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Introduction The research on the structure and physical property of ancient hidden hill, igneous rocks and basement is relatively difficult by using seismic data only. If we combine seismic data, magneto-telluric (MT) data and geophysical data together, better results can be obtained for the above problem. A number of geophysicists at home and abroad, such as CHEN and WANG (1990), Siri-punvarapor and Egbert (2000) have tried many methods to solve the problem by the inversion of seismic da… 相似文献
645.
Introduction The Great North China, located at longitude 106E to 124E and latitude 31N to 42N, in-cludes three secondary active tectonic blocks, Ordos, Yanshan and North China plain (Figure 1). The geological tectonics of these three secondary blocks is much different from each other. As a stable block with high rigidity, the Ordos block is mostly surrounded by down-faulted basins with an inactive interior since Cenozoic, although the fault zones along its boundary are strongly active wi… 相似文献
646.
Introduction Data mining (SHAO and YU, 2003) is a new kind of technique developed with database and artificial intelligence in recent years, which processes the data in the database to abstract the im- plied and pre-unknown, but potentially useful information and knowledge from large amounts of incomplete, noisy, blurring and stochastic data. For data mining, data purging is an important link beforehand that includes eliminating noise, making up lost domain, and deleting ineffective data, as… 相似文献
647.
Introduction Estimation of an attenuation relationship for strong ground motion parameters has been an interesting research subject in the field of engineering seismology and has played a very important role in seismic safety evaluation, seismic zoning, seismic hazard evaluation of major constructions, etc. At present, the generally used parameters include peak acceleration, peak velocity and elastic response spectrum. Such parameters mentioned above are essentially independent of the duration… 相似文献
648.
LI Rongfeng YOU Xiaobao & Peter C. Chu . LASG Institute of Atmospheric Physics Chinese Academy of Sciences Beijing China . Department of Oceanography Naval Postgraduate School Monterey CA - USA 《中国科学D辑(英文版)》2005,48(7)
The classic Sverdrup theory suggests that the water movement in the central subtropical gyre of North Pa-cific be slowly westward or southwestward.In the late sixties of the20th century,the existence of a peculiar eastward narrow flow between20°N and25°N in spring was theoretically predicted.It was named the Subtropical Countercurrent(STCC),although direct observational evidences were not yet sufficient to con-firm whether or not such eastward flow between20°N and25°N was a persistent… 相似文献
649.
The time history of strong ground motion can be synthesized by empirical Green's function (EGF) method.Firstly a large seismic event is discretized into a series of subevents; secondly recordings of earthquakes with proper size and spatial distribution are chosen as time history (EGF) of those subevents; finally the EGFs are summated to get the time history of ground motion caused by the large event. 相似文献
650.
Global ocean circulation models usually lack an adequate consideration of high-latitude processes due to a limited model domain
or insufficient resolution. Without the processes in key areas of the global thermohaline circulation, the characteristics
and flow of deep and bottom waters cannot be modeled realistically. In this study, a high-resolution (~20 km) ocean model
focused on the Weddell Sea sector of the Southern Ocean is combined with a low-resolution (2° × 2°) global ocean model applying the state estimation technique. Temperature, salinity, and velocity data on two Weddell Sea
sections from the regional model are used as constraints for the large-scale model in addition to satellite altimetry and
sea-surface temperatures. The differences between the model with additional constraints and without document that the Weddell
Sea circulation exerts significant influence on the course of the Antarctic Circumpolar Current with consequences for Southern
Ocean water mass characteristics and the spreading of deep and bottom waters in the South Atlantic. Furthermore, a warming
trend in the period 1993–2001 was found in the Weddell Sea and adjacent basins in agreement with float measurements in the
upper Southern Ocean. Teleconnections to the North Atlantic are suggested but need further studies to demonstrate their statistical
significance. 相似文献