A
Reinterpretation of the Misoa Facies
Types: Implications of a New Depositional Model,
Gamero, Helena1, Carlos Zavala2, Carmen Contreras1 (1) Schlumberger, Caracas, Venezuela (2) Universidad Nacional del Sur, Bahía Blanca, Argentina
The Eocene-age Misoa Formation is a prolific producer of hydrocarbons in
the Maracaibo Basin, Venezuela. To understand the
depositional origin of the reservoirs and predict their distribution and
continuity, it is important to undertake a detailed sedimentological
interpretation of the available cores. One of the first steps performed in any
core description is the facies identification, which
is defined on the basis of its distinctive lithologic
features, including composition, grain size, bedding characteristics and
sedimentary structures. The facies scheme developed
for the Misoa Formation involved tractive
structures originated from sediment-free diluted flows associated to a fluvio-deltaic system. Recently, in a revision of the facies scheme, the Misoa
Formation has been reinterpreted as being deposited from sustained fluvial-derived
hyperpycnal flows. The facies
types consist principally of thick ungraded sandstone
beds, which appear massive or displaying parallel
lamination, climbing ripples, and anisotropic hummocky cross stratification.
These structures suggest a deposition by traction plus fall-out processes from
an overpassing sand-laden sustained underflow. The
alternations and gradual recurrence of these structures evidence fluctuations
in flow velocity and concentration that characterize a quasi-steady hyperpycnal flow. In recent years, hyperpycnal
flows have received increasing attention as an efficient mechanism to
transport considerable volumes of sand into the basin. The main implication in
changing the fluvio-deltaic sedimentological
model for the Misoa Formation into a hyperpycnal system lies in the consequent changes in the
lateral extension, geometries, orientation, and continuity of their associated
reservoir sands. Improved modeling is crucial for planning secondary recovery
projects.