This volume covers the formation and biogeochemistry of a variety of important sediment types from their initial formation through their conversion (diagenesis) to sedimentary rocks. The volume deals with the chemical, mineralogical, and isotopic properties of sediments and sedimentary rocks and their use in interpreting the environment of formation and subsequent events in the history of sediments, and the nature of the ocean-atmosphere system through geological time. Reprinted individual volume from the acclaimed Treatise on Geochemistry, (10 Volume Set, ISBN 0-08-043751-6, published in 2003). Comprehensive and authoritative scope and focus Reviews from renowned scientists across a range of subjects, providing both overviews and new data, supplemented by extensive bibliographies Extensive illustrations and examples from the field
Kisch, 1966b, 1969; Kaplan, 1974); (b) the Permian Coal measures of the lower Hunter Valley, New South Wales (Kisch ... (Castano and Sparks, 1974) and Lower Cretaceous of the Great Valley sequence of Cache Creek (Dickinson et al., 1969; ...
Diagenesis in Sediments and Sedimentary Rocks, 2
Mrs. D. M. Powell helped in many ways with the organisation, and also retyped the entire manuscript of this book. A. Parker B. lv.
Diagenesis in Sediments and Sedimentary Rocks, Volume 2
Current ripples are small-scale bedforms with wavelengths of less than a few tens of centimetres and heights of less ... The shape of ripples and dunes is described as two-dimensional if the crests are straight, or three-dimensional, ...
This comprehensive, one-volume encyclopedia covers the sedimentological aspects of sediments and sedimentary rocks.
The book is intended not only for earth scientists studying sediments and sedimentary rocks, but also for researchers in fields such as radioactive waste disposal, petroleum and economic geology, environmental pollution, and sea-floor ...
This volume, although not an integrated synthesis, treats most aspects of Holocene sedimenta tion and diagenesis in the Persian Gulf, grouping 22 contributions under a single cover and in one language.
Ripples developed under unidirectional current flow are asymmetrical in cross-sectional shape, with a gently sloping upcurrent stoss side and a more steeply sloping lee side. Ripples of this type are called current ripples.
It forms in the marine environment within growth cavities and within sediment. ... Marine macrophytes (Figure 3.13c) are red, brown, and green soft non‐calcareous algae that thrive in cool‐ and cold‐water environments.