Chemical, Mineralogical and Isotopic Studies of Diagenesis of Carbonate and Clastic Sediments

Chemical, Mineralogical and Isotopic Studies of Diagenesis of Carbonate and Clastic Sediments
Author :
Publisher : MDPI
Total Pages : 218
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ISBN-10 : 9783036500782
ISBN-13 : 3036500782
Rating : 4/5 (782 Downloads)

Book Synopsis Chemical, Mineralogical and Isotopic Studies of Diagenesis of Carbonate and Clastic Sediments by : Ihsan Al-Aasm

Download or read book Chemical, Mineralogical and Isotopic Studies of Diagenesis of Carbonate and Clastic Sediments written by Ihsan Al-Aasm and published by MDPI. This book was released on 2021-06-10 with total page 218 pages. Available in PDF, EPUB and Kindle. Book excerpt: Diagenesis of carbonates and clastic sediments encompasses the biochemical, mechanical, and chemical changes that occur in sediments subsequent to deposition and prior to low-grade metamorphism. These parameters which, to a large extent, control diagenesis in carbonates and clastic sediments include primary composition of the sediments, depositional facies, pore water chemistry, burial–thermal and tectonic evolution of the basin, and paleo-climatic conditions. Diagenetic processes involve widespread chemical, mineralogical, and isotopic modifications affected by the original mineralogy of carbonate and clastic sediments. These diagenetic alterations will impose a major control on porosity and permeability and hence on hydrocarbon reservoirs, water aquifers, and the presence of other important economic minerals. In this Special Issue, we have submissions focusing on understanding the interplay between the mineralogical and chemical changes in carbonates and clastic sediments and the diagenetic processes, fluid flow, tectonics, and mineral reactions at variable scales and environments from a verity of sedimentary basins. Quantitative analyses of diagenetic reactions in these sediments using a variety of techniques are essential for understanding the pathways of these reactions in different diagenetic environments.


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