平  张鉴达  宋玉玲  王文华  于金莲 《海洋科学》2010,34(12):93-95

为了探讨麻痹性贝毒(PSP)对肝脏和肾脏损伤的机制,采用膝沟藻毒素GTX-1,4对小鼠进行急性暴露,剂量为1μg/kg,时间分别为60、90、120min。结果发现,与对照组相比,肝脏染毒组中的还原型谷胱甘肽(GSH)含量没有显著变化;在肾脏中,60 min时染毒组GSH含量没有明显变化,90、120 min时GSH含量降低;两器官中抗氧化酶(GSH-Px、SOD)活性与对照组相比均无显著变化(P0.05)。从而推断,GSH参与了PSP对肾脏损害的毒性过程;肾中GSH含量有可能作为PSP早期检测的敏感指标。  相似文献   

海涂围垦工程中悬挂式爆破挤淤基础处理技术探讨   总被引：1，自引：0，他引：1  

王文杰  赵微人  郭加根 《海岸工程》2010,29(3):51-56

沿海软土地基围涂工程中悬挂式爆破挤淤基础处理断面结构设计中遇到的最大难题是对腰宽的处理,腰宽太窄则工后沉降大,反之,则断面石方量增大,投资增加,因此,试图通过工程实例说明悬挂式爆破挤淤基础处理断面设计及工程实施过程中遇到的问题及对策措施。  相似文献   

GENETIC TYPES AND CHARACTERISTICS OF GROUND ICE IN NORTHEAST CHINA     

刘福涛  王春鹤  宋长春 《中国地理科学(英文版)》1999,9(2):166-171

１ＧＥＮＥＴＩＣＴＹＰＥＳＯＦＧＲＯＵＮＤＩＣＥＩＮＣＨＩＮＡＧｒｏｕｎｄｉｃｅｉｓｗｅｌｄｅｖｅｌｏｐｅｄｉｎｔｈｅｖｉｃｉｎｉｔｙｏｆｔｈｅｓｏｕｔｈｅｒｎｐｅｒｍａｆｒｏｓｔｌｉｍｉｔｉｎｔｈｅＥｕｒａｓｉａｎｃｏｎｔｉｎｅｎｔ，ｉｎｔｈｅｎ...  相似文献   

A virtual experiment technique on the elementary behaviour of granular materials with discrete element method     

Xia Li  Hai‐Sui Yu  Xiang‐Song Li 《国际地质力学数值与分析法杂志》2013,37(1):75-96

Multi‐scale investigations aided by the discrete element method (DEM) play a vital role for current state‐of‐the‐art research on the elementary behaviour of granular materials. Similar to laboratory tests, there are three important aspects to be considered carefully, which are the proper stress/strain definition and measurement, the application of target loading paths and the designed experiment setup, to be addressed in the present paper. Considering the volume sensitive characteristics of granular materials, in the proposed technique, the deformation of the tested specimen is controlled and measured by deformation gradient tensor involving both the undeformed configuration and the current configuration. Definitions of Biot strain and Cauchy stress are adopted. The expressions of them in terms of contact forces and particle displacements, respectively, are derived. The boundary of the tested specimen consists of rigid massless planar units. It is suggested that the representative element uses a convex polyhedral (polygonal) shape to minimize possible boundary arching effects. General loading paths are described by directly specifying the changes in the stress/strain invariants or directions. Loading can be applied in the strain‐controlled mode by specifying the translations and rotations of the boundary units, or in the stress‐controlled mode by using a servo‐control mechanism, or in the combination of the two methods to realize mixed boundary conditions. Taking the simulation results as the natural consequences originated from a complex system, virtual experiments provide particle‐scale information database to conduct multi‐scale investigations for better understanding in granular material behaviours and possible development of the constitutive theories provided the qualitative similarity between the simulation results from virtual experiments and observations on real material behaviour. Copyright © 2011 John Wiley & Sons, Ltd.  相似文献   

Tectonic Movement and Global Climate Change     

Yang Xuexiang  Chen Dianyou 《世界地质(英文版)》2000,3(2)

Glaciation between northern hemisphere and southern hemisphere were synchronous, the ice age occurred not in high but in low value of the eccentricity of the earth's orbit. Such facts went against the precession principle of the astronomical theory of ice age. The inhomogeneous distribution of climate consisted with the inhomogeneous distribution of ocean and continent. The north/south antisymmetry may be attributed to southward deviation of the thermal center and northward deviation of the mass center within the mantle demonstrated by seismic tomography. The core - mantle angular momentum makes rotational energy into thermal energy and mantle plumes erupt in the ocean bottom. The earth's deformation by tidal force makes the eruption of mantle plumes strong. They are the reason that glaciation between the Northern Hemisphere and Southern Hemisphere are synchronous and the ice age occurred in low value of the eccentricity of the earth' s orbit. The tectonic movement is playing a most important part in global climate change.  相似文献   

土压力滑楔理论的统一解   总被引：3，自引：0，他引：3  

翟越  林永亮  范文  俞茂宏 《地球科学与环境学报》2004,26(1):25-28

基于滑楔理论计算土压力的基本原理,运用考虑中间主应力效应的统一强度理论,对传统的土压力公式不能反映土体材料强度的中间主应力效应的公式进行了改进,推导了基于滑楔理论的土压力统一解公式,Coulomb和Rankine土压力公式为其特例.通过变换统一强度参数,可获得一系列的解.在工程运用中可根据土质和工程的实际情况,适当选择统一强度参数和应力状态来确定土压力的大小.  相似文献   

The effect of terrace geology on ground‐water movement and on the interaction of ground water and surface water on a mountainside near Mirror Lake,New Hampshire,USA     

Thomas C. Winter  Donald C. Buso  Patricia C. Shattuck  Phillip T. Harte  Donald A. Vroblesky  Daniel J. Goode 《水文研究》2008,22(1):21-32

The west watershed of Mirror Lake in the White Mountains of New Hampshire contains several terraces that are at different altitudes and have different geologic compositions. The lowest terrace (FSE) has 5 m of sand overlying 9 m of till. The two next successively higher terraces (FS2 and FS1) consist entirely of sand and have maximum thicknesses of about 7 m. A fourth, and highest, terrace (FS3) lies in the north‐west watershed directly adjacent to the west watershed. This highest terrace has 2 m of sand overlying 8 m of till. All terraces overlie fractured crystalline bedrock. Numerical models of hypothetical settings simulating ground‐water flow in a mountainside indicated that the presence of a terrace can cause local ground‐water flow cells to develop, and that the flow patterns differ based on the geologic composition of the terrace. For example, more ground water moves from the bedrock to the glacial deposits beneath terraces consisting completely of sand than beneath terraces that have sand underlain by till. Field data from Mirror Lake watersheds corroborate the numerical experiments. The geology of the terraces also affects how the stream draining the west watershed interacts with ground water. The stream turns part way down the mountainside and passes between the two sand terraces, essentially transecting the movement of ground water down the valley side. Transects of water‐table wells were installed across the stream's riparian zone above, between, and below the sand terraces. Head data from these wells indicated that the stream gains ground water on both sides above and below the sand terraces. However, where it flows between the sand terraces the stream gains ground water on its uphill side and loses water on its downhill side. Biogeochemical processes in the riparian zone of the flow‐through reach have resulted in anoxic ground water beneath the lower sand terrace. Results of this study indicate that it is useful to understand patterns of ground‐water flow in order to fully understand the flow and chemical characteristics of both ground water and surface water in mountainous terrain. Copyright © 2007 John Wiley & Sons, Ltd.  相似文献