01165nam 2200397 450 991058330410332120230120002718.00-12-811530-00-12-811529-7(CKB)4100000003844701(MiAaPQ)EBC5398370(EXLCZ)99410000000384470120180606d2018 uy 0engurcnu||||||||txtrdacontentcrdamediacrrdacarrierHeterogeneity of function in numerical cognition /Avishai HenikCambridge, Massachusetts :Elsevier,2018.1 online resource (482 pages)Mathematical abilityNumber conceptMathematicsPsychological aspectsMathematical ability.Number concept.MathematicsPsychological aspects.370.156Henik Avishai912906MiAaPQMiAaPQMiAaPQBOOK9910583304103321Heterogeneity of function in numerical cognition2044548UNINA02807nam 2200361 450 991067401400332120230626123507.0(CKB)5700000000300409(NjHacI)995700000000300409(EXLCZ)99570000000030040920230626d2022 uy 0engur|||||||||||txtrdacontentcrdamediacrrdacarrierEffects of Diagenetic Alterations on Hydrocarbon Reservoirs and Water Aquifers /Howri MansurbegBasel :MDPI - Multidisciplinary Digital Publishing Institute,2022.1 online resource (134 pages)3-0365-5545-5 Reservoir 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.Earth sciencesStudy and teachingEarth sciencesEarth sciencesStudy and teaching.Earth sciences.550.71Mansurbeg Howri1367660NjHacINjHaclBOOK9910674014003321Effects of Diagenetic Alterations on Hydrocarbon Reservoirs and Water Aquifers3391305UNINA