Includes bibliographical references and index.
|Statement||edited by B.C. Storey, T. Alabaster, R.J. Pankhurst.|
|Series||Geological Society special publication ;, no. 68|
|Contributions||Storey, Bryan C., Alabaster, T., Pankhurst, R. J.|
|LC Classifications||QE461 .M21758 1992|
|The Physical Object|
|Pagination||vi, 404 p. :|
|Number of Pages||404|
|ISBN 10||0903317834, 0903317796|
|LC Control Number||2002491538|
Electronic book Congrès: Additional Physical Format: Print version: Magmatism and the causes of continental break-up. London ; Salem, MA: Geological Society, (DLC) (OCoLC) Material Type: Document, Internet resource: Document Type: Internet Resource, Computer File: All Authors / Contributors: Bryan C Storey; T. The first section of the volume is concerned mainly with models of magma generation and breakup processes. Critical to the debate is the origin of the large continental flood basalt provinces and the difficult task of interpreting geochemical signatures. The remaining sections present examples from the geological record. They provide essential feedback to the models and it is clear that some. Download PDF: Sorry, we are unable to provide the full text but you may find it at the following location(s): (external link)Author: PHILIP LEAT. A two-day meeting of the Tectonic Studies Group was held in London at the Geological Society on October , to consider relationships between continental extension, super continent break-up, magmatism and mantle plumes. The approach was multidisciplinary, with contributions from geophysists, geochemists and tectonic geologists.
Magmatism and the causes of continental break-up. PHILIP LEAT. Journal of the Geological Society, , , 1 July , Add to Cart ($35) PHILIP LEAT. British Antarctic Survey, NERC, High Cross, Madingley Road, Cambridge, CB3 0ET, UK. Find this author on Google Scholar. adshelp[at] The ADS is operated by the Smithsonian Astrophysical Observatory under NASA Cooperative Agreement NNX16AC86A. This book brings together articles that explore the role of magmatism in rifting, from the initiation of continental break-up through to full seafloor spreading. We also explore the hazards related to rifting and the associated volcanism. continental break-up related magmatic activity recorded by basalt flows, magmatic underplates, and intrusive complexes. Drilling of the volcanic complexes and nearby sedimentary basins may provide important new insight into mantle melting processes and how magmatism may have caused rapid climate change in the earliest Eocene.
A source of sufficiently large renewable extensional stress to cause lithospheric failure is the hot, low-density upper mantle of the type associated with a plume. Widespread extensional stress may also result from subduction on opposite sides of a large continental plate. Volcanism and continental break-up: a global compilation of large igneous provinces T. and Pankhurst, R.J. (eds.) Magmatism and the causes of continental break-up. (Geological Society Special Publication, 68) London, UK. Geological Society of London, pp. Record type: Book Section Full text not available from this repository. More. Magmatism and deformation during continental breakup. The break-up of continent s and conductive heat loss from the upwelling mantle causes the amount of melt generated beneath a rift to. EPSL ELSEVIER Earth and Planetary Science Letters () Magmatism and continental break-up in the South Atlantic: high precision 40Ar-'9Ar geochronology Simon Turner a, Marcel Regelous a, Simon Kelley a, Chris Hawkesworth a, Marta Mantovani b Department of Earth Sciences, The Open University, Milton Keynes MK7 69A, UK 6 Departamento de Geofisico, Instituto .