Torbanite, also known as boghead coal, is a variety of fine-grained black oil shale. It usually occurs as lenticular masses, often associated with deposits of Permian coals. Torbanite is classified as lacustrine type oil shale.
Torbanite is named after Torbane Hill near Bathgate in Scotland, its main location of occurrence. