http://www.loc.gov/mods/v3 http://www.loc.gov/standards/mods/v3/mods-3-2.xsd
the organic cyclicities of the Kimmeridge Clay Formation (Yorkshire, GB) and the recent maar sediments (Lac du Bouchet, France)
1 online resource (viii, 187 pages) : illustrations (some color).
The accumulation of organic matter allows inferences about a wide selection of processes in the geological past. The Kimmeridge Clay Formation (Yorkshire, U.K.) can be regarded as a model of the formation of hydrocarbon source rocks. The driving force of organic matter accumulation is the organic phytoplankton productivity, whereas oxygenation conditions seem to have played a secondary role. In Lake Bouchet (French Massif Central) organic matter appears to be a good indicator of paleoenvironmental changes occurring for over 350000 years. The book is of special interest to geologists and geochemists interested in organic matter accumulation.
[edited by] Elisabeth Lallier-Vergès, Nicolas-Pierre Tribovillard, Philippe Bertrand.
Master and use copy. Digital master created according to Benchmark for Faithful Digital Reproductions of Monographs and Serials, Version 1. Digital Library Federation, December 2002. http://purl.oclc.org/DLF/benchrepro0212 MiAaHDL
digitized 2010 HathiTrust Digital Library committed to preserve pda MiAaHDL
Includes bibliographical references and index.
Organic matter accumulation : the organic cyclicities of the Kimmeridge Clay Formation (Yorkshire, GB) and the recent maar sediments (Lac du Bouchet, France)