PBS-SEPM Luncheon: Using XRF Analysis to Understand the Effects of Compositional Variations on Rock Strength Determine from Micro-Mechanical Devices

The exploration of unconventional resources and search for “sweet spots” requires understanding the geology and geologic variation of the formation of interest. Variations include stratigraphic
and structural (including strength) variations, which affect the deformation behavior and may be important when it comes to the rock’s response to hydraulic fracture stimulation. The fine-grained nature of many unconventional plays complicates traditional stratigraphic and structural analyses. Also, the high cost and time-consuming nature of many chemical analyses and rock deformation experiments using triaxial load cells may present an obstacle to adequately evaluate significant variations.

Data from three hand-held devices is used to analyze a Barnett Shale core from the Fort
Worth basin. Using energy-dispersive XRF allows assessment of the chemical and mineralogical variation and a micro-indentation tool and micro-rebound hammer are used to evaluate strength variations. These tools are easy to use, quick, relatively inexpensive, portable and non-destructive and reveal mineralogical and rock strength changes throughout the core. Furthermore, results can be used to assess how chemical variations affect rock strength.

The ~60 m cored interval was sampled every 30 cm, where XRF analyses and rock strength
tests were completed. Based on XRF analyses of both major and trace elements, the Barnett in this core is mostly a siliceous mudrock, although more quartz- and carbonate-dominated facies are locally present and overall the core can be broken into eleven chemostratigraphic facies. The unconfined compressive strength (UCS) based on the micro-indentation tool varies from ~38 to ~138 MPa with an average UCS of ~72 MPa. These values are similar to UCS values from the micro-rebound hammer. However, UCS results using the micro-rebound hammer and micro-indentation tools appear to vary systemically as mineralogy changes. While UCS values show a closer agreement in more siliceous facies, more calcareous facies appear to show greater divergence in UCS values, which suggests that the micro-rebound hammer is sensitive to the presence of carbonate material in the rock. Overall, our approach provides a quick, reliable assessment of the mineralogy and strength variations of the coreand shows how the former can influence the latter.

Speaker: Dr. Helge Alsleben, TCU
Speaker Dr. Helge Alsleben, TCU
Dr. Helge Alsleben is a structural geologist and Associate Professor in the School of Geology, Energy, and the Environment at TCU. Helge is a native of Germany and holds a B.S. equivalent from the University of Hamburg, Germany, a M.S. in geology from San Jose State University in San Jose, ...

Dr. Helge Alsleben is a structural geologist and Associate Professor in the School of Geology, Energy, and the Environment at TCU. Helge is a native of Germany and holds a B.S. equivalent from the University of Hamburg, Germany, a M.S. in geology from San Jose State University in San Jose, California, and a Ph.D. in geology from the University of Southern California in Los Angeles, California. He teaches undergraduate and graduate courses in “Structural Geology”, “Global Tectonics and Basin Analysis” and “Geomechanics”. He is primarily a field-oriented geologist with a background in strain analyses as well as structural and microstructural analyses of rocks. His academic expertise about stress and strain provides the theoretical background for applied geomechanical problems that are part of his current research interests. He has authored or co-authored numerous publications and regularly presents his research results at regional, national, and international conferences. He is a member of AAPG, AGU, and GSA.

Full Description

When?

Tue, Oct. 15, 2013
11:30 a.m. - 1 p.m.
(GMT-0500) US/Central

Event has ended

Where?

Midland Center
105 N. Main Street
Midland, TX 79701