Abstract
Having discussed matrix and grain types of carbonate rocks in previous chapters, this chapter focuses on the fabrics constructed by rock constituents. The term fabric includes textural as well as structural criteria. Most fabrics reflect depositional controls or early diagenetic processes. This chapter starts with the description of common depositional and diagenetic fabrics (Sect. 5.1), continues with criteria on the recognition and significance of discontinuity structures (Sect. 5.2) which are of major importance in sequence stratigraphy, and closes with a review of predominantly postdepositional features (Sect. 5.3).
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Basics: Depositional and diagenetic fabrics
Geopetal structures
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Nodular Fabrics
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Basics: Discontinuity surfaces in carbonate rocks
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Basics: Neptunian dikes and fissure fills
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Basics: Microfractures and ‘calcite veins’ in carbonate rocks
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Misik, M. (1966): Tentative classification of veinlets in limestones. – Geol. Sborn. Slov. Akad. Vied, 17, 337-344
Misik, M. (1998): Peculiar types of thin veins in the Mesozoic carbonates and silicates of the Western Carpathians. – Geologica Carpathica, 49, 271-298
Narr, W., Burruss, R.C. (1984): Origin of reservoir fractures in Little Knife field, North Dakota. – Amer. Ass. Petrol. Geol. Bull., 68, 1087-1100
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Basics: Carbonate breccias and conglomerates
Bathurst, R.G.C. (1959): Diagenesis in Mississippian calcilutites and pseudobreccias. – J. Sed. Petrol., 29, 365-376
Blount, D.N., Moore, C.H. (1969): Depositional and non-depositional carbonate breccias, Chiantla Quadrangle, Guatemala. – Geol. Soc. Amer. Bull., 80, 429-442
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Laznicka, P. (1988): Breccias and coarse fragmentites. – Dev. Econ. Geol., 25, 832 pp., Amsterdam (Elsevier)
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Flügel, E. (2010). Microfacies Data: Fabrics. In: Microfacies of Carbonate Rocks. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-03796-2_5
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