TM30免棱镜模式下的精度分析及其应用     

隗骏 《测绘与空间地理信息》2016,(6):201-203

随着科学技术的迅猛发展,许多先进的测量仪器被广泛地应用于测绘行业中,为测绘工作提供了更多的方法和技术手段。本文根据我校实验研究分析的需要,采用了新型的测量方法,利用经纬仪工业测量系统的高精度特性,对徕卡TM30在免棱镜模式下测量技术与精度进行了一系列探讨分析。经验证,免棱镜模式下徕卡TM30在室外检校场的研究实验可满足所需精度要求,且比传统测量手段更加合理,大大提高了工作效率。  相似文献   

Complete 40Ar resetting in an ultracataclasite by reactivation of a fossil seismogenic fault along the subducting plate interface in the Mugi Mélange of the Shimanto accretionary complex,southwest Japan     

《Journal of Structural Geology》2016

We used the K–Ar ages of clay-sized mineral grains to investigate the timing of activity on the Minami-Awa Fault, which is a fossil seismogenic fault along a subducting plate interface separating the coherent strata of the Shimanto accretionary complex to the north from the tectonic mélange to the south. The K–Ar ages from the matrix shale of the mélange range from 85 to 48 Ma and decrease with decreasing amount of detrital mica, indicating that they record a mixture of authigenic illite related to burial diagenesis and detrital mica. In contrast, the K–Ar ages of an ultracataclasite within the fault core are significantly younger, ranging from 29 to 23 Ma, and are unrelated to grain size and amount of detrital mica. This indicates that s Ar diffused completely from the ultracataclasite between 29 and 23 Ma, which postdates the formation of authigenic illite by at least several million years. The diffusion of ⁴⁰Ar in the ultracataclasite was probably caused by frictional heating or high-temperature fluid migration that occurred when the fault was reactivated. The results indicate that seismogenic faults that separate tectonic mélange from coherent strata in accretionary complexes may slip, not only during accretion, but also long after accretion.  相似文献   

关于雅鲁藏布江缝合带(东段)的新认识   总被引：8，自引：2，他引：6       下载免费PDF全文

郝杰  柴育成 《地质科学》1995,30(4):423-431

国内外不少地质学家大都将雅鲁藏布江蛇绿岩带视为印度板块与亚洲板块之间的缝合带。但是,笔者等在喜玛拉雅造山带的东段即仁布-康马一线以东地区的研究却发现,在雅鲁藏布江蛇绿岩带的南侧发育着一个宽大的增生杂岩体,它与雅江蛇绿岩是同一大洋即特提斯喜玛拉雅洋俯冲消减的产物,前者代表着特提斯喜玛拉雅洋消亡遗迹的主体,是印度板块与拉萨地块之间缝合带的主要组成部分;而后者代表的是俯冲带与拉萨地块之间的残余洋壳,它由北向南仰冲,构成日喀则-桑日弧前盆地前缘脊和南部基底,因而其不代表主缝合带。北喜玛拉雅增生杂岩体的发现改变了以Gansser(1964)为代表提出的喜玛拉雅造山带的构造模式,为重新审视印度板块与拉萨地块缝合作用过程提供了一个重要的地质制约和新的研究途径。  相似文献   

Numerical Investigations in the Analytical and Semi-Analytical Computation of Gravimetric Terrain Effects     

Tsoulis  D. 《Studia Geophysica et Geodaetica》2003,47(3):481-494

A recently proposed method for the computation of the gravitational effect due to the topographic masses defined by a Digital Elevation Model (DEM) involves the representation of the surface relief by means of parts of bilinear surfaces. The so-called bilinear method delivers eventually the mathematical model for the gravitational attraction of a right rectangular prism, whose top is modeled by a bilinear surface. Scope of the paper is to assess the new method by conducting numerical tests using both real and synthetic data. The performance of the bilinear method is evaluated in terms of its computational efficiency as well as its precision by comparing it with other analytical methods available for the practical evaluation of gravitational terrain effects. The techniques considered for the assessment of the bilinear approximation are the vastly applied right rectangular prism method and the polyhedral modeling, a less popular but extremely flexible approach based on the closed expression for the gravity field of an arbitrarily shaped mass distribution defined by planar faces. The different geometric modeling of the topographic relief produces discrepancies to the gravitational attraction of up to several mGal. Thus the choice for the geometric representation of the terrain plays a fundamental role to the numerical computation of potential field quantities especially in the critical region surrounding the computation point.  相似文献   

应用有限单元法恢复冲绳海槽和付加体古构造应力场及其意义     

卢汉堤  黄俭惠 《矿产与地质》2004,18(5):460-465

冲绳海槽是欧亚板块内大陆地壳的扩张作用所形成的一个弧后盆地。以弹性学原理和库仑—莫尔准则为基础,应用二维(2D)有限单元法模拟大陆岩石圈上部的构造应力场和断层发育状况。模型中使用两种位移边界条件,并采用平面应变条件进行计算。扩张位移边界条件加载于冲绳海槽内大陆地壳的底部,俯冲位移边界条件加载于菲律宾海板块的俯冲带。数学模拟的结果表明,大陆地壳底部的扩张作用使得冲绳海槽内发育正断层,最后导致冲绳海槽这一弧后盆地的形成。菲律宾海板块的俯冲作用引起欧亚板块付加体中形成逆掩断层。  相似文献   

