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Titlebook: Geochemistry and Sedimentology of the Mediterranean Sea; E. M. Emelyanov,K. M. Shimkus Book 1986 Springer Science+Business Media Dordrecht

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书目名称Geochemistry and Sedimentology of the Mediterranean Sea
编辑E. M. Emelyanov,K. M. Shimkus
视频video
丛书名称Sedimentology and Petroleum Geology
图书封面Titlebook: Geochemistry and Sedimentology of the Mediterranean Sea;  E. M. Emelyanov,K. M. Shimkus Book 1986 Springer Science+Business Media Dordrecht
描述The monograph presented to foreign readers has been prepared by the famous Soviet investigators of processes of geochemistry and sedimentation in the Mediterranean Sea. For more than 20 years E.M. Emelyanov has examined the recent sedimentation of the Mediterranean Sea and K.M. Shimkus has studied the Quaternary and the earlier sedi­ mentation of the area. The authors, scientific workers from the P.P. Shirshov Institute of Oceanology, USSR Academy of Sciences (Atlantic and Southern Depart­ ments), took part not only in numerous cruises on oceanographic vessels of the USSR, but in the study of cores of the deep-sea drilling on R/V "Glomar Challenger". A great number of scientific papers and some books devoted to the processes of sedimentation and geochemistry of the Mediterranean Sea were written by them. Although the scientific interests of the authors are not only limited to these questions, I should like to emphasise these aspects of their scientific activity when introducing this book. The Mediterranean Sea is a suitable natural laboratory for solving a number of principal problems of marine sedimentation and lithogenesis.
出版日期Book 1986
关键词Sediment; Sedimentation; diagenesis; geochemistry; sedimentology
版次1
doihttps://doi.org/10.1007/978-94-009-4490-9
isbn_softcover978-94-010-8500-7
isbn_ebook978-94-009-4490-9
copyrightSpringer Science+Business Media Dordrecht 1986
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Die Innungen, wie sie sich gestalten müssen but in other cases they are diluted. The transformation begins on the land when the denudation products are beginning to be transformed, continues in rivers and in the final basins of deposition (whilst in the water and on the sea floor), i.e. until the sediment reach a physical-chemical condition
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https://doi.org/10.1007/978-3-662-26199-6r (5°30′W) along the 38th parallel is about 3800 km (Fig. 1). The width of the Mediterranean Sea from the Bay of Sirte in the south (30°30′N) to the Adriatic Sea near Trieste in the north is about 1800 km.
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The Geochemistry of the Recent Sediments,r (5°30′W) along the 38th parallel is about 3800 km (Fig. 1). The width of the Mediterranean Sea from the Bay of Sirte in the south (30°30′N) to the Adriatic Sea near Trieste in the north is about 1800 km.
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The Geochemistry of the Recent Sediments,r (5°30′W) along the 38th parallel is about 3800 km (Fig. 1). The width of the Mediterranean Sea from the Bay of Sirte in the south (30°30′N) to the Adriatic Sea near Trieste in the north is about 1800 km.
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