Mini-seminars on Applications of Geochemistry


Humble Geochemical Services is pleased to offer one hour seminars on various topics and applications in organic geochemistry. If you would be interested in such a presentation, please contact to arrange a time. We have presented these topics either during regular working hours or as lunch-time presentations that provide a break from day-to-day activities with the opportunity for interaction between speaker and audience as well as among the audience themselves.

Topics

Planning a Geochemical Program
This discussion focuses on defining objectives for a particular geochemical study and the analyses and samples necessary to meet these objectives. A properly designed geochemical program is absolutely necessary to achieve maximum benefit from the program and to insure that the correct samples are gathered, that they are gathered properly, and that the analytical program is properly designed for the objectives of the study. Objective evaluation worksheets are provided. Budgeting is also included for both regional and well programs.

Kinetics for Geologists (or geochemists)
Befuddled by this chemical terminology and what it means in the process and timing of the generation of oil? This 1 hour discussion provides a simple explanation of the complex process of organic matter decomposition into oil and how it affects the timing of oil generation and expulsion. A “Velcro quilt” analogy is used to explain the process, structure and composition, and kinetic parameters in terms familiar to everyone. Examples of typical source rocks from around the world are also described and compared.

Finding Overlooked Payzones
One of my first applications in organic geochemistry was geochemically logging a well to identify payzones in the Anadarko Basin (Jarvie and Baker, 1984). The interesting aspect of this paper was not the fact the we correctly identified the productive interval discovered but the fact that one potentially productive zone was overlooked. Since that time we have used organic geochemistry to identify hard-to-find payzones and predict oil quality prior to testing. Where these techniques work best and how to incorporate data into your well evaluation process are discussed in this talk. Where does it work best? Fractured shale reservoirs, low resistivity sands, stacked sands, wells drilled with oil-based mud, wells drilled through fresh water. This technique has a straight-forward payback - oil/condensate in active or previously drilled wells.

Exploration Geochemistry
This is a general talk on aspects of geochemistry used to identify petroleum source rocks, their petroleum potential, products likely to be generated, thermal maturity, timing of generation, oil-to-source rock correlation, and oil typing and correlation. This talk focuses on recent advances in techniques and application of organic geochemistry for unraveling source potential and expulsion temperatures.

Reservoir Compartmentalization (for development geologists and engineers)
Looking to shut-in a well for pressure testing to evaluate reservoir continuity? This is an outstanding technique for evaluating connectivity but what about lost production and what if the well doesn't come back on line? Reservoir Oil Fingerprinting™ (ROF) is a technique that utilizes a graphical and statistical comparison of oil fingerprints to assess continuity. Oil samples from various wells and horizons are “fingerprinted” revealing any compositional hetergeneity that results when reservoirs are not connected. Does it work? Various examples both published and unpublished (but nonproprietary) examples are presented demonstrating the efficacy of this technique.

Interpretive Geochemistry
This is a sequential series of approximately 1 hour seminars providing basic and detailed assessment of geochemical data to really understand these data. The seminar series proceeds from basic, screening analysis to detailed basin wide evaluations. Topics are presented in the following sequence (although depending of the audience and level of understanding any topic may be presented in or out of sequence):

  1. TOC and Rock-Eval analyses - a wealth of information
  2. Vitrinite reflectance and Visual Kerogen Assessment - maturity and kerogen type
  3. Sampling for geochemical analyses
  4. Kerogen type assessment using pyrolysis gas chromatography and laboratory maturation
  5. Evaluating maximum temperature exposure of a section - application of apatite fission track analysis and age dating
  6. Determining the timing of oil/gas generation
    1. Understanding and applying bulk kinetic assessments using the appropriate model and checking experimental results
    2. Evaluating the timing of oil and gas generation - compositional Kinetic evaluations using open and closed system pyrolysis
  7. Assessing the products generated during thermal maturation
  8. Light hydrocarbon and whole gas chromatography interpretation (exploration)
  9. Oil typing and oil-to-oil correlation
  10. Oil-to-source rock correlation
  11. Evaluating expulsion, migration pathways, and seal efficiency
  12. Modeling the Generation and Expulsion of Oil/Gas - 1 D Basin Modeling
  13. Petroleum Systems Evaluation - From Source to Trap
  14. In-reservoir alteration of oils: processes and evaluation
  15. Finding overlooked payzones and assessing oil quality
  16. Evaluating reservoir continuity

Re-evaluation of Petroleum Systems of the Williston Basin
This is a summary presentation from four separate talks given on the petroleum systems of the Williston Basin. This talk focuses on previously unidentified effective source rocks in the basin, their rates of decomposition into oil and gas, and an evaluation of oil types across the basin. Oils from every producing horizon in the Williston Basin are discussed.

Rates and Products formed from oxygen and sulfur rich kerogens of the Monterey Formation, Santa Maria Basin, California
This talk focuses on the chemical characteristics of the Monterey Formation that result in quite different rates of kerogen decomposition among various organic facies within the Monterey Formation. Phosphatic Monterey Formation rocks having high oxygen and sulfur contents undergo transformation at much lower thermal thresholds than strictly sulfur rich Monterey Formation kerogens. Comparison to other Type II source rocks is presented.