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Titlebook: Coated Grains; Tadeusz M. Peryt Conference proceedings 1983 Springer-Verlag Berlin Heidelberg 1983 Dolomite.Gestein.Karbonatgestein.Konkre

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书目名称Coated Grains
编辑Tadeusz M. Peryt
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图书封面Titlebook: Coated Grains;  Tadeusz M. Peryt Conference proceedings 1983 Springer-Verlag Berlin Heidelberg 1983 Dolomite.Gestein.Karbonatgestein.Konkre
描述Coated grains have always attracted attention, at first of naturalists, and later of geologists, and the interest in these peculiar bodies was re­ lated both to their intriguing form and their significance in facies inter­ pretation and sedimentology and to their relevance to accumulations of hydrocarbons and other mineral deposits. This resulted in numerous publications on this subject, and the intention of this volume is to sum­ marize the present state of knowledge on coated grains. The idea of the book was to unite some general papers with papers reporting case studies of both recent and ancient coated grains. The organization of the book follows this intention. The papers presented in this volume have been invited by the editor; the theme of the book merits a few words of personal history. The development of studies of coated grains during the last two decades has not only resulted in a great increase in knowledge of recent and ancient environments of coated grain formation, but also numerous important and controversial questions of classification, environmental significance, mineralogical composition etc. of ancient coated grains have arisen. To answer these questions, in 197
出版日期Conference proceedings 1983
关键词Dolomite; Gestein; Karbonatgestein; Konkretion; Sediment; classification; diagenesis; environment; fabric; fo
版次1
doihttps://doi.org/10.1007/978-3-642-68869-0
isbn_softcover978-3-642-68871-3
isbn_ebook978-3-642-68869-0
copyrightSpringer-Verlag Berlin Heidelberg 1983
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John L. Plews,Kim Misfeldt,Feisal Kirumiraory of ancient carbonate rocks may be inferred by studying these compositions. The carbon and oxygen isotopes in carbonate minerals have both been used extensively in the studies of environment of deposition, diagenesis and burial history (Gross 1964, Land 1970, Tan and Hudson 1974, Weber et al. 197
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https://doi.org/10.1007/978-3-319-77134-2nd smooth as the trunk of a tree which divides into branches at the top.” This is the description of the initial ash cloud of the eruption of Mount Vesuvius on August 24, 79 A. D. as given by C. Plinius (the younger) in a letter to the historian P.C. Tacitus. Had he shown the same scientific interes
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Martin Mullen,Marta Giralt,Liam Murray-like grains, resembling the roe of a fish, each of which has usually a small fragment of sand as a nucleus, around which concentric layers of calcareous matter have accumulated.” Also Sorby’s detailed description of calcareous “oolitic grains” from 1879 is still modern. He distinguished between the
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Martin Mullen,Marta Giralt,Liam Murrayth cherty and chert-poor iron formations are similar morphologically to Recent calcareous ooids (Markun and Randazzo 1980, Rohrlich 1974). Ferriferous oolitic layers are always concentric and do not display the pervasive radial structure that cuts across concentric layers in many ancient calcitic oo
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Martin Mullen,Marta Giralt,Liam Murrayabric. Compositionally, modern ooids consist of low-magnesian calcite (0%–5% MgCO.), high-magnesian calcite (10%–18% MgCO.) and aragonite with more than one phase commonly occurring within an individual cortex (e.g, Land et al. 1979). The primary mineralogy of ancient (now low-magnesian calcite) cor
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Martin Mullen,Marta Giralt,Liam Murraythe dominant processes determining the character of these platform edges and distal lagoons (Hubbard et al. 1976, Hine 1977, Hine and Neumann 1977, Harris 1979, Palmer 1979, Hine et al. 1981a, b, Wilber 1981). The recent acquisition and analysis of high quality space and aerial imagery (see acknowle
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