Andere Kunden interessierten sich auch für
![Underplating in the west coast of India and adjoining Dharwar craton]( "Underplating in the west coast of India and adjoining Dharwar craton")
Underplating in the west coast of India and adjoining Dharwar craton23,99 €![Geomorphological studies of the Himalayan Glaciers in brief]( "Geomorphological studies of the Himalayan Glaciers in brief")
Geomorphological studies of the Himalayan Glaciers in brief26,99 €![Estimation of the velocity vector of moving targets from SAR images]( "Estimation of the velocity vector of moving targets from SAR images")
Estimation of the velocity vector of moving targets from SAR images36,99 €![Crustal Anisotropy and Shear Wave Velocity Structure]( "Crustal Anisotropy and Shear Wave Velocity Structure")
Crustal Anisotropy and Shear Wave Velocity Structure32,99 €![Aerosol characteristics over coastal India and adjoining oceans]( "Aerosol characteristics over coastal India and adjoining oceans")
Aerosol characteristics over coastal India and adjoining oceans51,99 €![Basic Geophysical Petroleum Exploration: A High Velocity Anomaly Case]( "Basic Geophysical Petroleum Exploration: A High Velocity Anomaly Case")
Basic Geophysical Petroleum Exploration: A High Velocity Anomaly Case40,99 €![Seismicity and Attenuation Studies of Delhi and Adjoining Areas]( "Seismicity and Attenuation Studies of Delhi and Adjoining Areas")
Seismicity and Attenuation Studies of Delhi and Adjoining Areas44,99 €
Among the oldest and most fundamental problems in seismology are determining the velocity-depth relation accurately, ascertaining the nature of discontinuities within the Earth, and translating this information into knowledge of the materials that constitute the interior of the earth. The crust, which occupies the outermost shell of the Earth, has always been of great interest to seismologists. In addition, knowledge of crustal structure is a prerequisite to obtain precise information on the nature of the Earth's interior below the Moho discontinuity.The long and complex history of Himalayan seismic arc makes it a geological nexus for understanding how crust forms, evolves and survives plate tectonic processes over billions of years. The goal of this study is to characterize the crustal thickness, composition, and Moho impedance contrasts across the three segments of Himalaya strike wise; the western Himalaya, the central Himalaya and the eastern Himalaya along with its for deep region.