共查询到20条相似文献，搜索用时 31 毫秒
1.
Scattering of wavefields in a 3-D medium that includes passive and/or active structures, is numerically solved by using the boundary integral equation method (BIEM). The passive structures are velocity anomalies that generate scattered waves upon incidence, and the active structures contain endogenous fracture sources, which are dynamically triggered by the dynamic load due to the incident waves. Simple models are adopted to represent these structures: passive cracks act as scatterers and active cracks as fracture sources. We form cracks using circular boundaries, which consist of many boundary elements. Scattering of elastic waves by the boundaries of passive cracks is treated as an exterior problem in BIEM. In the case of active cracks, both the exterior and interior problems need to be solved, because elastic waves are generated by fracturing with stress drop, and the growing crack boundaries scatter the incident waves from the outside of the cracks. The passive cracks and/or active cracks are randomly distributed in an infinite homogeneous elastic medium. Calculations of the complete waveform considering a single scatter show that the active crack has weak influence on the attenuation of first arrivals but strong influence on the amplitudes of coda waves, as compared with those due to the passive crack. In the active structures, multiple scattering between cracks and the waves triggered by fracturing strongly affect the amplitudes of first arrivals and coda waves. Compared to the case of the passive structures, the attenuation of initial phase is weak and the coda amplitudes decrease slowly. 相似文献
2.
Interpretation of transient electromagnetic soundings over three-dimensional structures for the central-loop configuration 总被引：2，自引：0，他引：2
Gregory A. Newman Walter L. Anderson Gerald W. Hohmann 《Geophysical Journal International》1987,89(3):889-914
Summary. An assessment is made of the bias of fitting constrained layered-earth models to transient electromagnetic data obtained over 3-D structures. In this assessment we use the central-loop configuration and show that accurate estimates of the depth of burial of 3-D structures can be obtained with layered-earth model fitting. However, layered-earth interpretations are not reliable for estimating depth extents and resistivities of 3-D structures. When layered earths are used for interpretation, it is advantageous in some cases to use data based on the magnetic field instead of the voltage. A magnetic-field definition of apparent resistivity, in contrast to a definition based on the voltage, eliminates apparent-resistivity overshoots and undershoots in the data. A resistivity undershoot in the data can produce an extraneous and misleading layer in an interpretation of a 3-D resistive structure. Due to 3-D effects, apparent-resistivity soundings (magnetic field and voltage) may rise so steeply at late times that it may not be possible to fit a sounding to a reasonable layered-earth model. Truncating such a sounding, over a buried conductor, allows for a reasonable layered-earth fit and an accurate estimate of the depth to the conductor. However, the resistivity of the conductor is overestimated.
Measurements of the horizontal field in the central-loop configuration can map 3-D structures, provided the sensor is located accurately at the centre of the transmitting loop. Horizontal-field calculations show that the transients peak on the flanks of a 3-D structure, but are depressed over the structure's centre. Weak transient responses flanked by two large transient responses, which are opposite in sign, locate the structure. The sign reversal is caused by a corresponding reversal in the currents that are channelled through or deflected away from conductive or resistive structures, respectively. 相似文献
Measurements of the horizontal field in the central-loop configuration can map 3-D structures, provided the sensor is located accurately at the centre of the transmitting loop. Horizontal-field calculations show that the transients peak on the flanks of a 3-D structure, but are depressed over the structure's centre. Weak transient responses flanked by two large transient responses, which are opposite in sign, locate the structure. The sign reversal is caused by a corresponding reversal in the currents that are channelled through or deflected away from conductive or resistive structures, respectively. 相似文献
3.
Previous studies have suggested the presence of large-scale flow structures in gravel-bed rivers. These structures are pictured as intermittent high-speed wedges separated by regions of lower velocity. However, the characteristics of these structures have not been examined in detail through either visualisation techniques or detailed field measurements. This paper confirms the presence of large-scale flow structures in gravel bed rivers, pictures their sequence and patterns and characterises their mean and individual properties. The analysis relies on a new technique for displaying velocity fluctuations in a space–time matrix that allows one to see the structures as they pass an array of current meters. Streamwise and vertical velocities were measured simultaneously with an array of three electromagnetic current meters. The sampling frequency was 20 Hz. Five velocity profiles of up to 13 1-min series of measurements and one profile of three 20-min measurements were sampled. These data suggest the presence of large wedges of faster fluid joined by regions of slower fluid. Space–time correlation analysis confirmed the presence of vertical coherence of the flow. The average angle of the front of the wedges is 36°. Although individual structures are variable in size and shape, a new detection technique using all three velocity signals simultaneously showed that their average frequency is nine events per minute and their duration is more than 2 s. The high-speed wedges display a complex organisation and do not show a preferred sequence of events as was postulated by previous studies. Because of their duration and size, these high-speed wedges are likely to play a major role in bedload sediment transport. 相似文献
4.
