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dc.contributor.editorAl-Aasm, Ihsan
dc.contributor.editorMansurbeg, Howri
dc.date.accessioned2022-01-11T13:31:15Z
dc.date.available2022-01-11T13:31:15Z
dc.date.issued2021
dc.identifierONIX_20220111_9783036500782_149
dc.identifier.urihttps://directory.doabooks.org/handle/20.500.12854/76413
dc.description.abstractDiagenesis 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.
dc.languageEnglish
dc.subject.classificationbic Book Industry Communication::G Reference, information & interdisciplinary subjects::GP Research & information: general
dc.subject.otherdiagenesis
dc.subject.otherauthigenic minerals
dc.subject.otherreservoir quality
dc.subject.otherEboliang
dc.subject.otherQaidam Basin
dc.subject.otherclay minerals
dc.subject.othermajor elements
dc.subject.othertrace elements
dc.subject.othersedimentary environment
dc.subject.otherdiagenetic Environment
dc.subject.othersilicification
dc.subject.othermeteoric diagenesis
dc.subject.otherfractures
dc.subject.otherdeltaic sequence
dc.subject.otherkarst
dc.subject.otherglacial period
dc.subject.otherdolomitization
dc.subject.otherHuron Domain
dc.subject.otherSilurian
dc.subject.otherDevonian
dc.subject.otherfluid composition
dc.subject.otherMichigan Basin
dc.subject.otherbipyramidal quartz
dc.subject.otherpseudohexagonal aragonite
dc.subject.otherIberian Range
dc.subject.otherUpper Triassic
dc.subject.otherhydrothermal circulation
dc.subject.othercarbonate reservoirs
dc.subject.othersedimentation
dc.subject.otherporosity
dc.subject.otherplatform carbonates
dc.subject.otherREE + Y chemistry
dc.subject.otherpaleoceanographic proxies
dc.subject.otherdiagenetic proxies
dc.subject.otherNE Turkey
dc.subject.otherhydrothermal dolomite
dc.subject.otherdiagenetic settings
dc.subject.otheroptical petrography
dc.subject.othergeochemical
dc.subject.otherTriassic-Jurassic successions
dc.subject.otherProvençal Domain
dc.subject.othern/a
dc.titleChemical, Mineralogical and Isotopic Studies of Diagenesis of Carbonate and Clastic Sediments
dc.typebook
oapen.identifier.doi10.3390/books978-3-0365-0079-9
oapen.relation.isPublishedBy46cabcaa-dd94-4bfe-87b4-55023c1b36d0
oapen.relation.isbn9783036500782
oapen.relation.isbn9783036500799
oapen.pages218
oapen.place.publicationBasel, Switzerland


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