05084nam 2201309z- 450 991067403380332120231214132833.0(CKB)5400000000042668(oapen)https://directory.doabooks.org/handle/20.500.12854/68466(EXLCZ)99540000000004266820202105d2021 |y 0engurmn|---annantxtrdacontentcrdamediacrrdacarrierFuture Advances in Basin ModelingSuggestions from Current Observations, Analyses, and SimulationsBasel, SwitzerlandMDPI - Multidisciplinary Digital Publishing Institute20211 electronic 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: generalbicsscnormal faultingsill intrusionstransient thermal effectssteady statebasin modelingvolcanic basinssaltthermal modelingsource rock maturationpetroleum systemsalt structuresmodeling principlesgeohistory evolutiontemperature effectsconductivity effects on maturationmultiscale/multiphysics basin modelingthermo-hydro-mechanical modelisostatic adjustmentcomputer simulationsfinite element methodbasin modellinghydro-mechanical couplingpassive marginsrock failureGlaciationsisostasyflexural stressfaultshydrocarbon migrationmagmatic intrusionsdiagenesisstressporositypermeabilitystress modelingfracture seismicfracture connectivityfracture mappingpassive seismicsedimentary basinsfluid flowcapillary sealschemical alterationresourceschalkcompactionwater weakeningrock-fluid interactionmodellingcrustal well-core poropermcrustal fluid flowcrustal flow channelingcritical state physicswell-log spectral scalingcrustal power law scalinglognormalpink noisecrustal fracture seismicscrustal fracture imaginghydrogen economynatural hydrogen ventsSao Francisco Basinpulsing gas emissionatmospheric pressure tidesnative hydrogenH2 explorationgas seepsH2 ventingradiolysisserpentinizationdraining faultsintra-cratonic basindiurnal hydrogen gas ventingearth tidescrustal sillshydrocarbon and mineral resourcesdirect inversion method of fault slip analysispaleo tectonic principal stress orientationswest-central New HampshireResearch & information: generalFjeldskaar Willyedt1338946Cathles LawrenceedtFjeldskaar WillyothCathles LawrenceothBOOK9910674033803321Future Advances in Basin Modeling3059245UNINA