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641.
The morphotectonics and its evolutionary dynamics of the central Southwest Indian Ridge (49° to 51°E) 总被引:1,自引:1,他引:0
LIANG Yuyang LI Jiabiao LI Shoujun RUAN Aiguo NI Jianyu YU Zhiteng ZHU Lei 《海洋学报(英文版)》2013,32(12):87-95
The morphotectonic features and their evolution of the central Southwest Indian Ridge (SWIR) are dis- cussed on the base of the high-resolution flfll-coverage bathyraetric data on the ridge between 49°-51°E. A comparative analysis of the topographic features of the axial and flank area indicates that the axial topogra- phy is alternated by the ridge and trough with en echelon pattern and evolved under a spatial-temporal mi- gration especially in 49°-50.17°E. It is probably due to the undulation at the top of the mantle asthenosphere, which is propagating with the mantle flow. From 50.17° to 50.7°E, is a topographical high terrain with a crust much thicker than the global average of the oceanic crust thickness. Its origin should be independent of the spreading mechanism of ultra-slow spreading ridges. The large numbers of volcanoes in this area indicate robust magmatic activity and may be related to the Crozet hot spot according to RMBA (residual mantle Bouguer anomaly). The different geomorphological feature between the north and south flanks of the ridge indicates an asymmetric spreading, and leading to the development of the OCC (oceanic core complex). The tectonic activity of the south frank is stronger than the north and is favorable to develop the OCC. The first found active hydrothermal vent in the SWIR at 37°47'S, 49°39'E is thought to be associated with the detach- ment fault related to the OCC. 相似文献
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644.
马里亚纳海沟“挑战者深渊”最深点水深探测 总被引:1,自引:0,他引:1
20112012年,海洋六号船采用EM122多波束测深系统在马里亚纳海沟最深海域"挑战者深渊"进行的多波束水深测量,通过对测深资料进行分析处理,获得了高精度海底地形图,揭示了马里亚纳海沟挑战者深渊附近海底地形呈近东西向延伸,有西部、中部和东部三个洼地,它们由10800m等深线圈闭,长轴方向与海沟方向一致。洼地底部水深大于10900m,地形较为平坦。三个洼地最深区域分别由10916m、10904m和10915m等深线圈闭。三个洼地最大水深为10917m(误差小于20m),位于西部洼地内,中心位置为142°12.14'E,11°19.92'N。该处也是马里亚纳海沟最深点。 相似文献
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研究了多模卫星导航系统的RAIM(接收机完好性自主检测)算法,根据多模卫星导航系统的定位模型,基于最小二乘法的原理计算伪距残差,构造奇偶矢量进行故障检测和故障排除。在只有一个观测量出现粗差的前提下,仿真了GPS与多模GPS/GLONAss/Galileo系统下的卫星可见数和DOP(精度因子),对比了衡量RAIM算法可用性的水平保护门限值(HPL)及这2种系统下的故障检测率与故障排除率。仿真结果表明:与GPS相比,多模导航系统具有更多的可见星,RAIM算法的可用性更高,并且其故障检测和故障排除的性能更好。因此,多模卫星导航系统不仅能为用户提供更高的定位精度,还能为用户提供更好的完好性保障。 相似文献
647.
A space-qualified low-noise 22 GHz receiver for the international space-VLBI mission Radioastron has been constructed. The microwave electronics is realized by using thermally matched hybrid circuits. The most important properties of the receiver are phase stability, sensitivity and reliability. The high sensitivity is due to a cooled low noise HEMT amplifier (LNA). The measured receiver noise temperature is less than 100 K. The phase stability is achieved by compact structure and thermal stabilization. Phase stabilities of better than 0.13°/°C and 0.2°/°C for the receiver and the LNA units are measured, respectively. The calculated reliability of the receiver exceeds the requirement of 0.97 for the three year mission. 相似文献
648.
Swath mapping system processing: Bathymetry and cartography 总被引:1,自引:0,他引:1
J. F. Bourillet C. Edy F. Rambert C. Satra B. Loubrieu 《Marine Geophysical Researches》1996,18(2-4):487-506
649.
