05121nam 2201333z- 450 991067403380332120210501(CKB)5400000000042668(oapen)https://directory.doabooks.org/handle/20.500.12854/68466(oapen)doab68466(EXLCZ)99540000000004266820202105d2021 |y 0engurmn|---annantxtrdacontentcrdamediacrrdacarrierFuture Advances in Basin ModelingSuggestions from Current Observations, Analyses, and SimulationsBasel, SwitzerlandMDPI - Multidisciplinary Digital Publishing Institute20211 online resource (366 p.)3-0365-0276-9 3-0365-0277-7 This volume describes the nature, causes, and consequences of the diverse fluid movements that produce energy and mineral resources in sedimentary basins. The contained papers point to new capabilities in basin analysis methods and models. The processes that operate in the resource-producing thermo-chemical-structural reactors we call sedimentary basins are reviewed. Efficient ways to infer the tectonic history of basins are described. Impacts on hydrocarbon maturation and migration of glacial tilting, magmatic intrusion, salt migration, and fracturing are illustrated. The conditions under which subsurface flow will channel with distance traveled are identified. Seismic methods that can image and map subsurface permeability channels are described. The surface maturation, surface charge, and chemical reaction foundations of creep subsidence are set forth. Dynamic aspects of the hydrogen resource in basins are analyzed. There is much that is new that is presented in these papers with the intent of stimulating thinking and enthusiasm for the advances that will be made in future decades.Future Advances in Basin Modeling Research & information: generalbicsscatmospheric pressure tidesbasin modelingbasin modellingcapillary sealschalkchemical alterationcompactioncomputer simulationsconductivity effects on maturationcritical state physicscrustal flow channelingcrustal fluid flowcrustal fracture imagingcrustal fracture seismicscrustal power law scalingcrustal sillscrustal well-core poropermdiagenesisdirect inversion method of fault slip analysisdiurnal hydrogen gas ventingdraining faultsearth tidesfaultsfinite element methodflexural stressfluid flowfracture connectivityfracture mappingfracture seismicgas seepsgeohistory evolutionGlaciationsH2 explorationH2 ventinghydro-mechanical couplinghydrocarbon and mineral resourceshydrocarbon migrationhydrogen economyintra-cratonic basinisostasyisostatic adjustmentlognormalmagmatic intrusionsmodeling principlesmodellingmultiscale/multiphysics basin modelingn/anative hydrogennatural hydrogen ventsnormal faultingpaleo tectonic principal stress orientationspassive marginspassive seismicpermeabilitypetroleum systempink noiseporositypulsing gas emissionradiolysisresourcesrock failurerock-fluid interactionsaltsalt structuresSao Francisco Basinsedimentary basinsserpentinizationsill intrusionssource rock maturationsteady statestressstress modelingtemperature effectsthermal modelingthermo-hydro-mechanical modeltransient thermal effectsvolcanic basinswater weakeningwell-log spectral scalingwest-central New HampshireResearch & information: generalFjeldskaar Willyedt1338946Cathles LawrenceedtFjeldskaar WillyothCathles LawrenceothBOOK9910674033803321Future Advances in Basin Modeling3059245UNINA