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The Surface Rupture of the 1957 Gobi-Altay, Mongolia, Earthquake 1-1-001-322-4330-322 sediment generation and transport

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Description

sediment generation and transport

and decision-makers interested in understanding earthquakes and seismic hazards in eastern North America and other intraplate settings

grounded theory

the wide range of disciplines involved

and gives readers an introduction to some of the uncertainties and controversies related to the evolution of the planet

The Surface Rupture of the 1957 Gobi-Altay, Mongolia, Earthquake 1-1-001-322-4330-322 sediment generation and transportAuthors: R. A. Kurushin, A. Bayasgalan, M. lziybat, B. Enhtuvshin, Peter Molnar, Ch. Bayarsayhan, Kenneth W. Hudnut, and Jian Lin Buy the e book (not available in print) The 1957 Gobi Altay earthquake is the last major earthquake (M ~ 8) to occur in a continental region. The full complement of processes that distinguish continental tectonics from plate tectonicsinternal deformation of blocks, conjugate faulting, variations in amounts of slip along

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