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901.
TheapplicationofultrasonicseismicmodelexperimentinqualitytestofcementmortarinjectionofYongjiangriversubmarinetun┐neltubefound... 相似文献
902.
Theideaandprojectofthe“Medium┐ScaleExperimentFieldforEarthquakePrediction”Researchonobservationsandapplicationsofminingearthq... 相似文献
903.
Zhou Shiyong Zhu LingrenSeismological Bureau of Xinjiang Uygur Autonomous Region Urumqi China 《中国地震研究》1996,(2)
During the preparation process of a great earthquake, there are certain patterns of less randomness but more order in the space-time distribution of micro-earthquakes, which had been proved by seismic events and experiments. The information entropy concerning the dimension of the order in seismic distribution is systematically defined from the point of modern statistical physics in this paper. Relations of dynamic variations of information entropy with a strong shock occurrence time and the distribution of information with a strong shock occurrence place were approached through seismic data from the Wuqia, Xikar, Wushi, and Manasi regions in Xinjiang. It is indicated that before strong earthquakes, the value of information entropy often noticeably drops in seismic region, and generally much lower in the epicentral area than the surrounding regions. These two characters are of important significance in strong shock risk region determination and large shock tendency prediction. 相似文献
904.
905.
In this paper,a test or alternative scheme for studying large earthquake sequences through the study of small earthquake sequences is suggested,and a small earthquake sequence,the Lima earthquake sequence for which analogue records have been turned into digital data,is used here.In order to provide the deep construction background and the spatial distribution of structure for generating earthquakes,the P-wave and S-wave layered velocity models in this area are obtained by using mine explosion and earthquake observed records; then,the hypocenter locations and focal depths of the Lima earthquake sequence are determined adopting the velocity models given above and using a location method with numerical properties for a microseismic monitoring network(Zhao et al.,1994)and a new method for determining focal depth from data of a local seismographic network(Zhao,1992); finally,based on this,the variation of quality factor Q of the crustal medium during the period of the sequence is estimated.The obtained resul 相似文献
906.
通过对青岗坪金矿区内发育的拆离断层系统的具体分析,揭示了其产生,发展的过程,对由其控制的几类金矿脉的形成机制进行了合理的探讨,并对不同的成矿阶段进行了划分。 相似文献
907.
908.
909.
Introduction Many earthquake cases indicate that there exists obvious heterogeneity in temporal-spatial distribution of earthquake precursors (FENG, 1983; MEI, et al, 1993). Therefore, it is very crucial for the study of earthquake prediction to describe the heterogeneity in temporal-spatial distribution of earthquake precursors and to understand its physical mechanism. Up to now, a lot of useful researches have been done in this field. Recently, WANG, et al (1999) and CHEN, et al (2000)… 相似文献
910.
利用“专家系统”的思想对每一地震前兆异常事件进行了综合评估,以每一异常的最可能发震时间计算发震概率,利用各类地震前兆异常群体信息熵研究了系统熵值与地震场,源兆的关系,分析了1976年唐山7.8级地震前各类地震前兆异常的时空分布特征,然后以唐山为中心在空间上划分三个区,近区,中间区和远区,分别计算了三个区各类地震前兆异常信息熵的时间演化值,分析了震前这种信息熵的场,源兆特征,震中近区的信息熵值要比中 相似文献