福建省古生代至中生代大地构造演化的格架   总被引：10，自引：0，他引：10  

边效曾  褚志贤 《福建地质》1993,12(4):280-291

松溪—长汀断裂带和福州—永定断裂带是控制福建古生代及以后大地构造演化的两条北东东向的断裂带。地质地球化学资料表明,前者是加里东期的地体碰撞带,沿线分布了构造混杂岩、变质超基性岩体、具有角闪岩相和中压矿物的变质岩以及同碰撞型花岗岩体,以后又发育为A型俯冲带;后者是发育于加里东构造层之上的海西期张裂带,在形成海西期的福州—永定海峡的同时,产生了石炭纪海底双模式火山岩及层控铁矿,印支期的碰撞活动使海峡封闭并发育A型俯冲作用。由此,北东东向的松溪—长汀断裂带和福州—永定断裂带可以将福建划分为三个古生代的构造地层地体:闽北地体、闽中地体和闽东南地体。通过对福建省古生代地体构造分析、古地磁测量及古地理重建,展现在我们眼前是:华南(其中包括福建)在古生代中期从冈瓦纳大陆分离出来后,横渡特提斯海,在古生代末至中生代初到达劳亚大陆,与中朝板块碰撞引起了福建地体间强烈的造山运动。  相似文献   

浙江晚中生代雁荡山地貌成因及其与火山构造协同性演化规律     

段政  张翔  卢琴飞  陈荣  余明刚  洪文涛  褚平利 《地质学报》2022,96(6):2021-2038

浙江雁荡山是东南沿海一座典型的晚中生代破火山，以发育丰富的白垩纪流纹质火山岩地貌为特色，主要包括火山岩相剖面和火山岩地貌两种类型地质遗迹。本次通过详细的野外地质调查、岩石学研究及遥感图像分析，进一步将其中火山岩相剖面划分为溢流相、基底涌流相、火山碎屑流相、空落相剖面地质遗迹四小类；火山岩地貌分为叠嶂、锐峰和岩洞地貌地质遗迹三小类，并综合分析了其分布规律与成因演化过程。研究表明这些地质遗迹的分布和演化明显受到火山构造与火山岩相的控制。另外，研究区显著发育3级夷平面，反映其至少经历过3期隆升- 剥蚀事件，是太平洋板块、菲律宾海板块与欧亚大陆板块相互作用的动力学过程及印度板块碰撞远程效应的综合影响结果，同时其也是研究流纹质火山岩地貌成因与演化过程的理想基地。  相似文献   

Basic characteristics of active tectonics of China   总被引：84，自引：8，他引：76  

邓起东  张培震  冉勇康  杨晓平  闵伟  楚全芝 《中国科学D辑(英文版)》2003,46(4):356-372

Active tectonics is inferred to all the structures which have been active since the late Pleisto-cene, 100—120 ka B.P., are still active recently, and will be active in a certain time period in the future, such as active faults, active folds, active basi…  相似文献   

北京地区单双频地基GPS大气水汽遥测试验与研究   总被引：5，自引：3，他引：5       下载免费PDF全文

谢璞  张朝林  王迎春  楚艳丽  张京江  王京丽  李矩  Ying Hwa Kuo  John Braun 《应用气象学报》2006,17(Z1):28-34

该文对北京地区单双频地基GPS大气水汽监测网布网依据、单频与双频地基GPS测量数据解算技术应用、GAMIT和Bernese地基GPS数据分析处理软件应用、远程遥控GPS数据采集与通讯系统、资料分析与数值同化应用等方面的工作进展进行简要介绍,重点讨论了单双频地基GPS大气水汽资料的解算技术及其应用效果。结果表明:在北京天气敏感区通过单双频地基GPS接收机合理组网布局,可构建并利用高分辨率电离层延迟订正技术将单频接收机的大气水汽监测精度提高到实用水平,为强降水天气预报提供有价值的产品。  相似文献   

数字化测绘的图形数据整理   总被引：1，自引：0，他引：1  

郑楚 《地理空间信息》2007,5(2):94-95

由于数据标准滞后和技术手段局限等原因,以往传统的CAD图形数据已经不能满足GIS入库的要求,因此数据整理已成为测绘工作者面临的一个重要课题。在分析图形数据的现状及其存在问题的基础上,对数据整理技术要求和方法提出了探讨,仅供同行们参考。  相似文献   

