VEIN EVOLUTION DUE TO THERMAL MATURATION OF KEROGEN IN THE MARCELLUS SHALE
Preliminary data shows that at least two fracturing and filling events occurred. Crosscutting relationship shows that the first event formed relatively thick (~1 to 3.5 mm) mineralized calcite-filled veins followed by relatively thin (<1 mm) mineralized veinlets of assorted fill. Fracture morphologies were grouped based on angle to bedding and include horizontal, vertical (continuous and offset), oblique, and secondary veinlets. Calcite-fill morphology and the number of generations of fill varied. Horizontal veins formed first during kerogen catagenesis and contained only one generation of bladed-fibrous calcite. Vertical fractures formed later and contained up to five generations of mineralization made up of acicular-fibrous, large blocky, and small blocky crystals. Bitumen, of varying thickness (<1 to 5 mm) shows a relationship with fracture morphology.
Individual groups of fracture morphologies have their own unique combinations of vein morphology, number of mineralization episodes, and bitumen thickness, which provide insight into the evolution of self-induced fractures during maturation. Calcite-filled fracture intensity and morphology can have a strong influence on development of complex geometry during hydraulic fracture stimulation of horizontal laterals.