Classroom Courses: CAN'T MAKE IT TO THE FIELD? THE NEXT BEST THING IS A 3- TO 5-DAY CLASS DESIGNED FOR THE CLASSROOM.
Superb outcrop and core examples
Great graphics
Clear descriptions of basic to advanced principles
Basin-wide outcrop to core to wireline-log examples
Oil and gas field case studies
Practical exercises that bring it all together
CD with all the essential material
The Clastic Reservoirs Facies course offers an
in-depth analysis of the distributions, geometries and sedimentary
architectures of clastic reservoir facies. The course is designed for
geologists, geophysicists, reservoir engineers, reservoir simulation engineers
and other asset team members. Participants will learn the criteria for
distinguishing reservoir facies using wireline log and core data, how to
interpret facies distributions at regional and field scales, and how to
integrate this information into exploration and development projects.
Emphasis is on fluvio-deltaic facies, with coverage of alluvial fan, fluvial,
eolian, shoreface, deltaic and shelf environments. Lectures cover the
basics; supporting details are drawn from numerous studies worldwide. Exercises
utilizing log and core data provide an opportunity for participants to practice
the methodologies addressed in the course. A wealth of outcrop and core
photos, as well as numerous wireline log examples, isopach maps, and seismic
attribute maps, are combined to yield a detailed yet very understandable
treatment of this complicated subject.
GENERAL STUDIES convey essential concepts and principles, drawing on
examples from a variety of geographical areas.
The Western Interior
Cretaceous Seaway of North America provides many of the examples used in the
course.
Facies Tracts: An introduction to facies tracts focusing on
coastal plain to shallow marine.
Sequence
Stratigraphic Concepts
Definition of terms
Sequences and systems tracts
Accommodation space and
coastal plain onlap
Parasequences and
parasequence stacking patterns
Parasequence sets and trajectory
Facies architecture in
parasequences
Shallow-Marine
Facies
Shoreface
Shoreface profile
Shoreface processes
Marginal marine
Shoreface erosion
Tse vs flooding surface
Transgressive deposits
Deltas
Tour of world deltas: a trip around the ternary diagram
Wave-, river-,
tide-dominated deltas
Distinguishing delta front and shoreface using outcrop and subsurface data
Delta vs delta complex
Relating channel belts to
their laterally equivalent delta-front deposits
Fluvial Strata
Categorization:straight, meandering,
braided and anastamosing, and the extent to which this may be a totally arbitrary exercise
Channel belt evolution
Barriers and baffles to
fluid flow
Methodologies for subsurface correlations in high
and low net-to-gross strata
Alluvial-fan facies
Eolian facies
Trace Fossils
FORMATION-SPECIFIC
STUDIES utilize information
from one or more formations, generally within a single basin or region.
Ferron Sandstone,
east-central Utah
Dakota Sandstone, cental and
southwestern Utah
Fall River Formation, Powder
River Basin, Wyoming
Muddy Sandstone, Powder River Basin, Wyoming
Lower Troncoso Member of
Huitrin Formation, Neuquen Basin,
Argentina
Mio-Pliocene strata of the KuraBasin, Republic of Georgia
Morrison Formation, Henry Mountains Basin, Utah
FIELD-SPECIFIC
STUDIES focus on the geology of
a single or several related oil and gas fields.
Coyote Creek-Miller Creek Trend, Powder River Basin - meanderbelt and delta-front reservoirs
Lunlunta-Carrizal field, Cuyo Basin, Argentina - high net-to-gross, ephemeral stream reservoirs
Kerisi and Hiu structures, WestNatunaBasin,
offshore Indonesia - fluvial to shallow lacustrine reservoirs
EXERCISES demonstrate how concepts presented in the course can
be applied in oil and gas exploration and development projects.
MuddyCanyon Sandstone Discovery. A fictitious oil and gas
discovery in the Muddy Canyon Sandstone (based on the Ferron Sandstone, Utah)
involves probabilistic estimates of recoverable oil. Does the project
meet your client's criteria?
Mapping Channel Belts at FrostbiteFalls. Another fictitious
reservoir, this one based on avulsion behaviour of the Saskatchewan
River. Depleted wells are to be recompleted in a shallower
gas zone. What is the range of uncertainty in the fluvial reservoir
volumes?
Fall River Correlation Exercise. Approximately 300
wireline logs are used to distinguish and map facies in fluvio-deltaic strata
in the Coyote Creek-Miller Creek productive trend, which produces oil from a
series of stratigraphic traps in the eastern part of the PowderRiver Basin.
Core photos guide the facies interpretation. (The exercise utilizes logs,
cross sections and maps compiled in Microsoft Powerpoint; it can all be done on
paper in situations where a sufficient number of PCs are not available.)