Numerical Investigation of Overpressure Causes in Eugene Island P1 Sand – Part II
نویسندگان
چکیده
منابع مشابه
Generation of overpressure and compaction-driven fluid flow in a Plio-Pleistocene growth-faulted basin, Eugene Island 330, offshore Louisiana
The complex pressure and porosity fields observed in the Eugene Island (EI) 330 field (offshore Louisiana) are thought to result from sediment loading of low-permeability strata. In this field, fluid pressures rise with depth from hydrostatic to nearly lithostatic, iso-pressure surfaces closely follow stratigraphic surfaces which are sharply offset by growth-faulting, and porosity declines with...
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ژورنال
عنوان ژورنال: International Journal of Engineering Research and Science
سال: 2017
ISSN: 2395-6992
DOI: 10.25125/engineering-journal-ijoer-jul-2017-7