SEISMOLOGY AND GEOLOGY ›› 2003, Vol. 25 ›› Issue (2): 327-337.
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DENG Zhi-hui, WANG Yu, CHEN Mei-hua, TANG Fang-tou, CHU Quan-zhi, XU Hao-min
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邓志辉, 王煜, 陈梅花, 唐方头, 楚全芝, 徐好民
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Abstract: This paper is aimed at the relationship between satellite infrared anomaly and tectonic activities by analysis of anomaly images of 3 earthquake cases (M>6) occurred in 2000 in China. Yao'an earthquake (MS6.5) occurred on January 15, 2000 in Yunnan Province, southwest China. The infrared anomaly of the earthquake began 20 days before the mainshock and disappeared after the event. It developed along the Honghe Fault, which is the most important fault near the epicenter. The brightness temperature along the fault is always higher than that away from the fault during the anomalous period. The anomaly of temperature difference along the fault and away from the fault exists not only when weather temperature increases but also when it falls down. It seems that the anomaly is more active along the fault than in the other area. Jingtai earthquake (ML6.2) occurred on June 6,2000 in Gansu Province, northwest China. Satellite Infrared anomaly appeared in a peculiar geometrical pattern before the earthquake. The monthly average infrared brightness temperature increased abnormally along 3 NE-trending tectonics which intersect with the NW-trending faults. Near the epicenter, the infrared anomaly developed in "Z" configuration that seems to extend along conjugated structures. Xinghai earthquake (MS6.6) took place on Sept. 12, 2000 in east Qinghai Province, northwest China. The epicenter is located near the NNW-trending Ngola Shan Fault. Before the earthquake, the monthly average infrared brightness temperature was different on both sides of the Ngola Shan Fault and its extension. It was higher than 10℃ on the eastern side, and less then 10℃ on the western side. From the above-mentioned 3 cases, the primary conclusions can be drawn as fellows: (1) The distribution of satellite infrared anomaly is closely related to geologic structures, especially active faults; (2) The earthquake epicenter is often located at the margin of relatively high infrared temperature anomaly area or its vicinity. Infrared anomaly develops asymmetrically, propagating from one side toward the epicenter. (3) The spatial and temporal distribution of infrared anomalies may vary in different areas. In the analysis of infrared anomaly information, therefore, it is necessary to take the tectonic conditions, geographical features and meteorological interferences into consideration.
Key words: satellite infrared remote sensing, earthquake prediction, Yao’an earthquake, Jingtai earthquake, Xinghai earthquake
摘要: 通过对2000年在中国大陆发生的3个6级以上地震的卫星红外异常特征的初步分析,得到了一些有意义的结果:1)卫星红外异常的分布与地质构造,特别是活动断裂的关系密切;2)地震震中常位于红外温度的相对高值异常的边缘或附近,异常的发展具有非对称性,异常一般都是从震中附近的某一侧向震中区扩展;3)红外异常的时空分布规律在不同的地区是不同的,异常信息的提取要结合具体的构造条件、地理环境和气象因素进行分析。
关键词: 卫星红外遥感, 地震预报, 姚安地震, 景泰地震, 兴海地震
CLC Number:
P315.72
DENG Zhi-hui, WANG Yu, CHEN Mei-hua, TANG Fang-tou, CHU Quan-zhi, XU Hao-min. SATELLITE INFRARED ANOMALY OF SEVERAL STRONG EARTHQUAKES IN CHINA MAINLAND[J]. SEISMOLOGY AND GEOLOGY, 2003, 25(2): 327-337.
邓志辉, 王煜, 陈梅花, 唐方头, 楚全芝, 徐好民. 中国大陆几次强地震活动的卫星红外异常分析[J]. 地震地质, 2003, 25(2): 327-337.
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https://www.dzdz.ac.cn/EN/Y2003/V25/I2/327