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Palabras clave – provistas por la editorial

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