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991.
北京地区气温诊断分析 总被引:1,自引:0,他引:1
本文讨论了北京地区百余年气温的变化特征,依据加法模型理论,提出了一种气候诊断和预测方法─—逐步回归多重因子方法,其优点在于将序列的周期因子、谱成分及外界气候振动因子同时引入回归模型中。这一方法,对单序列的气候诊断和预测具有明显效果。 相似文献
992.
油气化探异常形成的初步数字模拟 总被引:1,自引:0,他引:1
提出了油气地球化学异常形成动力学模型,并利用计算机进行数字模拟,通过数字模拟拟得出地表或近地表油气化探异常表现的顶部形态和环形形态是近地表地球化学作用的结果,油气球化学环形异常取于地下水中的碱土金属阳离子和非碱金属阳离子的浓度。 相似文献
993.
According to the joint probabilistic distribution model of magnitude and space,the author discusses the relationship between the probabilistic distribution of magnitude in a seismic province and that in an area with potential seismic sources.The results show that if the magnitude probabilistic distribution follows the truncated exponential form in a seismic province,there must be some potential source in which the magnitude probabilistic distribution does not conform to that form.The result is consistent with the concept of "characteristic earthquake" derived from the study of actual records of seismicity and the study of geology.The author suggests that the relationship between the probabilistic distribution of magnitude in a seismic province and that in a seismic potential area must be considered in the study of the analysis of seismicity,seismic zonation and engineering seismology,for the purpose of the evaluation of the probabilistic distribution of magnitude correctly in every area with potential s 相似文献
994.
Zhao Yanlai Sun Ruomei Mei ShirongCenter for Analysis Prediction SSB Beijing China Institute of Geophysics Academia Simca Beijing China 《中国地震研究》1994,(4)
In this paper a method of relocating hypocenter in inhomogeneous medium is introduced.Based on the velocity from the latest results on the crust and mantle structure of the Bohai Sea and its adjacent areas,by using the data recorded in Shandong,Hebei,Beijing,and Liaoning networks around the Bohai Sea we apply the method to relocate hypocenter parameters of 598 events occurring in the Bohai Sea and its adjacent areas.The accuracy of hypocenter relocation is discussed.We present the results of events ML≥4.0 in the Bohai Sea in recent years and discussed the distribution of focal depths. 相似文献
995.
本文综述指出:深部过程,可能导致放射性元素在地幔或下地壳的某些部位聚结而产生强烈的核反应,致使下地壳加热和上地壳的快速抬升和伸展垮塌,产生地震、火山作用、岩浆作用,形成山脉。通过对来自地球内部的α─粒子辐射监测,有可能对毁灭性地震作出预报。 相似文献
996.
Alba Zappone 《Surveys in Geophysics》1994,15(5):619-642
In order to determine the seismic properties of rocks representing the continental crust/upper mantle transition, a structural and petrographical study of peridotites of the Ivrea-Verbano zone (N. Italy) has been undertaken. The seismic behaviour (Vp, Vs, birefringence, orientation of the fast shear-wave polarisation plane) has been calculated from the modal composition of rock samples, together with the crystallographic preferred orientation and the single crystal elastic constants, using the methods of Mainprice (1990). It is shown that the intrinsic anisotropy of peridotites is mainly due to the lattice preferred orientation (LPO) of olivine and to the competing effects due to the LPO of orthopyroxene. If present, well-oriented hydrous phases such as phlogopite, leads to both P- and S-waves velocities becoming drastically reduced, but the anisotropy and the S-wave splitting (mainly on the foliation plane) is increased. An attempt has been made to apply this petrologic and microstructural approach to understand the seismic properties of ultramafic rocks with the aid of a mobile seismic network set up in the Ivrea-Verbano zone. Five recording units with 3-component geophones were installed on the most representative lithologies of the Ivrea-Verbano zone: kinzigites, gabbros, stronalites, and on metapelites of the adjacent outcrop of the Serie dei Laghi. During five months the seismic network recorded 49 events that were mainly regional earthquakes. The preliminary analysis of the first arrival revealed a high-velocity anomaly near the Finero ultramafic massif. Rough calculations indicated that this anomaly could be due to a shallow-depth, peridotitic body about six kilometres thick. S-wave polarisation analysis was carried out on the horizontal components of the seismograms of four regional earthquakes that showed a first arrival propagating almost vertically at the recording sites. Four earthquakes were chosen in order to reconstruct the orientation of the polarisation plane of the shear phases. The preliminary results of this analysis have shown a qualitatively good agreement between the orientation of the polarisation plane of the fast shear-wave and the strike of the foliation at the station near Finero, located on kinzigites of the Ivrea-Verbano zone, although the relationships between the local structural setting and the polarisation orientations at the other recording sites is not yet so clear. 相似文献
997.
Gordon Kaufman 《Natural Resources Research》1994,3(4):304-314
The relative efficiencies of alternative geometric patterns of both discrete borehole and continuous grid line search have been extensively discussed in the mathematical geology literature. However, an equally important problem has received virtually no attention: How to use a sample of properties of geologic anomalies detected by grid line search of a region to estimate systematically both the number and size distribution of geologic anomalies missed by the search. We show how estimation methods developed in the sample survey design literature can be adapted to this problem, and we apply these methods to data describing 94 anomalies identified by a seismic reconnaissance survey. 相似文献
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