GSA Annual Meeting in Seattle, Washington, USA - 2017

Paper No. 62-1
Presentation Time: 3:50 PM

STRUCTURAL DIAGENESIS OF NATURAL FRACTURES: IMPLICATIONS FOR WATER, ENERGY, ENVIRONMENT, AND HAZARDS


EICHHUBL, Peter, Bureau of Economic Geology, Jackson School of Geosciences, The University of Texas at Austin, 10100 Burnet Road, Austin, TX 78758 and LAUBACH, Stephen E., Bureau of Economic Geology, Jackson School of Geosciences, The University of Texas at Austin, University Station, P.O. Box X, Austin, TX 78713-8924, peter.eichhubl@beg.utexas.edu

Structural geology emerged as an applied geoscience discipline providing predictive tools in economic geology. Through the subsequent development of quantitative approaches and in conjunction with compositional and isotopic analytical tools, these techniques have provided fundamental insight into deformation processes that shaped our current understanding of global tectonic and planetary processes. A more recent development within this discipline is the close integration of brittle structural geology with low-temperature geochemistry. Among other advances, this structural-diagenetic workflow has enabled insight into coupled physical and chemical processes that control the formation of fractures in the upper crust and their flow properties, with relevance to crustal and basin-scale flow processes, groundwater resources, hydrocarbon exploration and production, CO2 sequestration, and the occurrence of natural and human-induced seismicity.

Recent work in structural diagenesis has shown that fracture opening and cementation are closely coupled processes, with chemical reactions influencing and in part controlling mechanical fracture opening, and physical fracture opening processes impeding or enhancing cement precipitation that reduces fracture flow. At the microscale, fracture opening processes control the rate and texture of fracture cement growth while host rock diagenetic processes control rate of fracture growth, with complex feedback loops among these coupled processes. At the nanoscale, solution and precipitation processes control the structure of grain boundary channels that provide pathways for fluid and mass transport in otherwise completely cemented fractures. Insight into these processes provides the basis for improved development strategies of conventional and unconventional oil and gas resources, with the aim of reducing the environmental impact associated with exploration and production including land and water resource utilization.