GIS地表塌陷计算的有限棱柱法及三维数据模型   总被引：2，自引：0，他引：2  

刘汉龙  刘立民  连传杰 《岩土力学》2004,25(6):913-916

具有强大信息管理和可视化功能的GIS已在地下硐室开挖、矿山采掘、边坡等许多工程领域中得到了广泛应用。笔者给出了一种用于地下开挖变形描述和应力分析的方法——有限棱柱法，并就该方法与GIS集成中的数据模型和数据组织方法进行了探讨，建立了基于GIS的虚拟地质体地下开挖变形描述与评价计算的三维可视化系统，并对多语言集成模式和数据可视化方法进行了探讨。同时还给出了该方法的工程应用实例，对该方法的可靠性和有效性进行了验证。  相似文献   

基于改进三棱柱模型的复杂地质体3D建模方法   总被引：8，自引：0，他引：8  

王占刚  曹代勇 《中国煤田地质》2004,16(1):4-6,64

建模方法是三维地质模型及其可视化研究的核心内容。针对连续体终止、错断位移等复杂地质体3D地质建摸的需要，本文对现有的三棱柱数据模型进行了改进，构建了完整的数据结构及其初步的拓扑关系，提出了基于改进三棱柱模型的连续体和不连续体的建摸算法，使其在处理地层尖灭、断层等复杂地质问题时更为灵活、适应面更广。  相似文献   

Morphodynamics of the barrier-inlet system, west-central Florida     

Richard A. Davis  Jr.  Patrick Barnard 《Marine Geology》2003,200(1-4):77-101

The barrier-inlet system along the Gulf Coast of peninsular Florida has one of the most diverse morphologies of any barrier system in the world. The delicate balance between tidal- and wave-generated processes on this low-energy coast permits only slight changes in either of these processes to result in significant and rapidly developing morphologic responses. Some of these responses are the result of natural phenomena such as hurricanes opening tidal inlets, closure of inlets due to longshore transport of sediment, and changes in the availability of sediment. Tidal prism is the primary factor in controlling inlet morphology and is greatly influenced by anthropogenic activities in the backbarrier area. Human activity has also modified the coast in many ways over the past several decades, beginning with the construction of the first causeways in the 1920s. The various modifications by development have resulted in important morphodynamic changes in the barrier-inlet system. These include hardening the coast on the beach and at inlets, dredging and filling in backbarrier environments, and construction of fill-type causeways connecting the islands to the mainland. Construction of seawalls and jetties has inhibited normal coastal processes. Examples include the downdrift erosion at Blind Pass and Big Sarasota Pass. Construction of fill-type causeways between the barriers and the mainland has created artificial tidal divides that reduce the tidal prism at some inlets, thereby resulting in instability or closure such as Blind Pass and Dunedin Pass. This is further exacerbated by dredge and fill construction that reduces tidal prism by reducing the area of open water in the backbarrier. Dredging of the Intracoastal Waterway also results in a negative impact on selected inlets by channeling tidal flux away from some inlets. Impacts of these changes inhibit the barrier/inlet environments from responding to open coast processes.  相似文献   

Unwrapping reworked crust at the Columbia supercontinent margin within central southern Amazon Craton using multi-source geophysics and geochronology data synergy     

《地学前缘(英文版)》2022,13(3):101348

The geometry and evolution of pre-existing basement in accretionary belts bordering supercontinents are often unclear. Integrative interpretation of long-wavelength potential field satellite data can image deep crust structure, improving our understanding of lithospheric processes that formed these margins bottom-up. Here, we present a multidisciplinary interpretation of the lithospheric architecture of the central southern Amazon Craton, a fragment of an accretionary belt at the southwestern Columbia supercontinent margin. Satellite-borne gravity and magnetic data, airborne magnetic data, passive seismic (V_p/V_s ratio, crustal thickness) and seismic tomography data reveals that basement terranes from the interior of the craton extend into the accretionary margin of Columbia. We demonstrate a vertically heterogeneous structure with an underlying strongly reworked pre-Columbia tectonic wedge that sustained prolonged modification during the supercontinent assembly as corroborated by Nd isotope and geochronology data. Nd isotope data suggest that the protracted orogenic wedge was influenced by subduction angle shifts over time, including addition of substantial juvenile material during slab retreat events. This interplay promoted Craton growth at the supercontinent margin while keeping a subtle record of the pre-existing framework. Our findings point to the possible misrepresentation of basement extension and geometry of supercontinent margins elsewhere.  相似文献   

全站仪免棱镜测绘线路横断面     

李雪刚  赵建三 《测绘工程》2007,16(1):70-72

测绘横断面是线路勘测的重要工作之一,若能准确、快速测绘横断面会取得显著的经济效益。介绍了全站仪免棱镜测量的基本原理,并对其测量精度作了分析,论述其在较差的测量条件下,简捷、高效、准确测绘横断面的具体应用和注意事项,具有实际指导意义。  相似文献