Includes bibliographical references and index.
|Statement||edited by M.S. Stoker, D. Evans, and A. Cramp.|
|Series||Geological Society special publication ;, no. 129|
|Contributions||Stoker, M. S., Evans, D. 1949-, Cramp, A.|
|LC Classifications||QE39 .G396 1998|
|The Physical Object|
|Pagination||355 p. :|
|Number of Pages||355|
|LC Control Number||99202490|
This, in turn, has led to greatly improved geological, geodynamic and numerical models for the crustal and mantle processes involved in continental-margin formation from the initial stages of rifting through to continental rupture and break-up, to the eventual development of a new ocean basin. Buy Sedimentary Basins and Crustal Processes at Continental Margins: From Modern Hyper-Extended Margins to Deformed Ancient Analogues (Geological Society Special Publications) on sinoppazari.com FREE SHIPPING on qualified ordersCited by: The continental margins of the world constitute the most impressive and largest physiographic feature of the earth's surface, and one of fundamentally great geological significance. Continental margins have been the subject of increasing attention in recent years, an interest focused by a body of. Abstract This book, edited by M.S. Stoker, D. Evans and A. Cramp, includes a number of papers considering the whole system of sedimentation on continental margins. The presented papers are based on results from the examination of gravity, piston and shallow drilling cores, as well as interpretation of multichannel and high-resolution seismic.
Geological Controls for Gas Hydrates and Unconventionals. Book • Authors: followed by an explanation of the evolution of continental margins with the focus on convergent and divergent margins. Finally complex structural configurations including sedimentary and volcanic processes of convergent margins together with deep-sea trenches. Apr 01, · Geological Processes on Continental Margins: Sedimentation, Mass-Wasting and Stability Leitchenkov, G.L This book, edited by M.S. Stoker, D. Evans and A. Cramp, includes a number of papers considering the whole system of sedimentation on continental margins. The presented papers are based on results from the examination of. Sedimentary Basins and Crustal Processes at Continental Margins: From Modern Hyper-extended Margins to Deformed Ancient Analogues has led to greatly improved geological, geodynamic and numerical models for the crustal and mantle processes involved in continental margin formation from the initial stages of rifting through continental rupture. An orogeny is an event that leads to both structural deformation and compositional differentiation of the Earth's lithosphere (crust and uppermost mantle) at convergent plate sinoppazari.com orogen or orogenic belt develops when a continental plate crumples and is pushed upwards to form one or more mountain ranges; this involves a series of geological processes collectively called orogenesis.
Geological processes on continental margins: sedimentation, mass-wasting and stability: an introduction • Large submarine slides at the NE Faeroe continental margin •Turbidite flux, architecture and chemostratigraphy of the Herodotus Basin, Levantine Sea, SE Mediterranean • Sediment delivery to the Gulf of Alaska: source mechanisms along. continental margin The broad, gentle pitch of the continental shelf gives way to the relatively steep continental slope. The more gradual transition to the abyssal plain is a sediment-filled region called the continental rise. The continental shelf, slope, and rise are collectively called the continental margin. Encyclopædia Britannica, Inc. The continental margin is one of the three major zones of the ocean floor, the other two being deep-ocean basins and mid-ocean sinoppazari.com continental margin is the shallow water area found in proximity to continent. The continental margin consists of three different features: the continental rise, the continental slope, and the continental shelf. The development of an understanding of large-scale processes requires an integrated approach. This book explores the current cutting-edge interdisciplinary research in lithospheric rheology and provides a broad summary of the rheology and deformation of the continental lithosphere in both extensional and compressional settings.