共查询到19条相似文献，搜索用时 142 毫秒
1.
色素痣三维结构的实现与研究 总被引：2，自引：0，他引：2
对临床已确诊的2例皮内痣进行连续切片，痣细胞和基底膜的表达分别采用S－100多克隆抗体和IV型胶原单克隆抗体LAB－SA免疫组化染色法。采用显微图像自动拼接技术显示皮内痣组织的全貌结构。结合三维可视化及测量系统软件，以体素重建法，结合插值拟合与光照处理技术，对手术切除的皮内痣进行三维重建，旨在真实反映基底膜和痣细胞的立体形态、空间位置和相互毗邻关系。对临床色素痣的教学和治疗提出新的方法和思路。 相似文献
2.
本文介绍了自行开发的解决Diseetor应用问题的计算机图像处理软件系统及关键技术、算法。本系统能依照Disector原理对多层组织细胞的电镜及光镜图像中的目标进行正确的分割,各层之间图像的人工交互及自动配准。针对每个目标的上下层关系实现目标的Disector自动计数及参数计算,并对每个目标进行体数据的提取和三维重建显示,通过切片级表面重建出曲面表面,再借助OpenGL的显示功能把曲面显示出来。使用Disector分析系统对多种粒子(细胞等)进行三维分析,可以简化寻找新出现粒子的过程,克服切片采集过程中的形变,在统计分析之后,立体地观察粒子结构,能够使操作者从繁琐的手工操作中解脱出来。自动统计新出现的粒子。文中同时还给出了用该系统对小白鼠神经细胞个数的Disector分析,肾小球个数统计分析和三维重建显示实例。 相似文献
3.
铸件的工业CT三维检测技术 总被引：2，自引：0，他引：2
通过对工业CT扫描得到的连续二维图片进行三维重建，得到试件的三维重建图像，从而可用于复杂构件的三维结构分析、缺陷硷测，并可与快速成型系统相结合，实现对复杂零件的快速复制，在产品开发及制造过程中起到了重要作用。 相似文献
4.
本文评述美国五家公司的显微CT（以下简称MCT）的现状和发展趋势,在颅凳面病人实际行皮肤切片,显示薄层细胞的基础上,结合MCT做二维和三维的CT成像,成立体,详尽和精确地显示皮肤表层5－10毫米,机体组织三维解剖结构,包括表皮,真皮、脂肪、动脉、静脉的空间分布及其相互关系,探讨显微CT和螺旋CT机在其成像分辨率提高的进程,再现美容病体模型的程度可达到亚微米级的精度,为掌握病情并制定合理的手术计划提供了重要依据,提高－整形的效果,实现全方位扫描和精密三维重建技术在颅凳面皮肤美容和减肥的适应症的应用价值。结果：显微CT三维重建技术是现代皮肤美容和保健的主要诊断方法之一,并具有重要的临床应用价值;近年来工业微焦点CT机其空间分辨率已达5－15微米,已发展了用于生物医学的研究,今后对可皮下组织作精细的CT成像,以了解形整美容,减肥,对当前的美容和保健产品给予在亚微米级,从细胞发育情况的定量评价,表述其CT影像的微观结果。 相似文献
5.
电子束CT三维重建方法 总被引：9，自引：0，他引：9
医学断层图像的三维重建技术提供了一种无创方法直观考察人体内的立体结构２,当用于电子束ＣＴ,更能充分显示它的价值。本文阐述了用电子束ＣＴ采集体层数据（包括步进容积扫描,连续容积扫描,电影扫描）后,用多层面重组,最大密度投影,表面阴影显示等方法进行三维重建的处理过程。 相似文献
6.
杏仁核的计算机三维重建及其临床意义 总被引：3，自引：0，他引：3
目的：用计算机重建杏仁核的空间形态与位置,为脑的立体定向手术提供解剖学基础。方法：对20只整脑40个杏仁核2mm厚的连续水平切面,运用表面重建法对杏仁核进行计算机三维重建。结果：重建后的杏仁核立体图像顺滑、自然、逼真,可任意缩放、旋转、切割。结论：计算机重建后的杏仁核空间形态与位置对脑立体定向手术有参考价值。 相似文献
7.
