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The Persian Gulf - Holocene Carbonate Sedimentation and Diagenesis in a Shallow Epicontinental Sea (Paperback, Softcover reprint of the original 1st ed. 1973)
Loot Price: R4,535
Discovery Miles 45 350
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The Persian Gulf - Holocene Carbonate Sedimentation and Diagenesis in a Shallow Epicontinental Sea (Paperback, Softcover reprint of the original 1st ed. 1973)
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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. Because these sediments and diagenetic minerals are
comparable to those existing in many ancient sedimentary basins,
their appraisal should be of value to the enlarging group of
workers who interpret ancient sedimentary rocks. The essential
morphological, climatic and oceanographic factors determining
Holocene sedimen tation and diagenesis in the Persian Gulf are
summarized in the introductory article by PURSER and SEIBOLD. These
environmental controls and the overall morphology of the Persian
Gulf have much in common with Shark Bay, Western Australia,
described by LOGAN et al. (1970). On the other hand, the Persian
Gulf is markedly different from the better known Florida and
Bahamian prov inces; the floor of the Persian Gulf is gently
inclined from continental shoreline to bathymetric axis (80-100 m);
the Bahamian province, on the other hand, is horizontal and
extremely shallow (2-10 m), with very sharply defined shelf edges
surrounded by deep oceanic waters. These contrast ing architectural
styles are related to different tectonic frames.
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