Download Cretaceous-Tertiary High-Latitude Palaeoenvironments: James by D. Pirrie, J. A. Crame, Editors J. E. Francis PDF

By D. Pirrie, J. A. Crame, Editors J. E. Francis

High-latitude settings are delicate to climatically pushed palaeoenvironmental swap and the consequent biotic reaction. weather switch during the top period of Cretaceous heat, overdue Cretaceous cooling, onset and enlargement of the Antarctic ice sheet, and therefore the range of Neogene glaciation, are all recorded in the sedimentary and volcanic successions uncovered in the James Ross Basin, Antarctica. This website offers the longest onshore checklist of Cretaceous-Tertiary sedimentary and volcanic rocks in Antarctica and is a key reference part for Cretaceous-Tertiary worldwide switch. The sedimentary succession is richly fossiliferous, yielding assorted invertebrate, vertebrate and plant fossil assemblages, permitting the reconstruction of either terrestrial and marine structures. The papers inside of this quantity offer an summary of modern advances within the realizing of palaeoenvironmental switch spanning the mid-Cretaceous to the Neogene of the James Ross Basin and similar biotic switch, and should be of curiosity to many engaged on Cretaceous and Tertiary palaeoenvironmental change.Also to be had: The Neuquen Basin, Argentina: A Case examine in series Stratigraphy and Basin Dynamics - ISBN 1862391904 Terrane approaches on the Margins of Gondwana - ISBN 1862391793The Palynology And Micropalaeontology of limitations - ISBN 1862391602

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Read Online or Download Cretaceous-Tertiary High-Latitude Palaeoenvironments: James Ross Basin, Antarctica - Special Publication no. 258 (Geological Society Special Publication) PDF

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A quantitative analysis of recumbent folded deformed crossbedding. Sedimentology, 31, 257-283. A. & HOMEWOOD,P. 1984. Evolution and dynamics of a Miocene tidal sandwave. Sedimentology, 31, 63-81. ANDERTON, R. 1976. Tidal-shelf sedimentation: an example from the Scottish Dalradian. Sedimentology, 23, 429-458. M. 1990. Classification of large-scale subaqueous bedforms: a new look at an old problem. Journal o f Sedimentary Petrology, 60, 160-172. M. & MEDINA,E 1989. Fauna y microflora del Cret~icico en Bahia Brandy, Isla James Ross, Antfirtida.

1980.

They also demonstrated that the development of this facies is influenced by its location on the delta slope. They noted that fully planar laminated ungraded beds are found on the upper slope. As beds are traced down-slope, structureless intervals appear and progressively form a greater proportion of the beds until there is virtually no lamination present in beds on the lower slope. Facies 4: M e d i u m - to thick-bedded sandstones Facies 4 is represented by fine- to coarse-grained sandstones, in beds 5-60 cm thick (Fig.

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