Titlebook: Carbonate Microfabrics; Richard Rezak (Professor Emeritus),Dawn L. Lavoie Book 1993 Springer-Verlag New York, Inc. 1993 chemistry.fabric.g

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Solid Mechanics and Its Applications of monomineralic allochems of known aragonite or HMC (high-magnesium calcite) mineralogy provide strong evidence supporting the inference of mineralogic control on the generation of ADP or CDP micrite microfabrics. The relationship between strontium contents and crystal size in micrites refutes int

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小丑

https://doi.org/10.1007/978-3-662-04299-1d conglomerate from the Trenton Limestone. This indicates that the substrate has a large effect on the CSD. There is no simple nucleation and growth law that explains the CSD of most of the ancient dolomites studied. However, a qualitative model of continuous nucleation and flux-limited growth is co

Postulate

Microfabrics in Carbonate Diagenesis: A Critical Look at Forty Years in Researchour theories over the last few decades has become apparent as we have sought revelation in various diagenetic environments, first the meteoric, then the open-system marine, later the deep-burial and now the closed-system marine. The narrative of kaleidoscopic change points only to a similarly challe

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Trends of Sedimentary Microfabrics of Ooid Tidal Channels and Deltasannel, ooids are bimodal in size (large ooids have numerous laminae and small ooids have fewer laminae) and therefore less well sorted. Nuclei of ooids are dominated by peloids in all environments. A trend of increasing size of ooids on ebb-tidal deltas and along intervening beaches in the direction

Triglyceride

Depositional and Early Diagenetic Controls on Texture and Fabric of Carbonate Mudbanks, South Florid south Florida have grown as physically dynamic sediment bodies and contain both physical and biogenic depositional facies. Mudbank facies are influenced to varying degrees by biological processes of sediment production, aggregation and substrate stabilization. Depositional facies have been partiall

Neutral-Spine

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