1975年海城7.3级地震在朝鲜半岛的震害及对日本九州地区的影响s          下载免费PDF全文

李裕澈  秋教昇  石川有三 《地震学报》2007,29(2):214-221

1975年中国海城7.3级地震波及整个朝鲜半岛，乃至日本九州地区. 本文系统收集了该震有关资料，并通过整理分析勾画出其烈度分布，以探讨该震的震害特点. 在半岛的北部， 除局部地区为Ⅵ度之外，大部分地区为Ⅴ度区，其震害情况与相同烈度的典型特征基本相符； 半岛南部大部分地区为Ⅳ度区. 然而，韩国首尔等大城市，除高层建筑强烈振动之外，还有人出现眩晕症状等特别的感觉，个别街区变压器跳闸造成一时停电. 这些可能是大震的长周期波在远场的效应所致.   相似文献   

Current plate motions across the Red Sea   总被引：3，自引：0，他引：3  

Dezhi Chu  & Richard G. Gordon 《Geophysical Journal International》1998,135(2):313-328

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The Abundance of QSOs in Various Cold Dark Matter Models     

Wen-Bin Lin  Yao-Quan Chu 《Astrophysics and Space Science》1998,262(1):15-27

Based on the statistics of the peaks in the random Gaussian field, we put forward a method to model the evolution of quasars, which are assumed to be a phenomenon of the early stages for some massive galaxies. Our calculations show that the cold-hot mixed dark matter model with _h = 0.3 cannot match the observed quasar abundance at redshift z = 4.5, and other prevailing CDM models, such as the mixed dark matter model with _h = 0.2, the tilted CDM models with n = 0.7 or 0.8, and the flat CDM models with = 0.6 or 0.7, are compatible with the observation of the abundance of QSOs on the range of z = 2-5.  相似文献   

HIGH INPUT IMPEDANCE TRANSISTOR AMPLIFIER FOR ACCELERATION MEASUREMENT     

Li Chu 《岩土力学》1980,2(2):65-74

This paper describes a high input impedance preamplifier ,a main amplifier ,including its specification and the circuits theories .An acceleration measurement system consist of the piezoelectric acceleration 、preamplifier、cable 、main amplifier and oscilloscope for measureing the acceleration of vibration due to explosion .The features of the system are :1.good stability ,2.small zero shift ,3.The preamplifier is a new circuit which consists of four transistors 3DG6C,3DG4E. Its input impedance is as high as 1500MΩ and is able to undertake a high instantaneous impulse voltage ,4.There is no power supply set near the preamplifier .The signal transmiting cable is also the power supply cable so that the transmiting characteristic is very well .when the cable length is varied from 1 meter to 1000 meters ,the frequency response of system will not change .The decrement of output amplitude is less than 6% etc.  相似文献   

A Theoretical and Experimental Investigation of Energy-Containing Scales in the Dynamic Sublayer of Boundary-Layer Flows   总被引：2，自引：2，他引：0  

Gabriel Katul  Chia-Ren Chu 《Boundary-Layer Meteorology》1998,86(2):279-312

The existence of universal power laws at low wavenumbers (K) in the energy spectrum (E_u) of the turbulent longitudinal velocity (u) is examined theoretically and experimentally for the near-neutral atmospheric surface layer. Newly derived power-law solutions to Tchen's approximate integral spectral budget equation are tested for strong- and weak-interaction cases between the mean flow and turbulent vorticity fields. To verify whether these solutions reproduce the measured E_u at low wavenumbers, velocity measurements were collected in the dynamic sublayer of the atmosphere at three sites and in the inner region of a laboratory open channel. The atmospheric surface layer measurements were carried out using triaxial sonic anemometers over tall corn, short grass, and smooth desert-like sandy soil. The open channel measurements were performed using a two-dimensional boundary-layer probe above a smooth stainless steel bed. Comparisons between the proposed analytical solution for E_u, the dimensional analysis by Kader and Yaglom, and the measured Haar wavelet E_u spectra are presented. It is shown that when strong interaction between the mean flow and turbulent vorticity field occurs, wavelet spectra measurements, predictions by the analytical solution, and predictions by the dimensional analysis of Kader-Yaglom (KY) are all in good agreement and confirm the existence of a -1 power law in E_u(= C_uuu² _* K^-1, where C_uu is a constant and u_* is the friction velocity). The normalized upper wavenumber limit of the -1 power law (Kz = 1, where z is the height above the zero-plane displacement) is estimated using two separate approaches and compared to the open channel and atmospheric surface-layer measurements. It is demonstrated that the measured upper wavenumber limit is consistent with Tchen's budget but not with the KY assumptions. The constraints as to whether the mean flow and turbulent vorticity strongly interact are considered using a proposed analysis by Panchev. It is demonstrated that the arguments by Panchev cannot be consistent with surface-layer turbulence. Using dimensional analysis and Heisenberg's turbulent viscosity model, new constraints are proposed. The new constraints agree with the open channel and atmospheric surface-layer measurements, Townsend's inactive eddy motion hypothesis, and the Perry et al. analysis.  相似文献