--> Abstract: Black Shale Diagenesis: Insights from Integrated High-Definition Analyses of Post-Mature Marcellus Formation Rocks, Northeastern Pennsylvania, by Christopher D. Laughrey, Herman Lemmens, Tim E. Ruble, Jaime Kostelnik, and Greg Walker; #90124 (2011)

Datapages, Inc.Print this page

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

Black Shale Diagenesis: Insights from Integrated High-Definition Analyses of Post-Mature Marcellus Formation Rocks, Northeastern Pennsylvania

Christopher D. Laughrey1; Herman Lemmens2; Tim E. Ruble1; Jaime Kostelnik3; Greg Walker1

(1) Weatherford Laboratories, Golden, CO.

(2) FEI Company, Eindhoven, Netherlands.

(3) Pennsylvania Geological Survey, Pittsburgh, PA.

Thermogenic shale-gas produced from the Marcellus Formation in northeastern Pennsylvania is post-mature. The reservoirs reached maximum burial temperatures characteristic of prehnite facies low-grade metamorphism. Although methane can be generated and remain stable under these conditions, this degree of burial diagenesis raises critical questions regarding metagenesis and reservoir quality. Late diagenesis implicates compaction, cementation, redox reactions involving formation fluids and transition metals, water loss, and dissolution/re-precipitation processes that may enhance or diminish reservoir potential.

Using a suite of high-resolution analytical techniques, we examined selected core samples from Sullivan County, Pennsylvania to characterize the reservoir and develop a diagenetic history of the Marcellus Formation in the region. The organic-rich intervals in these samples comprise mostly quartz, illite, and calcite. Quartz occurs as detrital silt, authigenic overgrowths, cryptocrystalline replacement of allochems, pore-filling microquartz and megaquartz, and patchy sheets of silica platelets. Illite occurs as crenulated detrital platelets and authigenic clay. The mean illite crystallite thickness is 211Å and the average Kübler index is 0.428 confirming the shales reached the low anchizone prehnite-pumpellyte metamorphic facies. Calcite occurs as crystalline spar replacing allochems and filling fossil molds, as crystals dispersed in clay and organic matrix, and as discontinuous parallel laminations of microspar. Additional minerals include anhydrite, plagioclase, illite-smectite, chlorite, pyrite, and graphite. Whole pattern fitting and Reitveld refinement quantify the abundance of graphite.

TOC ranges from 0.6 to 11 wt. percent. The original kerogen was mostly Type II. Microscopy and 3D modeling show that pyrobitumen comprises a significant volume of the rocks. Most porosity in the Marcellus is associated with this graphitic pyrobitumen.

Early diagenesis of Marcellus sediments involved mechanical compaction and dewatering of muds during burial to approximately 500 m. Chemical compaction at greater burial depths was dominated by quartz cementation and clay mineral transformations. Organic porosity developed during late catagenesis and continued on into metagenesis at depths greater than 8 km where storage capacity continued to evolve within a graphitic pyrobitumen matrix.