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Neritic Sedimentary Facies

2010
Understanding this vast depositional realm has been a protracted study. As each new sector of the continental margin was documented, the new findings necessitated re-evaluation of previous interpretations. This chapter is the result of a total re-study of all bottom samples acquired since 1989 and their placement in a facies scheme that is applicable ...
Noel P. James, Yvonne Bone
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Sedimentary facies of iron formation

Economic Geology, 1954
Discussion of conclusions relative to the intensity and duration of chemical weathering during the Precambrian contained in a paper on the origin of the iron formations of the Lake Superior district; points out that lateritic iron ores locally more than 100 meters thick are being formed at present by chemical weathering processes in the Conakry ...
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Sedimentary facies associations within subduction complexes

Geological Society, London, Special Publications, 1982
Summary Sedimentation patterns within modern subduction zones are complex and variable, and do not necessarily follow models of submarine fan sedimentation. Environmental reconstructions within ancient subduction complexes should follow modern analogues as closely as possible and consider several criteria, including turbidite facies ...
Michael B. Underwood, Steven B. Bachman
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Sedimentary Facies in Gulf Coast

AAPG Bulletin, 1949
The Gulf Coast of Texas and Louisiana belongs to a world community of Tertiary provinces that have been extensively drilled for oil, and in which the sedimentary characteristics of the producing formations are similar to the characteristics of modern sediments in the same regions to-day.
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Tide-influenced sedimentary environments and facies

Marine Geology, 1988
This volume contains examples of recent as well as fossil tide-influenced sedimentary facies. Studies of recent tidal processes and sediments provide an insight into the way in which tidal facies and sequences develop, and into the processes which are active.
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Sedimentary Facies Model of Turbidites: ABSTRACT

AAPG Bulletin, 1963
Deposits of turbidity currents are characterized by alternating layers of sandstone and shale, in which a unit layer is defined as the sandstone together with its overlying shale. Studies of turbidites of different ages, and from many different localities in Europe, make it clear that turbidites are characterized by one sedimentary facies model, which ...
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Facies Associations of Riphean Sedimentary Sequences

Lithology and Mineral Resources, 2002
Large-scale facies associations typical of intra- and pericratonic Riphean sections of the Volga–Ural region, western slope of the Urals, Timan–Pechora region, Kola Peninsula, outer and inner parts of the Siberian, North American, and Indian platforms are considered.
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