江汉平原村落空间分布与微地形结构关系探讨 总被引：4，自引：1，他引：3
主要对江汉平原村落点空间分布规律进行探讨, 分析其与平原微地形结构间的关系。本文采用GIS空间统计方法对研究样区村落点空间分布模式进行分析;并根据平原微地形起伏特点, 采用一种局部形态分析方法进行微地形结构提取;进而对村落点空间分布与微地形提取结果进行空间叠加分析。研究表明:村落空间分布与微地形结构之间表现出明显的空间相关性。约75.40%的村落点与所提取微地形凸起部位的空间位置重合, 而83.94%的村落点在距离微地形凸起50m范围内, 村落点整体表现出向所提取微地形凸起结构聚集的分布格局。江汉平原特有的村落空间结构主要受小尺度地形起伏的影响, 村落格局与微地形结构在空间上的相关性较好地体现了人类活动与洪涝等自然灾害间的相互作用。 相似文献
5.
对头塘山地系统的侵蚀结构的景观生态学分析，表明Ｈ，Ｅ，Ｂ指数对侵蚀结构的描述是可行和适用的，并对五个集水区的侵蚀结构进行了评价。 相似文献
6.
敦煌鸣沙“共鸣箱”成因类型 总被引：1，自引：1，他引：0
关于鸣沙表面结构及发声机制方面的研究已取得一定的成果,鸣沙发声主要与自然沙粒表面的多孔（坑）结构构成的共鸣腔有关,其共鸣机制与亥姆霍兹共鸣腔相似。通过分析敦煌鸣沙所处的自然环境以及扫描电镜下沙粒表面形态结构等,对鸣沙共鸣腔的成因类型展开了全面的探讨。结果表明：敦煌鸣沙所处的独特的自然环境是鸣沙鸣响的天然共鸣箱,主要受地形的影响;鸣沙沙粒表面广泛分布有多孔状的物理结构,且其表面形态多样,这种形态多样的多孔状结构可构成鸣沙鸣响的自身共鸣腔,主要受化学作用、物理机械作用以及二者叠加作用的影响。 相似文献
7.
Hongchao Fan Liqiu Meng 《International journal of geographical information science》2013,27(6):1091-1107
CityGML (City Geography Markup Language), the OGC (Open Open Geospatial Consortium) standard on three-dimensional (3D) city modeling, is widely used in an increasing number of applications, because it models a city with rich geometrical and semantic information. The underlying building model differentiates four consecutive levels of detail (LoDs). Nowadays, most city buildings are reconstructed in LoD3, while few landmarks in LoD4. For visualization or other purposes, buildings in LoD2 or LoD1 need to be derived from LoD3 models. But CityGML does not indicate methods for the automatic derivation of the different LoDs. This article presents an approach for deriving LoD2 buildings from LoD3 models which are essentially the exterior shells of buildings without opening objects. This approach treats different semantic components of a building separately with the aim to preserve the characteristics of ground plan, roof, and wall structures as far as possible. The process is composed of three steps: simplifying wall elements, generalizing roof structures, and then reconstructing the 3D building by intersecting the wall and roof polygons. The first step simplifies ground plan with wall elements projected onto the ground. A new algorithm is developed to handle not only simple structures like parallel and rectangle shapes but also complicated structures such as non-parallel, non-rectangular shapes and long narrow angles. The algorithm for generalizing roof structure is based on the same principles; however, the calculation has to be conducted in 3D space. Moreover, the simplified polygons of roof structure are further merged and typified depending on the spatial relations between two neighboring polygons. In the third step, generalized 3D buildings are reconstructed by increasing walls in height and intersecting with roof structures. The approach has been implemented and tested on a number of 3D buildings. The experiments have verified that the 3D building can be efficiently generalized, while the characteristics of wall and roof structure can be well preserved after the simplification. 相似文献
8.
Graben systems in extensional settings tend to be segmented with evidence of segment interaction. To gain a better understanding of the evolution of structures formed during graben growth and interaction, we here study the Grabens area of Canyonlands National Park, Utah, where a wide range of such structures is well exposed. With the aid of 3D numerical models, we attempt to reproduce structures observed in that region and to understand controls on the structural style of graben interaction by varying the spacing between pre‐existing structures. The sensitivity of the system to the thickness of the salt layer is also tested. Four distinct types of structures are observed when the spacing between inherited weak zones is varied: (1) grabens connecting in a relay zone divided by a narrow central horst; (2) graben segments interacting via a secondary stepover graben; (3) grabens propagating alongside each other with limited segment interaction; and (4) an abandoned graben segment in a system of multiple competing grabens. The presence of a basal salt layer (Paradox Member) promotes efficient graben propagation. A comparison between the observed structures and the numerical model results indicates that the detachment salt layer is relatively thin in the study area. 相似文献
9.
