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21.
本文提供了1989~1991年广东近岸表层水中~(90)Sr和~(137)Cs含量的分析结果。在调查海区,~(90)Sr含量为2.31~3.75mBq/L,平均值为3.21±0.45mBq/L。~(137)Cs含量为2.10~4.49mBq/L,平均值为3.47±0.89mBq/L。~(137)Cs/~(90)Sr放射性的比值为0.63~1.69,平均值为1.11±0.35。调查结果表明,近三年来未发现广东近岸海域有明显的人工放射性污染。目前广东近岸海水中的~(90)Sr和~(137)Cs主要仍是以往核试验所产生的放射性落下灰残余。 相似文献
22.
A three-component decomposition is applied to global analysis data to show the existence of a beta
gyre, which causes Tropical Cyclone (TC) to drift from a large-scale environmental steering current. Analyses
from the Global Data Assimilation and Prediction System (GDAPS) of the Korea Meteorological Administration (KMA),
the Global Forecast System (GFS) of NCEP, and the Navy Operational Global Atmospheric Prediction System (NOGAPS)
are used in this study.
The structure of the beta gyre obtained in our analyses is in good agreement with the theoretical structure,
with a cyclonic circulation to the southwest of the TC center, an anticyclonic circulation to the northeast,
and a ventilation flow directed northwestward near the center. The circulation of the beta gyre is strongest
at the 850-hPa level where the cyclonically swirling primary circulation is strongest, and decreases with
height, in a pyramid shape similar to the primary circulation. The individual structure of the beta gyre is
case- and model-dependent. At a certain analysis time, one model may clearly reveal a well-defined beta gyre,
but the other models may not. Within one model, the beta gyre may be well defined at some analysis times,
but not at other times. The structure of the beta gyre in the analysis field is determined by the nature of
the vortex initialization scheme and the model behavior during the 6-h forecast in the operational data
assimilation cycle. 相似文献
23.
根据BKG中心的转换参数结果,采用FFT方法,计算分析了PZ-90GLONASS与ITRF间转换参数及其周期变化特性,并得出了一些有益的结论。 相似文献
24.
This is a preliminary report on two sets of recent observations from a region of active tectonics that provide comparatively direct evidence for the critical state of the fluid-saturated microcracked crust. The first data set from crosshole seismics in a controlled source stress-monitoring site (SMS) shows that the crust of the Earth is highly compliant and responds to low-level changes of tectonic stress at substantial distances. The second set of data from earthquake seismograms shows that the seismically active Húsavík–Flatey Fault plane is pervaded by critically high pore-fluid pressures, which cause 90° flips in the polarisations of seismic shear waves. We suggest that both sets of observations confirm previous hypotheses for a compliant crack-critical (CCC) crust. This is a new understanding of low-level pre-fracturing deformation that has fundamental implications for a range of applications in solid earth geophysics. These applications range from monitoring hydrocarbon production with time-lapse seismics to monitoring tectonic stress in in situ rock and stress-forecasting the times and magnitudes of impending large earthquakes. 相似文献
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重磁数据处理在地球物理中占有很重要的地位.利用Fortran 90语言对现有的Fortran 77程序进行了改写,克服了受内存的限制,并且实现了在Visual Fortran环境下的图形图像显示. 相似文献
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《The Professional geographer》2013,65(3):367-368
ATLAS?GRAPHICS (Version 3.0). AutoCAD (Release 9.0 with ADE+1, ADE+2 and ADE+3). AutoSketch (Speed Enhanced Version 1.02). NUMERICAL RECIPES FORTRAN. Numerical Recipes Software SCIPLOT. 相似文献
30.
Ordovician backarc‐basin metadolerite and metabasalt of the South Kitakami Terrane,Northeast Japan 下载免费PDF全文
Basement rocks that occur along the northern margin of the South Kitakami Terrane in Japan consist of Ordovician ultramafic rocks (Hayachine ultramafic complex), gneissose amphibolite (Kuromoriyama amphibolite), and mafic rocks (Kagura igneous rocks, KIR). The KIR are composed of metagabbro, metadolerite, metabasalt, and minor felsic–intermediate dikes. Although the KIR contain green hornblende due to metamorphism of greenschist to epidote–amphibolite facies, they rarely retain primary brown hornblende. Approximately 30% of the metabasalt shows porphyritic textures, with phenocrysts of saussuritized plagioclase and/or altered mafic minerals. The geochemistry of the common metadolerite and metabasalt of the KIR shows a tholeiite trend, a low TiO2 content, and high Th/Nb and Ti/V ratios. The KIR are therefore indicative of a supra‐subduction zone tectonic setting, which implies a backarc origin (as also indicated by discrimination diagrams). Trace element patterns of the KIR resemble those of the backarc‐basin basalt of the Japan and Yamato basins in the Japan Sea. We propose that the KIR formed during backarc spreading from the Ordovician to Early Silurian. This view is supported by the geochemical data, the tectonic setting of the Hayachine ultramafic rocks, and the provenance of clastics within Silurian sedimentary rocks. 相似文献