多层螺旋CT后处理技术对气管支气管异物的诊断价值 总被引：1，自引：0，他引：1
目的:评价多层螺旋CT三维重建及仿真内窥镜技术对气管支气管异物的诊断价值。方法:对20例支气管异物、1例气管异物、1例先天性气管性支气管发育异常、1例气管良性肿瘤患儿行多层螺旋CT检查并进行三维重建及仿真内窥镜技术显示气管支气管病变;三维重建技术包括多平面重建、最大密度投影、最小密度投影、表面遮盖显示和容积再现,CT仿真内窥镜对气管支气管异物的显示与支气管镜所见具有一致性。结果:多层螺旋CT三维重建及仿真内窥镜可准确、直观地显示气管支气管异物的位置、大小、形态、密度及阻塞程度。结论:多层螺旋CT三维重建及仿真内窥镜可准确评价气管支气管异物,是一种准确无创性诊断方法,为临床治疗提供直观的影像学资料,具有较高的临床诊断及指导价值。 相似文献
8.
美国利用IMAGE卫星的极紫外辐射（EUV）探测器对地球等离子体层进行了连续5年的遥感成像观测。由于IMAGE卫星数据是沿观测路径上的积分投影数据,并且存在地球“遮挡”、“阴影”、“数据缺失”等问题,无法直接利用传统的CT方法对等离子体层进行三维重建。本文利用地球磁场模型,基于地球等离子体层的物理性质,建立一个联系地球磁赤道面密度与投影数据的EUV成像模型,实现了从单个角度的EUV观测图像进行地球等离子层三维重构的方法。 相似文献
9.
螺旋CT三维重建对髋臼骨折的临床应用价值 总被引：1，自引：1，他引：0
目的:评价多层螺旋CT三维重建在髋臼骨折中的临床应用价值.方法:对38例髋臼骨折患者的X线平片、CT三维重建资料进行回顾性分析.结果:X线平片确诊34例,疑诊3例,漏诊1例,对其中24例正确分型.CT三维重建对38例髋臼骨折的患者均明确诊断,且均能正确分型.结论:多层螺旋CT三维重建能立体、多方位、准确地显示髋臼骨折的部位、范围、碎骨片等情况,对髋臼骨折的诊断、分型及手术方案制定优于X线平片,有较人的临床应用价值. 相似文献
10.
断层等不连续性结构的检测在地震勘探中具有重要的意义.本文简单介绍了高维连续小波变换的基本理论,包括:高维连续小波变换的定义、高维小波变换系数的切片以及快速实现方法等,利用典型的合成信号说明了高维连续小波变换具有更好的方向选择性(相比于常用的高维张量积小波变换),将高维连续小波变换引入地震资料不连续性检测,并提出了利用小尺度高维连续小波变换系数检测地震资料不连续性的方法,同时给出了方法的实现流程.合成信号以及实际三维地震数据处理效果验证了本文所提方法的有效性. 相似文献
11.
12.
随着页岩气勘探与开发的深入,研究页岩裂隙的三维空间展布成为页岩岩石物理研究的必要步骤之一.但由于仪器的限制,页岩切片在深度上具有不连续性,以及数字岩心纵向上成像最小间隔与横向分辨率的不一致成为影响裂隙表征和数字岩石物理模拟精度提高的重要因素.为了更好的研究裂隙在三维的空间展布,本文将curvelet稀疏变换与凸集投影(POCS)迭代算法有效结合,实现三维数字岩心重建.首先对X射线扫描砂岩得到的三维数据体进行隔片抽稀,利用本文方法实现三维数据体重建,重建结果与完整数据体具有很好的一致性,且优于现有方法(spgl1),验证了新方法的有效性与先进性.其次对聚焦离子束扫描电镜(FIB-SEM)得到的纳米级页岩二维切片在深度上进行了加密重建,获得纵向上成像最小间隔与横向分辨率基本一致的三维数字岩心,由于仪器限制引起的页岩切片深度上的不连续性得到减弱,裂隙展布更加清晰.砂岩CT图像以及页岩FIB-SEM成像数据的重建结果验证了本文方法的有效性与先进性. 相似文献
13.
