LEADER 02807nam 2200361 450 001 9910674014003321 005 20230626123507.0 035 $a(CKB)5700000000300409 035 $a(NjHacI)995700000000300409 035 $a(EXLCZ)995700000000300409 100 $a20230626d2022 uy 0 101 0 $aeng 135 $aur||||||||||| 181 $ctxt$2rdacontent 182 $cc$2rdamedia 183 $acr$2rdacarrier 200 10$aEffects of Diagenetic Alterations on Hydrocarbon Reservoirs and Water Aquifers /$fHowri Mansurbeg 210 1$aBasel :$cMDPI - Multidisciplinary Digital Publishing Institute,$d2022. 215 $a1 online resource (134 pages) 311 $a3-0365-5545-5 330 $aReservoir quality (porosity and permeability) and heterogeneity in carbonate and siliciclastic hydrocarbon reservoirs and groundwater aquifers are significantly constrained by diagenetic processes, such as biological, chemical, biochemical, and mechanical changes, that occur in sediments subsequent to deposition and prior to low-grade metamorphism. Diagenesis, which has a variable but overall important impact on reservoir quality evolution, is controlled by several inter-related parameters. These parameters include the depositional composition of the sediments, depositional facies, sequence stratigraphy, pore water chemistry, burial history and tectonic setting of the basin, and paleoclimatic conditions.Carbonate and siliciclastic sediments often undergo multiple stages of diagenesis, which are related to complex patterns of burial-thermal history (subsidence and uplift) that are controlled by the tectonic evolution of the basin. Tectonic evolution of the basin is controlled by the position of the basin with respect to the type and activity along the plate boundaries. The episodes of burial and uplift may result in profound modifications in the pressure-temperature regimes and in the extent of mineral-water interaction, and hence in various phases of compaction, as well as mineral dissolution, recrystallization, transformation, and cementation. Diagenesis impacts reservoir quality in the following ways: (i) destruction by mechanical compaction and extensive cementation, (ii) preservation by prevention of mechanical and chemical compaction, or (iii) generation by dissolution of labile framework grains and intergranular cements. 606 $aEarth sciences$xStudy and teaching 606 $aEarth sciences 615 0$aEarth sciences$xStudy and teaching. 615 0$aEarth sciences. 676 $a550.71 700 $aMansurbeg$b Howri$01367660 801 0$bNjHacI 801 1$bNjHacl 906 $aBOOK 912 $a9910674014003321 996 $aEffects of Diagenetic Alterations on Hydrocarbon Reservoirs and Water Aquifers$93391305 997 $aUNINA