By Dieter K. Fütterer (auth.), Professor Dr. Horst D. Schulz, Dr. Matthias Zabel (eds.)

ISBN-10: 3662042428

ISBN-13: 9783662042427

ISBN-10: 3662042444

ISBN-13: 9783662042441

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Transport phase of transition metals in the Amazon and Yukon rivers. Geological Society of America Bulletin, 88: 829-843. Gingeie, F, 1992. Zur Klimaabhängigen Bildung biogener und terrigener Sedimente und ihre Veränderungen durch die Frühdiagnese im zentralen und östlichen Südatlantic. Berichte, Fachbereich Geowissenschaften, Universität Bremen, 85, 202 pp. D. , 1970. The sediments of the northern Indian Ocean. Deep-Sea Research, 17: 513-537. , 1996. The atmospheric transport of particles in the ocean.

Academic Press, London, NY, San Francisco, pp 137-215. , 1968. Relict sediments on continental shelves of the world. Bull. Am. Assoc. Petro!. Geologists, 52: 445464. , 1995. Erosion, sedimentation and sedimentary origin of clays. In: Velde, B. (ed) Origin and mineralogy of clays. Springer Verlag, Berlin, Heidelberg, NY, pp 162219. , 1934. Size frequency distribution of sediments. Journal of Sediment Petrology, 4: 65-77. c. , 1965. An introduction to statistical models in Geology. McGraw-Hill, NY, 328 pp.

Their mode of transport into the area of deposition - either by eolian or volcanic transport, or by means of water and ice - and finally the route of transportation (Petschick et al. 1996). In aglobai survey, it is easy to identify the particular interactions which c1imate, weathering on the continents, wind patterns, riverine transport, and oceanic currents have with regard to the relative distribution of the relevant groups of c1ay minerals (kaolinite, illite, smectite, and chlorite). The distribution of kaolinite in marine sediments (Fig.

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Marine Geochemistry by Dieter K. Fütterer (auth.), Professor Dr. Horst D. Schulz, Dr. Matthias Zabel (eds.)


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