Organic-rich shales are found
throughout
shale
gas
production. The
criteria for assessing the natural
gas
potential of these
shale
units included
(1) probable
gas
content as estimated from kerogen/bitumen
content, level of organic maturity and petrophysical
properties; (2) thickness and lateral extent of the
shale
under conditions for
gas
generation/retention; and (3) suitability for successful fracture
stimulation. The open lacustrine black
shale
facies of the Green River Formation (Eocene) possesses good
potential for large
gas
yields where in the
gas
generative window beneath the
Uinta basin, but resource development may be difficult and expensive. Shallow
microbial
gas
from this black
shale
is known, but commercialization in
significant quantities is unlikely. The
Shale
(Upper Cretaceous),
neither a conventional black
shale
, are excellent candidates for developing
large volumes of add-on
gas
in the southern Uinta basin. The lithologically similar and slightly older Tropic
Shale
(Turonian) may locally produce significant quantities of
add-on
gas
in association with future deep CBM development in southern
Shale
(Lower Cretaceous) has excellent potential as a
shale
gas
reservoir, but future exploitation will be restricted to just limited areas north of the
Shale
(Mississippian-Pennsylvanian)
and Delle Phosphatic
Shale
Member (Mississippian) are organic-rich and widespread through western
gas
only in very restricted areas and quantities.