S. Buske 《Pure and Applied Geophysics》1999,156(1-2):157-171
— This paper presents an overview of the results obtained from a 3-D prestack depth migration of the ISO89-3D data set. The algorithm is implemented as a Kirchhoff-type migration, in which the migrated image is generated by weighted summation along diffraction surfaces through the shot record section. The diffraction surfaces are computed by a 3-D finite difference solution of the eikonal equation. A 3-D macro-velocity model derived mainly from wide-angle tomographic inversion served as input for the travel-time calculations. The results of the migration are presented as slices through a volume covering an area of 21 km × 21 km in the horizontal and 15 km in the vertical direction, centered around the KTB drill hole. In these slices the continuation of the Franconian Lineament or SE1 reflector, respectively, can be identified over most of the survey area as a northeast dipping reflector plane. Its signature appears partly curved and discontinuous and with different strength of reflection down to a maximum depth of 9 km. About 5 km to the south-southeast of the KTB drill hole the uppermost top reflection of the Erbendorf body (EB) can be recognized at approximately the same depth. The slices clearly show its complicated internal structure consisting of several apparently separated reflective parts. Moreover, the geometry and the shape of a few other subsurface structures are described. 相似文献
14.
Hydrostratigraphic modeling of a complex,glacial-drift aquifer system for importation into MODFLOW 总被引：4，自引：0，他引：4
Deposition from at least three episodes of glaciation left a complex glacial-drift aquifer system in central Illinois. The deepest and largest of these aquifers, the Sankoty-Mahomet Aquifer, occupies the lower part of a buried bedrock valley and supplies water to communities throughout central Illinois. Thin, discontinuous aquifers are present within glacial drift overlying the Sankoty-Mahomet Aquifer. This study was commissioned by local governments to identify possible areas where a regional water supply could be obtained from the aquifer with minimal adverse impacts on existing users. Geologic information from more than 2,200 existing water well logs was supplemented with new data from 28 test borings, water level measurements in 430 wells, and 35 km of surface geophysical profiles. A three-dimensional (3-D) hydrostratigraphic model was developed using a contouring software package, a geographic information system (GIS), and the 3-D geologic modeling package, EarthVision. The hydrostratigraphy of the glacial-drift sequence was depicted as seven uneven and discontinuous layers, which could be viewed from an infinite number of horizontal and vertical slices and as solid models of any layer. Several iterations were required before the 3-D model presented a reasonable depiction of the aquifer system. Layers from the resultant hydrostratigraphic model were imported into MODFLOW, where they were modified into continuous layers. This approach of developing a 3-D hydrostratigraphic model can be applied to other areas where complex aquifer systems are to be modeled and is also useful in helping lay audiences visualize aquifer systems. 相似文献
15.
CT断面图象序列中多个目标三维重建和显示(英文) 总被引：3，自引：0，他引：3
本文在断面图象序列中,单个目标的三维重建的基础上,提出一种同时快速重建和显示断层斟象序列中多个目标的方法,并在微机图象处理系统上实现三维重建和显示,效果较为理想,这是当前世界上的前沿问题。 相似文献
16.
Tomá? Fischer Petra ?těpan?íková Magda Karousová Petr Tábo?ík Christina Flechsig Mahmoud Gaballah 《Studia Geophysica et Geodaetica》2012,56(4):1019-1036
Geodynamic activity in the area of West Bohemia is typified by the occurrence of earthquake swarms, Quaternary volcanism and high flux of mantle-derived CO2. The highest swarm activity occurs beneath the eastern edge of the Cheb basin, which is delineated by the NW-SE trending morphologically pronounced Mariánské Lázn?? Fault (MLF) controlling the formation of the basin. The previous trenching survey across the MLF zone has identified several fault strands with possible Quaternary activity. In this paper we present the results of the geophysical survey focused to trace the faults signatures in geophysical sections and to build an image of near surface tectonics. The method of electric resistivity tomography (ERT) along two profiles parallel to the trench identified a strong resistivity contrast between the bodies of sandy gravels in the middle and conductive clayey sands to the west and weathered crystalline basement to the east. The 2-D ground penetration radar (GPR) sections show direct correlation of reflections with lithological boundaries identified in the trench. As expected, the GPR signal amplitudes increase with the resistivities found in the ERT sections. Two of the four faults identified in the trench are indicated in the resistivity and GPR sections. A 3-D GPR measurement has identified a spot of high amplitudes elongated parallel to the MLF trend, which coincides with the high resistivity body. To improve the signal-to-noise ratio of the time slices we stacked the GPR time slices within vertically homogeneous blocks. This provided a contrast image of the sand-gravel body including its boundaries in three dimensions. The detailed analysis of the 3-D GPR cube revealed additional fault that limits the highly reflective sands and appears to be offset by another younger fault. Our results suggest a complex fault pattern in the studied area, which deserves a further study. 相似文献
17.
