Titlebook: Seismic Facies and Sedimentary Processes of Submarine Fans and Turbidite Systems; Paul Weimer,Martin H. Link Book 1991 Springer Science+Bu

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0939-6055 ntial to stay abreast of the most recent ideas and developments and to become familiar with certain topics in the field of sedimentary geology. This series deals with subjects that are in the forefront of both scientific and economic interests. The treatment of a subject in an individual volume, the

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Introductionnd reservoir pressure data will also add significantly to the understanding of these deep-water systems. The use of seismicstratigraphic concepts for submarine-fan deposition with outcrops has changed the interpretation of facies and their distribution in turbidite systems (Mutti, 1985; Mutti and Normark, this volume; Sgavetti, this volume).

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Global Petroleum Occurrences in Submarine Fans and Turbidite Systemsr petroleum-producing submarine fan deposits, and these reservoirs produce from a variety of structural, stratigraphic, and combined traps. To characterize these reservoir occurrences, tables were constructed for each continent and basin showing reservoir age, formation name(s), tectonic setting, an

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Introductional experiments. It is essential that this information be correctly obtained, analyzed, and well understood before making any interpretations, drawing too many conclusions, and developing forward models. Many interpretations are based on first impressions familiar to the researcher, either from perso

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An Integrated Approach to the Study of Turbidite Systemsas the limitations presented by the widely varying techniques used to map and describe the deposits. To facilitate such comparisons, we describe five basic elements of turbidite systems that, with appropriate types of field observations, can be recognized in both ancient and modern systems (i.e., in

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Models for Submarine-Fan Deposition within a Sequence-Stratigraphic Frameworkr, are considered most likely to occur and have the highest sand-to-mud ratio during lowstands of . During these intervals, depocenters shift to the outer shelf and beyond, increasing the likelihood of initiating sediment gravity flows. The stratigraphic units deposited during this time interval com