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Microfacies of Carbonate Rocks - Analysis, Interpretation and Application (with CD-ROM)
Flügel, Erik
Springer
2004
Hardcover with CD-ROM XIX, 976 pp, 330 illus and 151 plates ISBN 354022016X
£77.00
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The book provides a synthesis of the methods used in microfacies analysis, the potential
of microfacies in evaluating depositional environments and diagenetic history, and the
application of microfacies data in the study of carbonate hydrocarbon reservoirs and
the provenance of archaeological materials. The first part of the book (Microfacies Analysis)
deals with field and laboratory methods; the description and significance of microfacies data;
quantitative microfacies analysis; diagenetic processes and diagenetic products; common
textural limestone classifications and specific classifications for reef limestones, non-marine
carbonates, recrystallized limestones and mixed carbonate-siliciclastic rocks; biological
controls of carbonate sedimentation; and fossils in thin section. The second part (Microfacies
Interpretation) is focused on the methods of making of microfacies types; diagonsotic
criteria of palaeoenvironmental conditons and processes; the importance of integrated
facies analysis including mineralogical and geochemical data; the definition of depositional
facies models, facies zones and standard microfacies types, and the recognition of
depositional constraints influencing cyclic carbonates, reef limestones, cold-water carbonates,
vent and seep carbonates and mixed carbonate-siliciclastic rocks. The last chapter deals
with secular variations of facies features. The third part of the book (Practical Use of
Microfacies) underlines the facies controls of reservoir and host rocks, the importance
of microfacies and diagenesis for understanding technological properties of carbonate
rocks and the destruction and conservation of carbonate objects, and discusses the
potential of microfacies for archaeometrical studies. Nearly 230 instructive plates
(30 in color)showing thin-section photographs with detailed explanations form a
central part of the content.
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Springer
: Summer 2004
: geology
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