--> Abstract: My Source Rock Is Now My Shale-Gas Reservoir-Characterization of Organic-Rich Rocks, by Quinn R. Passey, Kevin Bohacs, Robert E. Klimentidis, William L. Esch, and Somnath Sinha; #90124 (2011)

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Making the Next Giant Leap in Geosciences
April 10-13, 2011, Houston, Texas, USA

My Source Rock Is Now My Shale-Gas Reservoir-Characterization of Organic-Rich Rocks

Quinn R. Passey1; Kevin Bohacs1; Robert E. Klimentidis1; William L. Esch2; Somnath Sinha1

(1) ExxonMobil Upstream Research Co., Houston, TX.

(2) ExxonMobil Exploration Co., Houston, TX.

Many currently producing shale-gas reservoirs are overmature oil-prone source rocks containing Type I or Type II kerogen. Recent studies indicate that although organic-rich shale-gas formations may be hundreds of meters in gross thickness (and may appear largely homogeneous), the vertical variability in the organic richness and mineralogy can vary on relatively short vertical scales. The vertical heterogeneity observed can be directly tied back to geologic and biotic conditions when deposited. The accumulation of organic-rich rocks is a complex function of many interacting processes that can be summarized by three main control variables: rate of production, rate of destruction, and rate of dilution. The marine realm includes three physiographic settings that accumulate significant organic-matter-rich rocks: constructional shelf margin, platform/ramp, and continental slope/basin. In general, the fundamental geologic building block of shale-gas reservoirs is the parasequence, or its equivalent, and commonly 10’s to 100’s of parasequences comprise the organic-rich formation whose lateral continuity can be estimated using techniques and models developed for source rocks. Many geochemical and petrophysical techniques developed to characterize organic-rich source rocks in the oil-generation window, can be applied, sometimes with modification, to shale-gas reservoirs that currently exhibit high thermal maturity. Well logs can be used to calculate TOC, porosity, and hydrocarbon saturation, but in clay-rich mudstones, the fundamental definition of porosity is complicated by the high surface area of clay minerals (external and sometimes internal), the volume of surface water, and the presence of water held by capillary forces in very small pores between silt and clay size mineral grains. Moreover, SEM images of ion-beam-milled samples reveal a separate nano-porosity system contained within the organic matter, and the gas may be largely contained in these organic pores. The use of high-vertical resolution standard logs and borehole image logs enhances the interpretation of vertically heterogenous shale-gas formations. It is important to keep in mind that kerogen occupies a much larger volume percent (vol%) than is indicated by the TOC weight percent (wt%); this is because of the low grain density of the organic matter compared to that of common rock-forming minerals. Well logs play a critical role in characterizing and quantifying shale-gas resources.