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Autor:
Joel Wesley Martin, Mark Joseph Gresko, Robert A. Skopec, David M. Byrd, Kyle Ross Koerner, Roy Lee Hathcock, Gustavo Dario Cavazzoli, Bernhard Lungwitz, Christopher N. Fredd
Publikováno v:
All Days.
The Macaé formation (Cretaceous age, Campos Basin, Brazil) is predominantly an oolitic and oncolitic grainstone and packstone limestone with a bottomhole static temperature (BHST) of about 150°F. The formation permeability often exceeds one darcy.