青藏高原东部的Pn波层析成像研究

利用INDEPTH/ASCENT台阵和其它布设在青藏高原的流动宽频带地震仪数据,反演了青藏高原东部和周边区域的上地幔顶层Pn波速度以及台站延迟.研究区域的平均Pn波速度是8.1 km/s,略高于中国大陆的平均Pn波速度.低速区主要分布在羌塘地块的西部和松潘-甘孜地块,高温异常的岩石圈上地幔很可能是导致这一低速区的原因.班公-怒江缝合带东端区域的Pn波速度达到8.35 km/s,这一高速区可能与向北俯冲的印度板块(东端)有关.另一Pn波高速区分布在祁连山和昆仑山之间,主要由柴达木盆地和共和盆地及其周边地区,两个并不完全连续的高速异常区组成,它可能对应于特提斯洋闭合时北部增生的克拉通地体;在后来的欧亚板块与印度板块的碰撞中,这一地体有可能阻挡了青藏高原向北的生长.相对密集的台站提供了高分辨率的速度结构横向分布和地壳厚度变化.台站延迟显示青藏高原北部和东部的地壳存在显著的减薄--松潘-甘孜地块东北缘的地壳厚度仅为约50 km,而羌塘地块东部唐古拉山地壳最厚,达到75 km,这可能是由于印度-欧亚板块碰撞引起的羌塘地块内部变形增厚所致.     

The lithosphere and asthenosphere system in Italy as inferred from the Vp and Vs 3D velocity model and Moho map

We present an updated high-resolution tomographic P- and S-wave velocity model of the lithosphere and asthenosphere system in Italy, obtained by adding the observations from ∼25,000 earthquakes (recorded between 2003 and April 2012 at three-component stations) to the previously inverted dataset (165,000 P-wave phases from ∼8000 events recorded between 1988 and 2002 at single-component). The final dataset includes ∼586,000 P- and ∼290,000 S-wave arrival times. The main strength of this research is the use of a method able to model P- and S-seismic phases refracted at the Moho discontinuity. We use a new and original map of the 3D Moho geometry obtained by integrating selected high quality controlled source seismology (CSS) and teleseismic receiver function data. Resolution strongly benefits also from the fast increase in number and quality of INGV National Seismic Network since year 2003 and from its integration with several permanent regional seismic networks. This study confirms the main structural features in the best-resolved parts of the inverted volume and much better images details in the less resolved areas of previous Vp models, due to both the larger number of inverted phases and the more even distribution of seismic stations. A new 3D Vp/Vs model is presented and discussed. Shallow structures and the relationships between the Adriatic, Tyrrhenian, and Adria plates are better imaged.     

硬膜下血肿的CT表现与预后

硬膜下血肿是常见的脑部外伤性病变之一。本文对我院１９８９年３月至１９９３年６月间收治的２５８例硬膜下血肿患者作了系统分析，对硬膜下血肿的ＣＴ表现与预后关系作一初步探讨。     

数字拓扑学和层析成像

本文论述拓扑学在数字图像中的应用，首先定义数字图像子集的性概念，并论述当前正孕育着一门分支－数字拓扑学及其在层析成像的可能具有的联系。     

A rapid method for converting medical Computed Tomography scanner topogram attenuation scale to Hounsfield Unit scale and to obtain relative density values

Medical Computed Tomography scanners permit to rapidly obtain qualitative and quantitative information on objects in a non-destructive manner in both longitudinal and transversal directions. CT-scan scales used to express attenuation on the images are different for longitudinal (topograms) and transversal (tomograms) views, restraining the complementary use of the information extracted from both views. Moreover, topograms are of full use in core analysis as they reveal fine-scale information on stratigraphical, sedimentological and physical properties of the material. This paper presents a method to convert CT-scan topogram intensity scale to Hounsfield Unit (HU; scale used on tomograms) and to later extract a relative density from it. The method is based on relationships between topogram and tomogram values, absolute density and effective atomic numbers obtained on a series of minerals. Results show excellent correlations between converted topogram values and HU values obtained on the tomograms, as well as between relative densities derived from the converted topogram values, and the absolute density of the minerals.     

肾脏CT扫描前准备工作的改进方法

本文回顾分析１９８７年３月￣１９９２年５月行肾脏ＣＴ扫描１０２例，其中诊断肾结石３１，当时因ＣＴ扫描前准备方法问题，及开始经验不足造成４例无结石的病人误诊为结石。找到误诊石的原因是ＣＴ扫描前静脉试验及口服泛影葡胺造影剂造成，采取改进ＣＴ扫描前准备方法；（１）扫描前不行静脉试验（２）口服造影剂改为口服温水或牛奶，经上述改进方法，以后未出现造影剂造成肾结石误诊。     

面部和颅底骨折的CT分析

为了提高对面部和颅底骨折的认为。本组７４例，男性６３例，女性１１例，年龄２－７１岁，车祸外伤６４例，拳击伤５例，铁棍击伤２例，从高处跌下３例，全部病例均采用轴位ＣＴ平扫。眶内壁骨折２０例，其中爆裂骨的１１例，直接骨折８例，１列同时受直接和间接外力作用；眶下壁骨折１例，为爆裂骨折；眶外后壁骨折１例，眶顶壁骨折９例，均为直接骨折；其他骨折３３例；蝶窦内液平为颅底骨折的重要间接征象。ＣＴ检查可确定骨折类     

地形表面反射强度的数学层析成像方法

若二维ＲＦ窄波反射函数是定义在地面一圆形区域内部的，并假定该圆域表面介质是弱反射介质，那么在给定时刻，接收发射器（如机载合成孔径雷达）所接收到的近回数据可视 过该圆域的一圆弧上的线积分值，Ｍｕｍｓｏｎ，ｅｔ，ａｌ。在假定圆域半径与接收发射器运动路径到该圆域中心的距离相比很小的情况，用直线上的线积分值来代替圆弧线上的线积分值，利用古典的Ｒａｄｏｎ变换方法，给出了该圆域反射函数的成像模式。本文将克服这     

Wavefield tomography based on local image correlations

The estimation of a velocity model from seismic data is a crucial step for obtaining a high‐quality image of the subsurface. Velocity estimation is usually formulated as an optimization problem where an objective function measures the mismatch between synthetic and recorded wavefields and its gradient is used to update the model. The objective function can be defined in the data‐space (as in full‐waveform inversion) or in the image space (as in migration velocity analysis). In general, the latter leads to smooth objective functions, which are monomodal in a wider basin about the global minimum compared to the objective functions defined in the data‐space. Nonetheless, migration velocity analysis requires construction of common‐image gathers at fixed spatial locations and subsampling of the image in order to assess the consistency between the trial velocity model and the observed data. We present an objective function that extracts the velocity error information directly in the image domain without analysing the information in common‐image gathers. In order to include the full complexity of the wavefield in the velocity estimation algorithm, we consider a two‐way (as opposed to one‐way) wave operator, we do not linearize the imaging operator with respect to the model parameters (as in linearized wave‐equation migration velocity analysis) and compute the gradient of the objective function using the adjoint‐state method. We illustrate our methodology with a few synthetic examples and test it on a real 2D marine streamer data set.