Larry A. Mayer 《Marine Geophysical Researches》2006,27(1):7-17
Over the past few years there have been remarkable and concomitant advances in sonar technology, positioning capabilities,
and computer processing power that have revolutionized the mapping, imaging and exploration of the seafloor. Future developments
must involve all aspects of the “seafloor mapping system,” including, sonars, ancillary sensors (motion sensors, positioning
systems, and sound speed sensors), platforms upon which they are mounted, and the products that are produced. Current trends
in sonar development involve the use of innovative new transducer materials and the application of sophisticated processing
techniques including focusing algorithms that dynamically compensate for the curvature of the wavefront in the nearfield and
thus allow narrower beam widths (higher lateral resolution) at close ranges . Future developments will involve “hybrid”, phase-comparison/beam-forming
sonars, the development of broad-band “chirp” multibeam sonars, and perhaps synthetic aperture multibeam sonars. The inability
to monitor the fine-scale spatial and temporal variability of the sound speed structure of the water column is often a limiting
factor in the production of accurate maps of the seafloor; improvements in this area will involve continuous monitoring devices
as well as improved ocean models and perhaps tomography. Remotely Operated Vehicles (ROV’s) and particularly Autonomous Underwater
Vehicles (AUV’s) will become more important as platforms for seafloor mapping systems. There will also be great changes in
the products produced from seafloor mapping and the processing necessary to create them. New processing algorithms are being
developed that take advantage of the density of multibeam sonar data and use statistically robust techniques to “clean” massive
data sets very rapidly. A range of approaches are being explored to use multibeam sonar bathymetry and imagery to extract
quantitative information about seafloor properties, including those relevant to fisheries habitat. The density of these data
also enable the use of interactive 3-D visualization and exploration tools specifically designed to facilitate the interpretation
and analysis of very large, complex, multi-component spatial data sets. If properly georeferenced and treated, these complex
data sets can be presented in a natural and intuitive manner that allows the simple integration and fusion of multiple components
without compromise to the quantitative aspects of the data and opens up new worlds of interactive exploration to a multitude
of users. 相似文献
650.
Jean-Yves Collot Jean Delteil Keith B. Lewis Bryan Davy Geoffroy Lamarche Jean-Christophe Audru Phil Barnes Franck Chanier Eric Chaumillon Serge Lallemand Bernard Mercier de Lepinay Alan Orpin Bernard Pelletier Marc Sosson Bertrand Toussaint Chris Uruski 《Marine Geophysical Researches》1996,18(2-4):357-381
The southern Kermadec-Hikurangi convergent margin, east of New Zealand, accommodates the oblique subduction of the oceanic Hikurangi Plateau at rates of 4–5 cm/yr. Swath bathymetry and sidescan data, together with seismic reflection and geopotential data obtained during the GEODYNZ-SUD cruise, showed major changes in tectonic style along the margin. The changes reflect the size and abundance of seamounts on the subducting plateau, the presence and thickness of trench-fill turbidites, and the change to increasing obliquity and intracontinental transpression towards the south. In this paper, we provide evidence that faulting with a significant strike-slip component is widespread along the entire 1000 km margin. Subduction of the northeastern scrap of the Hikurangi Plateau is marked by an offset in the Kermadec Trench and adjacent margin, and by a major NW-trending tear fault in the scarp. To the south, the southern Kermadec Trench is devoid of turbidite fill and the adjacent margin is characterized by an up to 1200 m high scarp that locally separates apparent clockwise rotated blocks on the upper slope from strike-slip faults and mass wasting on the lower slope. The northern Hikurangi Trough has at least 1 km of trench-fill but its adjacent margin is characterized by tectonic erosion. The toe of the margin is indented by 10–25 km for more than 200 km, and this is inferred to be the result of repeated impacts of the large seamounts that are abundant on the northern Hikurangi Plateau. The two most recent impacts have left major indentations in the margin. The central Hikurangi margin is characterized by development of a wide accretionary wedge on the lower slope, and by transpression of presubduction passive margin sediments on the upper slope. Shortening across the wedge together with a component of strike-slip motion on the upper slope supports an interpretation of some strain partitioning. The southern Hikurangi margin is a narrow, mainly compressive belt along a very oblique, apparently locked subduction zone. 相似文献