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861.
The probability of received-power fluctuation in the turbulent atmosphere is discussed with a simple and yet reasonable model for a direct-detection optical system. Good agreement was found between the theore-tical results and the field experiment. Thus the analysis in this paper may be taken as a guide for the design of atmospheric optical system. 相似文献
862.
Yu-Jun Zhang Xing-Bin Li Lin-Shan Song Ling Yuan Bao-Guan Chen Bing-Ru Chen Yu-Oi Wang Jing-Xin Sun 《Geostandards and Geoanalytical Research》1986,10(1):61-71
The concentrations of 36 elements in geochemical reference samples issued by the Ministry of Geology and Mineral Resources of China were determined by neutron activation analysis. Three main variants of the technique, instrumental, epithermal, and nreirradiation separation neutron activation analysis (INAA, ENAA, PNAA), were employed in a systematic study of the samples by three laboratories: the Institute of Atomic Energy of the Academia Sinica (INAA, ENAA), the Institute of High Energy Physics of the Academia Sinica (INAA), and the Institute of Geophysical and Geochemical Prosnecting of the Ministry of Geology and Mineral resources (INAA,PNAA). Both long and short irradiations and both Ge(Li) and HPGe detectors were used. A supplementary software nackage for data processing was developed. About 81% of the data determined by neutron activation agreed with recomended values with in 15%. 相似文献
863.
长江三峡工程坝址西南约10km的狮子口地区,发育一个长约8km、宽约3km的重力滑动构造系统。它由下伏系统、滑动系统和前缘推挤带构成,是一个典型的多层次滑褶型重力滑动构造。它形成时的温、压条件为130.5~193.7℃和180~230MPa;l;形成深度约5~10km;总体岩层收缩量32.2%;总滑移距离1060m;活动时间上限127.65士38.29万年。它是燕山运动期间南北向挤压体制下,在黄陵背斜东、西两侧应力屏蔽区内派生的近东西向拉伸构造应力场的产物。 相似文献
864.
通过对胶东牟平-乳山地区1:2.5万航空甚低频电磁异常的分析研究,并结合航磁,航放、遥感以及区域构造地质资料,进行了构造地质填图,首次进一步证实了被前人所忽视的近东西向断裂构造的存在,并给予了准确定位。在此基础上进行了金矿成矿远景预测,取得了比较满意的效果。 相似文献
865.
This paper discusses the Cretaceous-Tertiary magnetic polarity sequence of the the Hengyang Basin on the basis of magnetostratigraphic study. The age of each stratigraphic unit has been determined with the magnetic polarity time scale combined with 39Ar/40Ar dating, thus providing evidence for determining the geological ages of different formations. The authors assign the age of the Dongjing Formation of the Hengyang Basin to Early Cretaceous, the Shenhuangshan Formation to Early-Late Cretaceous, the Daijiaping Formation to Late Cretaceous, and the Dongtang and Xialiushi formations to Palaeocene. 相似文献
866.
陆内碰撞体制流体作用及成矿作用研究的意义和现状 总被引:11,自引:0,他引:11
陆内碰撞作用和流体作用都是80年代以来的研究前沿,它们的研究必然会大大促进成矿作用研究的发展,也是跟踪和超越世界地球科学先进水平的重要途径。中国拥有最多最复杂的陆内碰撞带,为中国学者开发有关研究并取得高水平成果提供了得天独厚的条件。对陆内碰撞、流体作用和成矿作用研究现状的分析表明,三者之间研究的相互结合是薄弱环节,限制了有关问题的深入,但为我国学者开发该方向的研究,取得领先于国家水平的成果,提供了 相似文献
867.
