Download Carbonate Platforms: Facies, Sequences and Evolution (IAS by Maurice E. Tucker, James Lee Wilson, Paul D. Crevello, J. PDF

By Maurice E. Tucker, James Lee Wilson, Paul D. Crevello, J. Rick Sarg, J. Fred Read

This quantity additionally discusses the pc modelling of carbonate cycles and series research. this may end up a useful textual content for senior undergraduate and postgraduate scholars within the earth sciences normally and also will be of worth to the pro researcher. Carbonate systems comprises contributions from a world authorship and the quantity has been edited through the most revered names within the earth sciences. parts lined contain; early rifting deposition; examples from carbonate sequences of Sardinia (Cambrian) and Tuscany ( Triassic-Jurassic), Italy; geometry and evolution of platform-margin bioclastic shoals, overdue Dinantian (Mississippian), Derbyshire, united kingdom; cyclic sedimentation in cabonate and combined carbonate/clastic environments; 4 simulation courses for a computing device machine; center Triassic carbonate ramp platforms within the Catalan foundation, N.E. Spain; facies, cycles, depositional sequencies and controls; phases within the evolution of overdue Triassic and Jurassic platform carbonates; western margin of the Subalpine basin, Ardech, France. The formation and drowning of remoted carbonate systems; tectonic and ecologic keep an eye on of the Northern Apennines; controls on top Jurassic carbonate building up improvement within the Lusitanian Basin, Portugal; Hauterivian to reduce Aptian carbonate shelf sedimentation and series stratigraphy within the Jura and northern Subalpine chains (southeastern France and Swiss Jura); basement structural controls on Mesozoic carbonate facies in northeastern Mexico; the Aptian-Albian carbonate episode of the Basque-Cantabrian foundation (Northern Spain); normal features, controls and evolution; reaction of the Arabian carbonate platform margin slope to orogenic remaining of an ocean basin, Cretaceous, Oman,

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Extra resources for Carbonate Platforms: Facies, Sequences and Evolution (IAS Special Publication 9)

Sample text

Fig. 10. Photomicrographs of microfacies 1 and intraclasts. (a) Bioclast peloid intraclast grainstone microfacies (microfacies 1). Note intensively micritized crinoid ossicles. Pin Dale, basinward dipping foresets sub-sequence 1. Photomicrograph of a peel. Scale bar= 250 �-tm. (b) Sorted bioclast grainstone intraclast. Pin Dale, basinward dipping foresets sub-sequence 1. Photomicrograph of a peel. Scale bar= 250�-tm. (c) Calcretized bioclast packstone intraclast. Micrite lining intergranular porosity is arrowed.

However, the asymmetric thick­ ening of the coating indicates alternating low energy conditions when the oncolites were stationary. The occurrence of packstone is attributed to infiltration carbonate mud through the sediment following a change to lower energy conditions. The bioclastic wackestone intraclasts indicates reworking of low energy sediment from sheltered areas adjacent to the sand body complex. A significant contrast with microfacies 1 is that the allochems within this micro­ facies have not been micritized.

Geol. Bull. 69, 1 - 2 1 . ROZANOV, A. Yu . & DEBRENNE, F. ( 1974) Age o f archae­ ocyathid assemblages. Am. J. Sci. 274, 833-848. RoZANOV, A. Yu. S. (1984) Lower Cambrian stage subdivision . Stratigraphy. Izd. Nauk. Acad. Sci. USSR 5 - 19 (In Russian) . R. , BAMBACH, R . K . , BARTON, C . , VAN DER Voo, R. M. (1979) Paleozoic base maps. J. Geol. 87 , 217-277. VAI, G . B . & CocozzA, T. (1986) Tentative schematic zonation of the Hercynian chain in Italy. Bull. Soc. Geol. France 2, 95- 1 14. L. (1975) Carbonate Facies in Geologic History, Springer Verlag, New York, p.

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