2008年5月12日汶川发生里氏8.0级地震的发震机制与龙门山断裂带的构造特征紧密相关,应用反射地震探测方法精细探测发震构造内部的结构特征,对研究汶川地震的发震机理有重要意义.5.12地震后在地表错断最剧烈的区域之一虹口乡白庙村穿过发震构造和深钻科研井WSFD-1和WSFD-2布置了兼顾浅中深层信息的反射地震探测剖面,该区域断裂带硬岩出露,地形地貌复杂多变,起伏剧烈,只能采取弯线地震测线布设方式采集二维反射地震数据,而且弯曲度大,造成CDP点分散严重.区域内构造复杂,褶皱逆推构造发育,地层和构造倾角大,采用常规二维地震数据处理方法进行叠加处理时,易将不同地层的反射信息叠加到同一反射层.弯线叠加剖面上侧面波,混波干扰严重,会显著地降低原本低信噪比数据的分辨率,或剖面可靠性低,容易在二维剖面中造成解释陷阱.本文利用弯线地震采集的三维特性,用拟三维地震叠加技术处理汶川地震科学钻井附近横跨北川-映秀断裂带的二维弯线地震数据,弥补常规二维弯线地震数据处理技术的不足,将不同地层的反射信息分离归位到不同的三维叠加剖面上,解决二维弯线地震数据处理时混波干扰严重的难题.通过理论分析和实验选取合适的共中心点面元,获得了高分辨率的三维叠加剖面.相比于二维弯线叠加剖面,三维叠加剖面切片成像更真实,剔除了不同地层反射信息混叠的影响,能得到更准确的断点信息,并可以获得沿断层走向横向的信息,显著提高了构造解释的可靠性和精度.应用拟三维地震数据处理方法处理龙门山断裂带的二维弯线地震数据,获取高分辨率的构造信息,有利于断裂带内汶川地震发震机制和龙门山隆起机制的解释. 相似文献
18.
采用代数重建技术重建三维物体,提出了一种基于splatting原理的ART权值计算方法,以增强重建图像的空间分辨率.该算法基于三维锥束扫描方式,采用双三次样条局部基函数作为插值核,并利用其足印函数对物体进行插值来计算像素的权值.与常量插值相比,这种方法对物体的灰度值有更精确的近似,在相同的实验条件下可重建出分辨率高的物体.给出了适用于三维锥束重建的splatting算法的具体实现,并对实验数据进行了实物重建及误差分析. 相似文献
19.
This paper studies the computation method of two-step inversion of interface and velocity in a region. The 3-D interface is
described by a segmented incomplete polynomial; while the reconstruction of 3-D velocity is accomplished by the principle
of least squares in functional space. The computation is carried out in two steps. The first step is to inverse the shape
of 3-D interface; while the second step is to do 3-D velocity inversion by distributing the remaining residual errors of travel
time in accordance with their weights. The data of seismic sounding in the Tangshan-Luanxian seismic region are processed,
from which the 3-D structural form in depth of the Tangshan seismic region and the 3-D velocity distribution in the crust
below the Tangshan-Luanxian seismic region are obtained. The result shows that the deep 3-D structure in the Tangshan seismic
region trends NE on the whole and the structure sandwiched between the NE-trending Fengtai-Yejituo fault and the NE-trending
Tangshan fault is an uplifted zone of the Moho. In the 3-D velocity structure of middle-lower crust below that region, there
is an obvious belt of low-velocity anomaly to exist along the NE-trending Tangshan fault, the position of which tallies with
that of the Tangshan seismicity belt. The larger block of low-velocity anomaly near Shaheyi corresponds to a denser earthquake
distribution. In that region, there is an NW-trending belt of high-velocity anomaly, probably a buried fault zone. The lower
crust below the epicentral region of the Tangshan M
S=7.8 earthquake is a place where the NE-trending belt of low-velocity anomaly meets the NW-trending belt of high-velocity
anomaly. The two sets of structures had played an important role in controlling the preparation and occurrence of the M
S=7.8 Tangshan earthquake.
Contribution RCEG97006, Research Center of Exploration Geophysics, China Seismological Bureau, China.
This project is supported by the Chinese Joint Seismological Science Foundation. 相似文献