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首页> 外文期刊>Journal of the Geological Society of India >Seismic velocities and crustal structure beneath the Shillong Plateau, Mikir Hills and Naga Thrust zone in Northeastern India
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Seismic velocities and crustal structure beneath the Shillong Plateau, Mikir Hills and Naga Thrust zone in Northeastern India

机译:印度东北部西隆高原,米基尔山丘和纳迦冲断带以下的地震速度和地壳结构

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摘要

A study of travel times for the P-g, P-* and P-n waves is conducted selecting three traverses over the Shillong Plateau, Mikir Hills and Naga Thrust zone respectively in the Northeast India region. Seismic velocities and thickness of the upper crust, lower crust and depth to the Moho are estimated. These traverses are selected through the location of the maximum number of seismic stations and the epicentres of the earthquakes in the study area. About 136 earthquakes, with magnitude range 2.0-5.0 and depth range 5-30 km, recorded during the period 1986-1999 are used. The P-g, P* and P. velocities (km/sec) are estimated to be 6.04-6.21, 6.51-6.62 and 8.47-8.65 respectively in the region. The corresponding thickness (km) of the upper crust, lower crust and depth of the Moho are 16-19, 27-30 and 40-50, respectively. The presence of high P. wave velocity (8.47-8.65 km/sec) in the region is possibly representing a colder and denser lithosphere.
机译:对印度东北地区西隆高原,米其尔山丘和纳加推力带的三个横断面分别进行了研究,研究了P-g,P- *和P-n波的传播时间。估计了地壳上部,下部地壳的地震速度和厚度以及到莫霍面的深度。这些横移是通过最大地震台数的位置和研究区域地震的震中来选择的。使用了1986-1999年期间记录的大约136次地震,震级范围为2.0-5.0,深度范围为5-30 km。该区域的P-g,P *和P.速度(公里/秒)估计分别为6.04-6.21、6.51-6.62和8.47-8.65。莫霍面的上地壳,下地壳和深度的相应厚度(km)分别为16-19、27-30和40-50。该地区高波速(8.47-8.65 km / sec)的存在可能表示岩石圈更冷更密。

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