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Surface manifestations after the Gujarat earthquake

机译:古吉拉特邦地震后的地表表现

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Once again the myth about the Indian shield as a stable shield shattered the Indian geoscientific community after the Gujarat earthquake of January 2001. This earthquake occurred far from the edge of the Indian Plate and quite close to the M_s = 7.5 earthquake that occurred in 1819. The Gujarat earthquake caused severe damage and killed tens of thousands and left many more homeless. The Gujarat earthquake of 26 January 2001 generated intense shaking which was felt at about 70 percent of the region of India. The intense shaking brought out changes in the ocean and land surface. Singh et al. have found significant changes in ocean parameters (chlorophyll and suspended sediment concentrations) after the earthquake. The present communication discusses the changes on land surface revealed from IRS-ID LISS-III remote sensing data. IRS-ID, LISS-III digital data of numerous scenes prior and after the earthquake have been acquired from National Remote Sensing Agency, Hyderabad. Digital analyses of remote sensing data along various paths and rows have been carried out. The maximum surface manifestations have been found in the scene covered by row 90 and path 55, which was taken from detailed surface features extraction. The digital remote sensing data prior (4 January 2001) and after (29 January 2001) the earthquake were geo-referenced using topo-sheets and with the help of ground control points observed in the field using handy Global Positioning System (GPS). The FCC image of bands 4,2,1 prior and after the earthquake is shown in Figures 1 a and b, respectively. The comparison of two images shows significant surface manifestations. The band ratio of the two data sets (prior and after earth-quakes) has been carried out. The band ratio image is shown in Figure 1 c. The band ratio image of band 4 (Figure 1 c) clearly brought out changes in surface features after the earthquake of 26 January 2001. Prominent surface manifestations, paleo-channel and water bodies are clearly seen in and around Rann of Kutch. The area where these manifestations are seen is covered by saline soil, which looks brighter in both the images (Figures I a and b).
机译:在2001年1月古吉拉特邦地震后,有关印度盾构作为稳定盾构的神话再次粉碎了印度地球科学界。该地震发生在远离印度板块边缘的地方,非常接近1819年发生的M_s = 7.5地震。古吉拉特邦地震造成了严重破坏,并造成数万人死亡,并使更多人无家可归。 2001年1月26日的古吉拉特邦地震造成强烈震动,这种震动在印度地区的70%左右。剧烈的晃动使海洋和陆地表面发生了变化。辛格等。发现地震后海洋参数(叶绿素和悬浮沉积物浓度)发生了显着变化。本来文讨论了从IRS-ID LISS-III遥感数据揭示的陆地表面变化。从海得拉巴国家遥感局获得了地震前后许多场景的IRS-ID,LISS-III数字数据。已对沿各种路径和行进行的遥感数据进行了数字分析。在由行90和路径55覆盖的场景中找到了最大的表面表现,该场景取自详细的表面特征提取。使用地形表对地震之前(2001年1月4日)和之后(2001年1月29日)的数字遥感数据进行地理参考,并借助方便的全球定位系统(GPS)在现场观察到的地面控制点进行了参考。图1a和b分别显示了地震之前和之后的频带4、2、1的FCC图像。两个图像的比较显示出明显的表面表现。已经执行了两个数据集(地震之前和之后)的频带比率。带宽比图像如图1c所示。在2001年1月26日地震后,频带4的频带比率图像(图1c)清楚地显示了地表特征的变化。在库奇兰(Rann)周围及其周围,清晰可见明显的地表表现,古河道和水体。看到这些表现的区域被盐渍土覆盖,在两个图像中看起来都更亮(图1a和b)​​。

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