Design Method of Armour Grate Plates for Sloping Breakwaters     

Wu Guiqiu  Ji Zaihua Sun Xuexin Zhang Jiuzi Associate Professor  First Institute of Oceanography  State Oceanic Administration  Qingdao Associate Professor 《中国海洋工程》1993,(1)

- Laboratory tests have been conducted on the basis of theoretical analysis of stability of armour Grate Plates with reference to 20 structures. Some empirical formulas of statility thickness of Grate Plates have been obtained in consideration of the effects of water depth in front of the structures and critical wave period. The test results have been compared with field data.  相似文献   

F阵广义积的运算保持性质及其应用     

刘文斌  李敏 《中国海洋大学学报(自然科学版)》2006,36(6):889-891

给出F阵广义积的概念,在较为广泛的范围内,讨论F阵与布尔阵的运算保持问题,得到F阵与布尔阵运算一致性的法则,为F阵的研究提供新的方法和视角。  相似文献   

高分辨率光学卫星遥感影像高精度无地面控制精确处理的理论与方法   总被引：3，自引：2，他引：1  

龚健雅  王密  杨博 《测绘学报》2017,46(10):1255-1261

卫星影像全球无地面控制高精度几何定位是卫星摄影测量技术发展追求的主要目标,也是实现困难地区和境外地区测图的关键支撑技术。本文围绕我国国产遥感卫星的技术发展,详细论述了高分辨率光学卫星遥感影像高精度无地面控制几何定位的理论与方法,在天星地一体化全链路误差建模分析的基础上,提出了在轨几何定标理论与方法、稳态重成像几何处理模型与方法及大规模无地面控制区域网平差理论与方法。将本文方法应用于资源三号卫星影像的数据处理,试验结果满足1∶50 000测图精度,证明了理论和方法的正确性。  相似文献   

基于可见光通信的MIMO技术研究现状     

迟楠  乔梁  赵嘉琦  卢星宇 《南京气象学院学报》2017,9(2):113-122

随着灯光与光无线通信技术的结合,基于LED的可见光通信（VLC）越来越受到人们的关注.本文首先探讨了可见光通信的基带处理过程.为了提高室内照明度,LED阵列渐渐被广泛使用,基于此,可见光通信系统中基于LED阵列的MIMO技术也进入研究者的视野,因此,随后介绍了两种VLC-MIMO机制,并介绍了空时分组编码（STBC）在VLC-MIMO系统中的研究进展.作为对比,最后对LTE系统中的物理层处理过程和多天线技术进行技术探讨,并大胆预测了可见光通信基带处理后续可能发展的方向.  相似文献   

Numerical modeling of block structure dynamics: dependence of a synthetic earthquake flow on the structure separateness and boundary movements     

V. I. Keilis-Borok  I. M. Rotwain  A. A. Soloviev 《Journal of Seismology》1997,1(2):151-160

A seismically active region is modelled as a system of absolutely rigid blocks separated by infinitely thin plane faults. The interaction of the blocks along the fault planes and with the underlying medium is viscous-elastic. The system of blocks moves as a consequence of prescribed motion of the boundary blocks and of the underlying medium. When for some part of a fault plane the ratio of the stress to the pressure exceeds a certain strength level a stress-drop (a failure) occurs (in accordance with the dry friction model), and it can cause a failure in other parts of the fault planes. In the model the failures represent earthquakes. As a result of the numerical simulation a synthetic earthquake catalog is produced. The numerical modelling was carried out for three types of structures with increasing of the structure separateness inside of each type and for two types of boundary movements. A synthetic earthquake flow is characterised by several features including the frequency-magnitude relation (the Gutenberg-Richter curve). When the structure separateness increases the slope of the curve changes monotonously in the same direction for all considered types of structures if the boundary movement is the same. The directions of changing of the slope are opposite for two considered boundary movements.  相似文献   

3-D Shear Wave Velocity Structure of the Crust and Upper Mantle in South China Sea and its Surrounding Regions by Surface Wave Dispersion Analysis   总被引：5，自引：0，他引：5  

