Basin deconstruction-construction: Seeking thermal-tectonic consistency through the integration of geochemical thermal indicators and seismic fault mechanical stratigraphy ​– Example from Faras Field, North Western Desert, Egypt
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文摘

A basin model is a geological boundary value problem with specified ending conditions but with unknown initial conditions.

Fault mechanical stratigraphy can be used to validate the observed pulses of crustal extension and shortening observed in 1D tectonic subsidence history profiles.

Thermal-tectonic modeling for Faras Field reveals three rifting events with three intervening crustal shortening events.

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