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

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https://doi.org/10.1007/978-3-319-77134-2of the eastern Swiss Alps which differed from an ooid in that the coated grain called oncoid possessed (Heim 1916, p. 566): (1) non-concentric overlapping of separate envelopes, (2) not exclusively rounded form, (3) compact structure, with or without nucleus, and (4) sharp or indistinct boundaries.

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Martin Mullen,Marta Giralt,Liam Murrayarine ooids, from Cayeux (1935) to Shearman et al. (1970) and has been reestablished by Simone (1974), Sandberg (1975) and Wilkinson and Landing (1978) only in the last ten years. (3) “Recrystallized structure” is developed in calcitized former aragonitic oolitic grains, in which “the larger irregul

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Conference proceedings 1983ed 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 pres

sebaceous-gland

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