Future Advances in Basin Modeling  Suggestions from Current Observations, Analyses, and Simulations 

<br/><br/><br/>English[eng] 
<br/><br/><label>Subjects--Topical Terms: </label><br/>normal faulting||sill intrusions||transient thermal effects||steady state||basin modeling||volcanic basins||salt||thermal modeling||source rock maturation||petroleum system||salt structures||modeling principles||geohistory evolution||temperature effects||conductivity effects on maturation||multiscale/multiphysics basin modeling||thermo-hydro-mechanical model||isostatic adjustment||computer simulations||finite element method||basin modelling||hydro-mechanical coupling||passive margins||rock failure||Glaciations||isostasy||flexural stress||faults||hydrocarbon migration||magmatic intrusions||diagenesis||stress||porosity||permeability||stress modeling||fracture seismic||fracture connectivity||fracture mapping||passive seismic||sedimentary basins||fluid flow||capillary seals||chemical alteration||resources||chalk||compaction||water weakening||rock—fluid interaction||modelling||crustal well-core poroperm||crustal fluid flow||crustal flow channeling||critical state physics||well-log spectral scaling||crustal power law scaling||lognormal||pink noise||crustal fracture seismics||crustal fracture imaging||hydrogen economy||natural hydrogen vents||Sao Francisco Basin||pulsing gas emission||atmospheric pressure tides||native hydrogen||H2 exploration||gas seeps||H2 venting||radiolysis||serpentinization||draining faults||intra-cratonic basin||diurnal hydrogen gas venting||earth tides||crustal sills||hydrocarbon and mineral resources||direct inversion method of fault slip analysis||paleo tectonic principal stress orientations||west-central New Hampshire||n/a