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The present study investigates the factors associated with the occurrence of landslides along with the National Highway (NH
39) connecting Assam-Manipur (India) to Myanmar. Kinematics and slope stability analyses were used to gain an understanding
of the causes of slope failure despite the terrain comprising material with a high safety factor. The study area falls within
a high seismic zone along the regional Churachandpur-Mao Thrust (CMT) situated west of the Indo-Myanmar subduction zone. Based
on these studies of seismicity, slip rates, creeping, among others, it was inferred that CMT is a creeping regional fault
running parallel to the subduction zone boundary creeping segment of CMT and that the CMT requires further monitoring to assess
the landslide hazard in the region. 相似文献
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Arun Kumar Manichandra Sanoujam L. Someshwar Roy L. Kosigyn W. Arun Kumar Singh Ajeet P. Pandey 《Journal of the Geological Society of India》2016,87(1):5-34
Late Maastrichtian through middle Eocene planktic foraminiferal biostratigraphy and erosion patterns from three Cauvery basin wells are compared with the Krishna-Godavari basin, Madagascar and South Atlantic Site 525A. Maastrichtian sedimentation appears continuous at DSDP site 525A and substantially complete in the Cauvery basin and Madagascar for the interval from ~70.3 to 66.8 Ma (zones CF6-CF3). But the latest Maastrichtian through early Paleocene record is fragmented, except for some Krishna-Godavari and Cauvery basin wells protected from erosion by Deccan traps or graben deposition, respectively. Hiatuses are observed correlative with sea level falls at 66.8, 66.25, 66.10, 65.7, 63.8 and 61.2 Ma with erosion amplified by local tectonic activity including doming and uplift due to Deccan volcanism. 相似文献
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