LEADER 03903nam 2200841z- 450 001 9910557441703321 005 20231214133313.0 035 $a(CKB)5400000000043305 035 $a(oapen)https://directory.doabooks.org/handle/20.500.12854/76413 035 $a(EXLCZ)995400000000043305 100 $a20202201d2021 |y 0 101 0 $aeng 135 $aurmn|---annan 181 $ctxt$2rdacontent 182 $cc$2rdamedia 183 $acr$2rdacarrier 200 10$aChemical, Mineralogical and Isotopic Studies of Diagenesis of Carbonate and Clastic Sediments 210 $aBasel, Switzerland$cMDPI - Multidisciplinary Digital Publishing Institute$d2021 215 $a1 electronic resource (218 p.) 311 $a3-0365-0078-2 311 $a3-0365-0079-0 330 $aDiagenesis 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. 606 $aResearch & information: general$2bicssc 610 $adiagenesis 610 $aauthigenic minerals 610 $areservoir quality 610 $aEboliang 610 $aQaidam Basin 610 $aclay minerals 610 $amajor elements 610 $atrace elements 610 $asedimentary environment 610 $adiagenetic Environment 610 $asilicification 610 $ameteoric diagenesis 610 $afractures 610 $adeltaic sequence 610 $akarst 610 $aglacial period 610 $adolomitization 610 $aHuron Domain 610 $aSilurian 610 $aDevonian 610 $afluid composition 610 $aMichigan Basin 610 $abipyramidal quartz 610 $apseudohexagonal aragonite 610 $aIberian Range 610 $aUpper Triassic 610 $ahydrothermal circulation 610 $acarbonate reservoirs 610 $asedimentation 610 $aporosity 610 $aplatform carbonates 610 $aREE + Y chemistry 610 $apaleoceanographic proxies 610 $adiagenetic proxies 610 $aNE Turkey 610 $ahydrothermal dolomite 610 $adiagenetic settings 610 $aoptical petrography 610 $ageochemical 610 $aTriassic-Jurassic successions 610 $aProvenc?al Domain 615 7$aResearch & information: general 700 $aAl-Aasm$b Ihsan$4edt$01302214 702 $aMansurbeg$b Howri$4edt 702 $aAl-Aasm$b Ihsan$4oth 702 $aMansurbeg$b Howri$4oth 906 $aBOOK 912 $a9910557441703321 996 $aChemical, Mineralogical and Isotopic Studies of Diagenesis of Carbonate and Clastic Sediments$93026258 997 $aUNINA