Christian Lucas 《International journal of geographical information science》2013,27(10):1897-1915
To improve the formal integration of verbally given spatial information in a geographical information system, a methodology for converting such information to a geographical representation was developed. This was applied to examples of a spatial-related analysis of natural language text messages in the domain of disaster management. This article presents an approach for such a conversion by using a suitable knowledge representation as well as formal modelling structures. The structures are provided by an ontology-supported knowledge base. With respect to spatial uncertainty, a formal representation based on possibility theory was defined. Moreover, a cluster algorithm was developed for handling information of different sources and building a spatial context. 相似文献
10.
This study presents estimates of the impact adaptation costs due to damage to coastal and marine structures located along the Mediterranean coast of Israel caused by sea-level rise in the 21st century. The study examines the effects on various types of constructions, including seaports, power plants, marinas, desalination plants, sea walls, detached breakwaters, and bathing beach infrastructures for sea-level rises of 0.5 m and 1 m. To this end, we conduct an analysis of hydrodynamic forces on the structures and an uncertainty analysis of their occurrence. The study find that the impact of wave overtopping of breakwaters can lead to extensive damage to port infrastructure and to the vessels moored inside. Adaptation costs are computed as the corrective measures to be taken to maintain the functionality of the structures. 相似文献
11.
B. R. Arora F. E. M. Lilley M. N. Sloane B. P. Singh B. J. Srivastava S. N. Prasad 《Geophysical Journal International》1982,69(2):459-475
Summary Magnetic disturbance events and quiet daily variation as recorded by the 1979 magnetometer array study in north-west India are analysed for evidence of electrical conductivity structures in the region. Contour maps of Fourier transform parameters are presented, and the disturbance event data are also reduced to sets of real and quadrature Parkinson arrows over a range of periods. A variety of conductive structures in the area are mapped, including some relatively shallow ones thought to be caused by sediments, as in the Ganga basin. More information is obtained on a major conductivity structure which strikes perpendicular to the Ganga basin into the foothills of the Himalayas; a second major conductivity structure is detected to lie to the west of the array area, and may be associated there with some aspect of the suture zone of India and Asia. 相似文献
12.
Crustal extension during and following continental collision is well documented in the Arctic Caledonian fold belt. However, models for the post-collisional extension of the Caledonides are mainly based on geoscientific data from Scandinavia. For a more complete understanding of the evolution of the Caledonides, knowledge of the crustal structure of East Greenland is vital. Seismic and gravity studies have revealed a pronounced Moho topography and a west-dipping lower crustal reflector beneath the fjord region of East Greenland. These deep crustal structures are related to Late Caledonian extensional structures at the surface. The observations can be satisfactorily explained by applying simple shear or eduction models proposed for upper crustal extension in Scandinavia to the complementing lower crustal structures in East Greenland. However, exhumation of the Caledonian Northeast Greenland eclogite province cannot be accomplished by these models. Instead, a synthesis of geoscientific data has shown marked differences in the crustal structure of East Greenland north and south of about 76°N, indicating a different crustal evolution of the northern and southern parts of the East Greenland Caledonides. 相似文献
13.
14.
《Geography and Natural Resources》2008,29(4):375-380
The scheme is suggested for studying the modern exogenous relief formation on the basis of the concept of leading processes, and of developing interconnected and mutually complimentary procedures of mapping, analysis of structures and regionalization. The principles and methods of mapping and regionalization of the processes are considered, the basic notions of the structures of modern exogenous relief formation are defined, and the main factors of their formation are shown. 相似文献
15.
David M. Theobald 《International journal of geographical information science》2013,27(8):689-705
Topology is a central, defining feature of geographical information systems (GIS). The advantages of topological data structures are that data storage for polygons is reduced because boundaries between adjacent polygons are not stored twice, explicit adjacency relations are maintained, and data entry and map production is improved by providing a rigorous, automated method to handle artifacts of digitizing. However, what explains the resurgence of non-topological data structures and why do contemporary desktop GIS packages support them? The historical development of geographical data structures is examined to provide a context for identifying the advantages and disadvantages of topological and non-topological data structures. Although explicit storage of adjacent features increases performance of adjacency analyses, it is not required to conduct these operations. Non-topological data structures can represent features that conform to planar graph theory (i.e. non-overlapping, space-filling polygons). A data structure that can represent proximal and directional spatial relations, in addition to topological relationships is described. This extension allows a broader set of functional relationships and connections between geographical features to be explicitly represented. 相似文献
16.
