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Carbonate Sedimentology: A Comprehensive Review of Limestone Formation and Evolution
Carbonate rocks, such as limestones and dolomites, are among the most important geological formations in the world. They contain not only 60% of the world's known hydrocarbons, but also host extensive mineral deposits. Carbonate sedimentology is the study of how these rocks form, change and interact with their environment.
One of the most authoritative and comprehensive books on carbonate sedimentology is Carbonate Sedimentology by Maurice E. Tucker and V. Paul Wright, first published in 1990. This book covers all aspects of carbonate sedimentology, from the basic constituents and classification of carbonate rocks, to the geological background and modern environments of carbonate deposition, to the diagenetic processes and products that affect carbonate rocks, to the dolomitization models and geological record of carbonate rocks. The book also includes a chapter by J.A.D. Dickson on carbonate mineralogy and chemistry.
Carbonate Sedimentology is aimed at advanced undergraduate and postgraduate students, as well as geologists working in the oil industry or in carbonate research. The book is designed to take the reader from the basic aspects of carbonate recognition and classification through to an appreciation of the most recent developments such as large scale facies modelling and isotope geochemistry. The book also features a detailed review of carbonate mineralogy, non-marine carbonate depositional environments and an in-depth look at carbonate deposition and diagenesis through geologic time.
The book is available as a PDF download from various online sources[^1^] [^2^] [^3^]. However, readers are advised to purchase the original print or ebook version from Wiley Online Books[^1^] or Google Books[^2^] for better quality and accuracy.
One of the main strengths of Carbonate Sedimentology is that it provides integrated reviews of carbonate sedimentology and diagenesis, within one volume. Diagenesis refers to the physical and chemical changes that affect carbonate rocks after their deposition, such as compaction, cementation, dissolution, recrystallization and dolomitization. Diagenesis can have a significant impact on the porosity, permeability, mineralogy and geochemistry of carbonate rocks, and thus affect their reservoir quality and economic potential. The book discusses the various diagenetic processes, products and environments that affect carbonate rocks, as well as the methods and techniques used to study them.
Another strength of Carbonate Sedimentology is that it reviews the carbonate depositional systems in a process-based approach rather than a simple comparative sedimentology approach. This means that the book focuses on the physical, chemical and biological processes that control the formation and distribution of carbonate sediments and rocks, rather than just describing their morphology and facies. The book covers both marine and non-marine carbonate depositional environments, such as reefs, lagoons, tidal flats, sabkhas, lakes and caves. The book also discusses the deeper-water facies of pelagic and resedimented limestones, which are often overlooked in other carbonate sedimentology books.
A third strength of Carbonate Sedimentology is that it includes a chapter on carbonate mineralogy and chemistry by J.A.D. Dickson, a leading expert in this field. This chapter covers the crystallography, structure, stability and geochemistry of carbonate minerals, such as calcite, aragonite, dolomite and siderite. The chapter also discusses the isotopic composition of carbonates, which can provide valuable information on the origin, age and diagenetic history of carbonate rocks. a474f39169