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Table of Content

    02 December 1987, Volume 9 Issue 4
    Brief Report
    SYMPOSIUM ON GEOLOGY AND SEISMOLOGY OF TAIWAN STRAIT AND OF ITS BOTH COASTS HELD IN FUZHOU
    Yao Yan-zhi
    1987, 9(4):  18-18. 
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    DYNAMIC VARIATION OF COMPOSITE FAULT PLANE SOLUTION OF SMALL EARTHQUAKES IN THE NORTH CHINA
    Jin Ya-min, Yu Xin-chang
    1987, 9(4):  19-31. 
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    Based on the first motion data of more than 4000 small earthquakes from 115 seismic station, the stress fields of small earthquakes in the North China were determined by the method by which compositive fault plane solution is solved from first motion data of p wave. It is suggested that on the same seism otectonic zone, the directions of principal compressional stress of fault plane solution of small earthquakes are consistent. Before and after a large earthquake, regional stress field may change. The dynamic variation characteristics of stress field of small earthquakes before Heze 5.9 earthquake of 1981 were analysed. It is suggested that regional stress field variation with the occurrence of large earthquakes is the base for forming complicated and multi-level seismic activity. Finally, the stress field characteristics of the North China and the areas with high stress background are discussed.
    ANALYSIS OF PRESENT STRESS STATE IN FANGSHAN GRANODIORITE MASS AND ITS SURROUNDINGS IN BEIJING
    Liang Hai-qing, Zhai Qing-shan, Li Fang-quan
    1987, 9(4):  32-40. 
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    According to an analysis of in-situ stress measurements, on the whole, activity of general NE-trending Babaoshan, Huang zhuang and Gaoliying fault zone is considered as clockwise torsion Characters of in-situ stress state on different segments of the fault zone differ from main directions of the maximum horizontal compressive stresses in the Beijing-Tianjin-Tangshan area. General NE-trending fault zone shows tensile antitorsion components from the additional stress state calculated by stress principle of stress superposition of elastic theory. The fault segments in Dahuichang and Niukouyu zones have the same character as well. The stress state in this region is still considered as one in adjusment period after the major Tangshan earthquake. It seems that the stress state determined in deeper crust is affected by the tectonic activities too.
    5TH INTERNATIONAL SPECIALIST SEMINAR ON THERMOLUMINESCENCE AND ELECTRON-SPIN-RESONANCE DATING, 5-10 JULY, 1987, CAMBRIDGE, ENGIAND
    Lu Yan-chon
    1987, 9(4):  40-40. 
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    2TH SYMPOSIUM ON TECTONOPHYSICS HELD IN WUDU, GANSU PROVINCE
    Hong Han-jing
    1987, 9(4):  48-48. 
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    DISCUSSION ON GENESIS OF RECENT LONGWAN- SHANGYUKOU FRACTURE ZONE IN HANCHENG COUNTY, SHAANXI PROVINCE
    Zhang An-liang, Mi Feng-shou
    1987, 9(4):  55-61. 
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    This paper gives a detailed description about a series of appearances of modern fracture deformation found in Paleozoic strata at Xishan Hill, Hancheng, Shaanxi. It is thought that they are at a special tectonic and geomorphic locality and result from gravitation under the condition of human activities (mining), and that there is not enough evidence that these appearances are the traces of prehistorical large earthquakes.
    12TH INQUA CONGRESS, 31 JULY-9 AUGUST, 1987, OTTAWA, CANADA
    Lu Yan-chou
    1987, 9(4):  61-61. 
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    INTERNATIONAL SYMPOSIUM ON TECTONIC EVOLUTION AND DYNAMICS OF CONTINENTAL LITHOSPHERE-THE THIRD ALL CHINA CONTERENCE ON TECTONICS, 24-28, AUGUST, 1987, BEIJING
    Wang Xiao-yuan
    1987, 9(4):  62-62. 
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    TWO-PHASE DEFORMATION IN THE FAULT ZONE AND RELATED EARTHQUAKE GENERATION
    Zhang Jia-sheng
    1987, 9(4):  63-70. 
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    Five kinds of fault rocks and thier structures concerned have been discribed respectively along the Tancheng-Lujiang fault zone at the recent erosion surface. It is clear that the two-phase deformation on the sence of mechanics commonly in various scales, in which both brittle and ductile deformation components are presented through faulting. On the basis of these inverstigations, a model for earthquake generation in the large fault zone has been discussed.
    ANALYSIS OF OBSERVING DATA FOR SEISMIC SOURCE DYNAMIC FROM EARTH'S ROTATION IN EAST ASIA CONTINENT
    An Ou
    1987, 9(4):  71-80. 
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    The active belt strikes, mobile fashions, source principal compressive stress directions, total shift directions, distribution along latitudes and change along with the time of large earthquakes in East Asia continent all correlate to the speed change of earth's rotation The initial two years in the increasing speed of earth's rotation are the active periods of EW and SN striking earthquake belts, principal compressive stress directions in this region are in NW quadrant and earthquakes shift totally from NW to SE in these periods, after these are active periods of NE and NW striking earthquake belts, principal compressive stress directions in this region are about in 90°angles near EW and earthquakes shift totally from W to E; the times on uniform speed of earth's rotation are active periods of NE and NW striking earthquake belts, principal compressive stress directions in this region are in 90°angles near SN and earthquakes shift totally from N to S; the initial two years in the decreasing speed of earth's rotation are the active periods of NNE and WNW striking earthquake belts, principal compressive stress directions in this region are in NE quadrant and earthquakes shift totally from NE to SW in these periods, the times after these are active periods of NE and NW striking earthquake belts, principal compressive stress directions in this region are about in 90°angles near EW and earthquakes shift totally from E to W. The most places of M≥7 earthquake frequency along latitudes are at N42°. The earthquakes decrease during increasing speed of earth's rotation and the earthquakes increase during decreasing speed of earth's rotation. The earthquakes happening during lower speed of earth's rotation are more than during higher speed of earth's rotation.

    JOINT INTERPRETATION OF THE APPARENT RESISTIVITIES AND IMPEDANCE PHASES FROM MAGNETOTELLURIC DATA
    Jin Guang-wen
    1987, 9(4):  81-86. 
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    This paper deals with the principles of computation method for joint interpretation of the apparent resistivities and impedance phases from magnetotelluric data. Analysis of concrete actual examples indicates that the method is correct and effective. This method is more predominant in respect of reducing solutions than is inversion method for pure apparent resistivity data or impedance phase data.

    MULTI-ADDRESS DIGITAL WATER-TABLE REMOTE SYSTEM (SSY-1)
    Wang Ke-ren, Wang Li-yun
    1987, 9(4):  87-94. 
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    Multi-address digital water-potential remote system(SSY-l)and digital water-potential recorder(SSJ-l) have been made recently. The system consists of the sensor and digital water-potential instrument of observation. This paper describes the principle and the components of the system and also presents the design and the results of the observations. Such problems as accurancy, error analyses and interference rejecting transmission usually lying in many conventional system are discussed as well.A new sensor and a decode circuit have been designed, following above analyses and discussions.Viewed from the data obtained from observations for one or two years, the idea of the design proved to be correct and useful. This can be extended to other detection and remote system of low variation.
    SYMPOSIUM ON ENTROPY AND INTERDISCIPLINARY SCIENCES HELD IN URUMQI
    Yao Yan-zhi
    1987, 9(4):  94-94. 
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