03942nam 2200865z- 450 991055744170332120220111(CKB)5400000000043305(oapen)https://directory.doabooks.org/handle/20.500.12854/76413(oapen)doab76413(EXLCZ)99540000000004330520202201d2021 |y 0engurmn|---annantxtrdacontentcrdamediacrrdacarrierChemical, Mineralogical and Isotopic Studies of Diagenesis of Carbonate and Clastic SedimentsBasel, SwitzerlandMDPI - Multidisciplinary Digital Publishing Institute20211 online resource (218 p.)3-0365-0078-2 3-0365-0079-0 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.Research and information: generalbicsscauthigenic mineralsbipyramidal quartzcarbonate reservoirsclay mineralsdeltaic sequenceDevoniandiagenesisdiagenetic Environmentdiagenetic proxiesdiagenetic settingsdolomitizationEboliangfluid compositionfracturesgeochemicalglacial periodHuron Domainhydrothermal circulationhydrothermal dolomiteIberian Rangekarstmajor elementsmeteoric diagenesisMichigan Basinn/aNE Turkeyoptical petrographypaleoceanographic proxiesplatform carbonatesporosityProvençal Domainpseudohexagonal aragoniteQaidam BasinREE + Y chemistryreservoir qualitysedimentary environmentsedimentationsilicificationSiluriantrace elementsTriassic-Jurassic successionsUpper TriassicResearch and information: generalAl-Aasm Ihsanedt1302214Mansurbeg HowriedtAl-Aasm IhsanothMansurbeg HowriothBOOK9910557441703321Chemical, Mineralogical and Isotopic Studies of Diagenesis of Carbonate and Clastic Sediments3026258UNINA