Titlebook: Carbonate Depositional Systems: Assessing Dimensions and Controlling Parameters; The Bahamas, Belize Hildegard Westphal,Bernhard Riegl,Gre

cartilage

Book 2010 and hydrocarbon reservoirs. Complex interaction of physical and chemical parameters with biological parameters determines the architecture and composition of carbonate sedimentary bodies. This book closes some of the still existing gaps in our understanding of the influence and interplay of physica

audiologist

sedimentological settings.Data useful for biologists and geCarbonate sediments are of increasing relevance for archives of past environmental conditions and for economical reasons in areas of geothermal energy and hydrocarbon reservoirs. Complex interaction of physical and chemical parameters with

white-matter

Encapsulate

預(yù)防注射

mydriatic

The Gulf: Facies Belts, Physical, Chemical, and Biological Parameters of Sedimentation on a Carbonaed a ramp. Despite this controversy, the Holocene sedimentary fill of the current Gulf has been and will continue to be used as a model for a carbonate ramp. This interest in the area is hightened by the fact that is one of the few places in which Holocene dolomite and evaporites form.

Intractable

惡名聲

https://doi.org/10.1007/978-1-4757-3155-2ination of both, the sedimentary -processes and their products that can thus be tied together. General rules extracted from observations of modern analogues help reconstructing past depositional processes and understanding the facies arrangement preserved in sedimentary rocks.

小淡水魚(yú)

Parameters Controlling Modern Carbonate Depositional Environments: Approach,was triggered by research groups of several large petroleum companies, ignited a boom in carbonate research (among others: Ginsburg 1956, 1957; Ginsburg and Lloyd 1956; Lowenstam and Epstein 1957; Newell and Rigby 1957; Wells 1957; Purdy 1961, 1963; Imbrie and Purdy 1962).

燒烤

Summary: The Depositional Systems of the Bahamas, Belize Lagoon and The Gulf Compared,ination of both, the sedimentary -processes and their products that can thus be tied together. General rules extracted from observations of modern analogues help reconstructing past depositional processes and understanding the facies arrangement preserved in sedimentary rocks.