Haynesville Shale - Lithology of Haynesville Shale

Lithology of Haynesville Shale

The Haynesville Shale is a lithologically heterogeneous, often organic-rich, mudstone. The composition of these mudstones varies greatly depending on position on geographic location and stratigraphic position. They vary from calcareous mudstone near the carbonate platforms and islands to argillaceous mudstone in areas where submarine fans prograded into the basin and diluted organic matter For example, the Haynesville Shale has been observed to vary in composition from 25 to 35 percent clay and 5 to 30 percent calcite in samples recovered from one oil and gas well. In that well, the Haynesville Shale consists of silty, argillaceous mudstones, silty, calcareous mudstones, and dolomitic mudstones and dolostones. The silty, argillaceous mudstones contain more than 30% silt-sized siliceous grains. The silt often occurs as laminations within these mudstones. In addition, the argillaceous matrix of such mudstones frequently contains numerous calcareous particles and stringers. The calcareous particles include coccoliths, bivalve, and gastropod fragments, and calcispheres. Organic matter in the form of amorphous kerogen coats the argillaceous material. Silty, calcareous mudstones contain more than 20% calcite. In these mudstones, the calcite occurs as silt-sized microfossil hash composed of fragmented fossils and carbonate mud. Where organic matter is low and silts are rare, the calcareous microfossil and carbonate mud has recrystallized. Possibly, further alteration of silty, calcareous mudstones has resulted in the formation of the dolomitic mudstones and dolostones. Both the silty, argillaceous mudstones and silty, calcareous mudstones often exhibit sparse to abundant, laminated pelletal fabrics.

The Haynesville Formation consists of marine and coastal plain limestone, shale, mudstone, and sandstone. In addition to the Haynesville Shale, the Haynesville Formation contains two formal subdivisions, which geologists call members. They are the Gilmer Limestone, also informally known as the Cotton Valley Limestone, and Buckner Anhydrite members. The Gilmer Limestone and Buckner Anhydrite members represent coastal and shallow marine deposits, which form along northern boundary of the basin in which the Haynesville Shale accumulated and separate it from contemporaneous undifferentiated nonmarine deposits that occur beneath Arkansas further north. In addition, the Gilmer Limestone member also represents a carbonate platform with oolite shoals that lie beneath central Upshur and western Smith counties, Texas. They comprise the western boundary of the ancient shelf basin within which Haynesville Shale accumulated. A third, informal member, which called the "Gray sandstone," of the Haynesville Formation interfingers with Haynesville Shale along its northern edge. This sandstone is regarded as having accumulated as submarine fans carrying sediment from the coastline into the basin within which the Haynesville Shale accumulated.