Hsin-Hung Wu  Yi-Ben Tsai  Tung-Yi Lee  Ching-Hua Lo  Chao-Hui Hsieh  Dinh Van Toan 《Marine Geophysical Researches》2004,25(1-2):5-27

In this study, we construct a 3-D shear wave velocity structure of the crust and upper mantle in South China Sea and its surrounding regions by surface wave dispersion analysis. We use the multiple filter technique to calculate the group velocity dispersion curves of fundamental mode Rayleigh and Love waves with periods from 14 s to 120 s for earthquakes occurred around the Southeast Asia. We divide the study region (80° E–140° E, 16° S–32° N) into 3° × 3° blocks and use the constrained block inversion method to get the regionalized dispersion curve for each block. At some chosen periods, we put together laterally the regionalized group velocities from different blocks at the same period to get group velocity image maps. These maps show that there is significant heterogeneity in the group velocity of the study region. The dispersion curve of each block was then processed by surface wave inversion method to obtain the shear wave velocity structure. Finally, we put the shear wave velocity structures of all the blocks together to obtain the three-dimensional shear wave velocity structure of crust and upper mantle. The three-dimensional shear wave velocity structure shows that the shear wave velocity distribution in the crust and upper mantle of the South China Sea and its surrounding regions displays significant heterogeneity. There are significant differences among the crustal thickness, the lithospheric thickness and the shear wave velocity of the lid in upper mantle of different structure units. This study shows that the South China Sea Basin, southeast Sulu Sea Basin and Celebes Sea Basin have thinner crust. The thickness of crust in South China Sea Basin is 5–10 km; in Indochina is 25–40 km; in Peninsular Malaysia is 30–35 km; in Borneo is 30–35 km; in Palawan is 35 km; in the Philippine Islands is 30–35 km, in Sunda Shelf is 30–35 km, in Southeast China is 30–40 km, in West Philippine Basin is 5–10 km. The South China Sea Basin has a lithosphere with thickness of about 45–50 km, and the shear wave velocity of its lid is about 4.3–4.7 km/s; Indochina has a lithosphere with thickness of about 55–70 km, and the shear wave velocity of its lid is about 4.3–4.5 km/s; Borneo has a lithosphere with thickness of about 55–60 km, and the shear wave velocity of its lid is about 4.1–4.3 km/s; the Philippine Islands has a lithosphere with thickness of about 55–60 km, and the shear wave velocity of its lid is about 4.2–4.3 km/s, West Philippine Basin has a lithosphere with thickness of about 50–55 km, and the shear wave velocity of its lid is about 4.7–4.8 km/s, Sunda Self has a lithosphere with thickness of about 55–65 km, and the shear wave velocity of its lid is about 4.3 km/s. The Red-River Fault Zone probably penetrates to a depth of at least 200 km and is plausibly the boundary between the South China Block and the Indosinia Block.  相似文献   

防波堤断面结构型式及护面块体稳定性模型试验研究——2008北京奥运会青岛帆船比赛基地水工模型试验     

史宏达  HAN Gui-Ping  韩桂萍  范天会 《中国海洋大学学报(自然科学版)》2006,36(6):999-1007

为确保2008北京奥运会青岛帆船比赛基地内工程的水工建筑物安全可靠，对给定的2种防波堤断面结构型式及护面块体稳定性进行物理模型试验。准确掌握在极端高水位、设计高水位、设计低水位和极端低水位时．SW向、25a和50a一遇波浪作用下，试验断面所承受的波浪作用力，及SE向50a一遇波浪作用下块体的稳定重量。并绘制各工况1％峰值波压力分布图，得出断面波压力的分布规律。对断面结构和护面块体稳定性进行分析。  相似文献   

