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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

their contributions provide illustrative examples of the applicability of geochemical techniques to paleoclimatology by exploring theoretical and practical frameworks used to analyze and interpret isotopic and elemental data from marine and terrestrial materials

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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