四川盆地基底及深部地质结构研究的进展 总被引:6,自引:1,他引:6
根据对近年来区域地质、多种地球物理资料和深钻井资料的综合研究,认为四川盆地属扬子板块,岩石圈巨厚,最厚可达200km。川西高原属青藏板块的东缘,同时位于中国南北构造带中段,软流圈呈北东向上隆,岩石圈减薄,其最薄处厚度约70km左右。四川盆地的基底由结晶基底与沉积岩变质基底组成,上震旦统为该地区在扬子古板块形成后的第一套沉积盖层。基底的性质、厚度、埋深在不同地区各不相同,从而决定了盆地内部构造区的划分。基底深断裂对盆地的形成与盖层构造的发展也有重要的控制作用。 相似文献
868.
Jian Sheng 《Climate Dynamics》1995,12(2):125-140
The Madden-Julian oscillation (MJO) simulated by the Canadian Climate Centre general circulation model (CCC GCM) is identified
by a principal oscillation pattern (POP) analysis and compared with that observed in the real atmosphere. The results are
based upon two integrations of the CCC GCM, one with a parameterization of penetrative cumulus convection (EXP1) and the other
with a moist convective adjustment scheme (EXP2). The signal of MJO can be detected in both integrations as the first POP
of the 200 hPa velocity potential along the equator. The disturbances show a distinctive wave number one structure with the
strongest local amplitude found in the longitudes corresponding to the region of the Asian monsoon. The phase speed of the
eastward wave propagation is higher in the eastern Pacific and lower in the monsoon region where the convective activities
are strongest. These features are in good agreement with the observations. The energy spectrum of the velocity potential peaks
at the frequency corresponding to a period of about 38 days for EXP1, which is somewhat shorter compared to the observed periods
of 40–50 days. On the other hand, two spectral peaks can be clearly identified for EXP2, one with a period of 24 days and
the other with a much longer period, somewhere near 112 days. Both peaks appear statistically significant at 95% level. Long
term data of the observed atmosphere show little indication of such spectral separation. The horizontal patterns identified
by the POP analysis resemble to some extent the baroclinic response of tropical flow to a heat source travelling with the
speed of MJO. At the upper level, Rossby wave energy propagates westward with winds generally following the height contours,
whereas Kelvin wave energy propagates to the east from the heat source with strong cross-contour flow near the equator. At
the lower level, the patterns are essentially reversed. The model-generated precipitation and diabatic heating are examined
by compositing against the moving MJO. It is found in EXP2 that the composite heating distribution is coherent with the flow
pattern only in a certain sector of the equator, depending on whether the fast or slow mode is used to determine the reference
point. The composite vertical heating profile of a slower mode tends to have a maximum found at a lower level. The sensitivity
of simulated MJO to the cumulus convection scheme in the model is discussed.
Received: 19 December 1994 / Accepted: 11 July 1995 相似文献
869.
中国地震历史资料的信息开发与利用 总被引:7,自引:1,他引:7
本文对全国历史地震资料的有用信息作了进一步的开发和利用,按统一方法处理了大量有感以上地震的文字记载,确字每个独立地震的时间与地点;分区求得地震的有感区长半径与震级的关系式;确定了历史有感地震的最低震级为4;取得了8000余次有感地震垢基本参数;用等震线测定了巨大地震的参数;将有感强震目录统编成全国与几个大区M≥4.0地震目录,按《地震学地震预报实用程序系统》(EPSEIS)的格式要求建库;同时编制 相似文献
870.
Xian-Kang Zhang Zhuo-Xin Yang Yu-Chun Yang Jian Yang Jian-Li Song Ping Zhao 《地震学报(英文版)》1995,8(4):519-529
In this paper, the theory and method, obtaining the tomographic determination of three-dimensional velocity structure of the
crust by use of the joint inversion of explosion and earthquake data, are given. The velocity distribution of the crust is
regarded as a continuous function of the spatial coordinates without parametrization of the velocity model ahead, so that
the inversion solution would not be influenced by different parametrization procedures. The expressions of integration kernels,
which relates the two kinds of data sets, are also given. The authors have processed the observed data in Tangshan earthquake
region by the method proposed in this paper, and obtained the tomographic results of the middle and upper crust structures
in this region. The comparison of these results with the result obtained only by the explosion data, has also been made. 相似文献