滇西北独龙江岩浆弧和丙中洛地块的划分与特征     

王学武  李新仁  刘凤祥  严城民  周喜林  王长兵 《世界地质》2016,35(4):1034-1040

为查明滇西北贡山地区大地构造单元的划分与特征,系统收集整理了不同比例尺的区域地质调查资料,得出4方面新认识:1该区大地构造单元划分为独龙江岩浆弧和丙中洛地块,二者分界为向东倾斜的高黎贡山逆冲推覆断裂;2独龙江岩浆弧属腾冲造山带,丙中洛地块属三江造山带,其间被中特提斯洋所分隔;3中特提斯洋于中侏罗世打开,晚侏罗世—早白垩世早期向西俯冲消减,早白垩世晚期—晚白垩世闭合;4班公错—东巧缝合带在该区已被向西逆冲推覆的高黎贡山岩群(Pt_1G.)所压覆。  相似文献   

柴北缘乌兰地区花岗岩锆石SHRIMP定年及其成因   总被引：4，自引：0，他引：4  

吴才来  雷敏  吴迪  李天啸 《地球学报》2016,37(4):493-516

柴北缘乌兰地区花岗岩锆石SHRIMP U-Pb定年结果表明,哈德森沟岩体的年龄为(413±3)Ma,许给沟岩体的年龄为(254±3)Ma,椅落山岩体的年龄为(251±1)Ma,察汗诺岩体角闪闪长岩和花岗岩的年龄分别为(249±1)Ma和(248±2)Ma,察汗河岩体年龄为(240±2)Ma,晒勒克郭来岩体的花岗闪长岩和花岗岩年龄分别为(250±1)Ma和(244±3)Ma。从年龄上看,这些花岗岩明显地分为两期:早期属早泥盆世(年龄为413 Ma),形成的岩石组合为:石英二长岩+碱长花岗岩;晚期属晚二叠世—早三叠世(年龄为254~240 Ma),又可进一步细分为254~251 Ma、250~248 Ma、244~240 Ma三次侵位,对应的岩石组合为:闪长岩+花岗闪长岩+花岗岩。岩石地球化学研究表明,早期花岗岩类不仅富集大离子亲石元素,而且还富集部分高场强元素(Zr、Y、Nb等),属A型花岗岩;晚期花岗岩类富集大离子亲石元素,亏损高场强元素,属I型花岗岩。早期花岗岩的87Sr/86Sr比值(0.710 8)和Nd模式年龄(T2DM=2.10 Ga)均高于晚期花岗岩(0.707 6~0.710 7,T2DM=1.41~1.58 Ga),但晚期花岗岩的εNd(t)值(-11.6)低于早期花岗岩(-4.8~-6.8),表明早期A型花岗岩可能起源于古元古代的大陆地壳,而晚期I型花岗岩起源于中元古代地壳。结合区域地质构造特征,我们认为,早期A型花岗岩的形成与祁连岩石圈拆沉导致欧龙布鲁克陆块北缘减薄、拉伸有关,也标志着宗雾隆裂陷的开始;而晚期I型花岗岩类的形成与宗雾隆洋壳向南俯冲于欧龙布鲁克陆块之下有关。  相似文献   

鹤庆-洱源断裂带中段晚更新世以来的走滑活动     

沈晓明  李德文  孙昌斌  康艳蕊  刘睿  张亚娇 《大地构造与成矿学》2016,(1):29-37

鹤庆–洱源断裂带是滇西北活动断裂系的重要组成部分,对其性质、特征和活动历史的研究可为区域地震活动评价和震害防御提供依据,也可为青藏高原东南缘构造变形特征、历史和方式提供基础数据。通过对鹤庆–洱源断裂带中段基岩山区的室内外调查和研究,结合光释光和14C 定年,初步查明该段断裂具有复杂的空间展布格局,由多条左旋走滑性质的分支断裂构成,它们共同吸收了断裂带在鹤庆盆地南端与洱源盆地北端之间的走滑分量;运动性质以左旋走滑为主,局部地段兼具正断或逆冲性质;剖面地层断错和覆盖关系表明该段断裂在晚更新世活动强烈,现有证据表明最新活动时代约为距今2万年。结合区域构造环境,作者认为鹤庆–洱源断裂带中段晚更新世以来的活动是对青藏高原强烈隆升的响应,其左旋走滑符合滇中次级块体顺时针转动模型,是块体旋转在角端的局部应变响应。  相似文献