Carbonates in Continental Settings: Facies, Environments, by A.M. Alonso-Zarza, Lawrence H. Tanner PDF

By A.M. Alonso-Zarza, Lawrence H. Tanner

ISBN-10: 0444530258

ISBN-13: 9780444530257

This e-book presents an up to date compilation of the newest learn at the petrography, facies, paleonvironmental value and financial points of continental carbonates. the general association of the publication first emphasizes the descriptive features and tactics working on carbonate deposits in significantly diverse settings, after which considers functions for basin research, in addition to financial and old elements. This quantity might be a important instrument for graduate and postgraduate scholars in addition to for skilled researchers. the second one part (volume sixty two during this series) will take care of the geochemistry, diagenesis and functions of carbonates in continental settings.

  • Covering the drastically different elements of carbonate deposits from continental settings deposits
  • Clear and simple to stick to association
  • Up so far details, so readers can locate references from the vintage literature to the newest research

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Additional info for Carbonates in Continental Settings: Facies, Environments, and Processes

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Kirby et al. (2002) link d18O signals in the carbonate sediments of Fayetteville Green Lake (New York, USA) to circumpolar vortex variability affecting rainfall patterns. , 1991; Ricketts and Johnson, 1996b; Ricketts and Anderson, 1998). , 2008, 2009). A baseline on isotopic water composition must be established from the sampling of all input waters (or inferences about isotopic values for all possible lake inputs in the geologic record). Then, the proportional effects of these inputs are inferred, so that past environmental and climatic changes can be deduced more accurately.

1997). , 2001) have been linked through Sr isotopic analysis to sublacustrine seeps. Logan et al. (1962) classified stromatolitic (biohermal) algal structures and reefs according to the arrangements of algal structures based on environmental parameters in the marine realm. Their growth is dependent on the wave energy, position in the intertidal to subtidal zone, and sediment input. This general idea is also applied to algal reef zones as well as oncolite formation in lakes. , 1997; Paul and Peryt, 2000), including energy conditions (depth) and sediment influx.

Bed contains charophytes, ostracodes, and carbonized plant material and is interpreted as shallow deltaic sediment. Lens cap for scale. (D) Core photo with massive limestone facies overlain by laminated carbonate within association A (see Figure 14) from the Pennsylvanian Upper Freeport Limestone, northern Appalachian Basin (USA), interpreted as littoral sediments of a shallow carbonate lake with very rare exposure. Scale bar 1 mm. Photo by Blas Valero. (E) Thin section (regular light) of massive carbonate mudstone overlain by ostracode wackestone within association C (see Figure 14) from the Pennsylvanian Upper Freeport Limestone, northern Appalachian Basin (USA), interpreted as a bioturbated deposit overlain by an ostracode coquina bed in a shallow carbonate lake.

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Carbonates in Continental Settings: Facies, Environments, and Processes by A.M. Alonso-Zarza, Lawrence H. Tanner


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