ØRNULF LAURITZEN 《Polar research》1983,1(2):157-160
Some unusual karst structures occur in the upper part of the evaporite-dominated sequence of the Gipshuken Formation. This Lower Permian unit is characterized by interbedded anhydrite and dolomites, and is now interpreted in terms of superimposed sabkha cycles. The karst structures are found in the inner Part of Skansdalen in Dickson Land, and have not yet been observed elsewhere in corresponding horizons in Svalbard. These structures, often seen as linked hemispheroids, consist of almost pure anhydrite and are here interpreted as representing the remnants of consolidated sabkhas; the original sabkha plain was flooded and partly dissolved, and abandoned channels between the hemispheroidal structures were then filled with sediments of later sabkha cycle. The younger sediments which fill the relief between and above the structures contain small enterolithic folds which indicate primary formed anhydrite. Anhydrite is still the most common subsurface mineral in these sulphatic deposits, and there is no evidence of gravitational or tectonic movements within these beds. 相似文献
17.
18.
以大湄公河次区域(GMS)47个城市为研究对象,运用社会网络分析和Multilevel p2模型方法,分析GMS城市群空间经济联系结构、程度及影响因素。结果表明,目前GMS城市群空间经济联系呈"核心-边缘"分布的三级圈层结构,各层级之间经济发展差异较大,空间经济联系程度比较松散。同时,GMS城市群空间经济联系程度还受单个城市经济、资源集聚效应的影响,而城市间要素的扩散效应影响尚不显著。随着各成员国经济发展速度加快,GMS城市群空间经济网络正迅速形成与拓展,中心城市的增加与城市之间相互建立新的经济联系将显著增强该次区域空间经济关联度,未来强化产业支撑、拓展通道建设、完善合作机制是加深GMS城市空间经济联系的发展方向。 相似文献
19.
3D seismic expression of fluid migration and mud remobilization on the Gjallar Ridge, offshore mid-Norway 总被引：3，自引：1，他引：3
This paper presents a three‐dimensional (3D) seismic analysis of sediment remobilization and fluid migration in a 2000‐km2 area above the Gjallar Ridge located in the Vøring Basin, offshore Norway. Three distinct types of mounded structures have been identified as resulting from focused fluid/gas migration and associated mud remobilization and intrusion. Type A structures are gently mounded, and we infer that these structures formed because of in situ remobilization of Middle Eocene to Lower–Middle Oligocene fine‐grained sediments in response to fluid and minor sediment injection via deep‐seated normal faults. Type B structures comprise relatively steep‐sided mounds and are restricted to the pre‐Miocene interval. They are often located above narrow zones of discontinuous low‐amplitude reflections resembling gas chimneys. Some of the Type B structures are associated with stacked amplitude anomalies and possible mud volcanoes at the base Pleistocene indicating their long‐term significance as vertical fluid conduits. Type C structures comprise discrete mound features that seem to jack up the Top Palaeocene (Top Brygge) horizon. These are similar to hydrothermal mounds found elsewhere on the Norwegian Margin and associated with igneous sill intrusion during North Atlantic breakup. This study highlights the utility of 3D seismic data for mapping of fluid and sediment mobilization through time over large basinal areas. 相似文献
20.
中国农村房屋震灾脆弱性评估及其成因分析 总被引：4，自引：1，他引：3
中国农村地区的房屋普遍处于地震未设防的状态,在地震中房屋结构破坏是造成人员伤亡和财产损失的主要因素。作为重要的灾害承险体之一,从房屋结构方面进行区域震灾损失的预测对把握各个地区的灾害脆弱性,科学地制定区域防灾战略和规划具有极其重要的意义。①基于中国县级尺度房屋结构数据库的前期基础工作,以2000 年中国地震区划为基本依据,参考震灾条件下的不同结构房屋破坏比和易损性曲线的研究成果,对中国县级空间尺度的农村房屋震灾脆弱性进行了整体评估。② 根据房屋破坏损失的预测结果,将中国农村地区划分为低脆弱性、一般脆弱性、较高脆弱性和极高脆弱性地区4 类,并对较高、极高脆弱性地区的空间分布规律进行了分析。结果表明,中国约18.6%的县处于脆弱性较高和极高的地区,主要集聚在南疆,北疆的乌苏、精河、伊宁等地区,陕西、甘肃、宁夏地区,山东中南部、安徽、江苏等地区,西藏南部边境地区,云南以及青藏高原板块边缘纵贯青川滇的都兰—玛多—道孚—泸定—冕宁—昆明—建水沿线地区。③ 根据各个地区震灾脆弱性的成因和类型,以及较高、很高脆弱性地区的区域发展水平特征,提出了区域防灾策略的建议。 相似文献