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Non-Volcanic Rifting of Continental Margins: A Comparison of Evidence from Land and Sea (Geological Society Special Publication Number 187)
 
 
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Non-Volcanic Rifting of Continental Margins: A Comparison of Evidence from Land and Sea (Geological Society Special Publication Number 187) [Hardcover]

R. C. L. Wilson (Author, Editor), R. B. Whitmarsh (Editor), B. Tayor (Editor), N. Froitzheim (Editor)

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Book Description

January 1, 2002 Geological Society Special Publication Number 187
Non-volcanic continental margins may form up to 30% of all present-day passive margins, and remnants of them are preserved in mountain belts. The papers in this volume demonstrate the benefits of integrating offshore and onshore studies, and illustrate the range of information obtained at different scales when comparing evidence from land and sea. Data sets collected across a range of spatial scales are evaluated: thin sections, cores, outcrops, seismic reflection profiles, and other geophysical data. The outcrop scale is crucial because it enables the spatial gulf to be bridged between DSDP and ODP cores and marine seismic data. There is also the problem that basins on land and beneath the sea inevitably have had different post-rift histories resulting in their contrasting present-day elevation. In mountain belts, portions of continental margins and oceanic crust are superbly exposed, but dismembered by subsequent compressional tectonics. Of present-day passive margins, extensional features have only been slightly deformed, if at all, by compressional movements, but are buried beneath significant thicknesses of post-rift sediments and so can only be sampled by ocean drilling at a small number of points.

The first paper reviews the synergies that have occurred between investigations of the eastern North Atlantic non-volcanic margins and remnants of similar Mesozoic margins preserved in the Alps, and some later papers return to this theme. However, papers describing margins from other parts of the world show that it may be premature to use models based on the Atlantic and the Alps as the paradigm for all non-volcanic margins. The following 25 papers in the book are grouped under the following headings: (1) Margin overviews; (2) Exhumed crust and mantle; (3) Tectonics and stratigraphy; and (4) Numerical models of extension and magmatism.

Readership: Geologists, geophysicists, geochemists, oceanographers, petroleum explorationists.

Also available:

The Gregory Rift Valley and Neogene-Recent Volcanoes of Northern Tanzania - Memoir no 33 - ISBN 1862392676
Permo-carboniferous Magmatism And Rifting in Europe (Geological Society Special Publication) - ISBN 1862391521

The Geological Society of London

Founded in 1807, the Geological Society of London is the oldest geological society in the world, and one of the largest publishers in the Earth sciences.

The Society publishes a wide range of high-quality peer-reviewed titles for academics and professionals working in the geosciences, and enjoys an enviable international reputation for the quality of its work.

The many areas in which we publish in include:

-Petroleum geology
-Tectonics, structural geology and geodynamics
-Stratigraphy, sedimentology and paleontology
-Volcanology, magmatic studies and geochemistry
-Remote sensing
-History of geology
-Regional geology guides


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Inside This Book (learn more)
First Sentence:
Twenty years after the discovery by dredging of the peridotite ridge bounding the Galicia margin (Boillot et al. 1980; Sibuet et al. 1987), and after three Ocean Drilling Program (ODP) Legs (103, 149, 173; Fig. 1), three French diving cruises, and several British, German, US and French geophysical surveys on the West Iberia margin, the advance in the understanding of processes controlling continental break-up and the onset of sea-floor spreading appears to be spectacular, and many of the major problems seem to be solved. Read the first page
Key Phrases - Statistically Improbable Phrases (SIPs): (learn more)
yield stress, border fault, fresh peridotite, exhumed mantle rocks, rift duration, mean apparent age, peridotite ridge, serpentinite zone, ultramafic sea floor, continentward dipping reflectors, related rock emplacement, total crustal extension, mantle weakness, tinized mantle, serpentinite unit, exhumed subcontinental mantle, initial lithospheric structure, peridotite section, cia margin, fallout tephra layers, amagmatic rifting, border fault system, extensional allochthons, extinct spreading axis, magnetic anomaly chart
Key Phrases - Capitalized Phrases (CAPs): (learn more)
Iberia Abyssal Plain, Ocean Drilling Program, Journal of Geophysical Research, College Station, Geological Society, West Iberia, Woodlark Basin, Special Publications, Scientific Results, Red Sea, Papua New Guinea, West Greenland, South China Sea, Labrador Sea, Gulf of Suez, Initial Reports, Hobby High, Moresby Seamount, Shipboard Scientific Party, Woodlark Rift, Southern Alps, Galicia Bank, South Alpine, American Geophysical Union, Comparison of Evidence
Browse Sample Pages:
Front Cover | Table of Contents | First Pages | Index | Back Cover | Surprise Me!
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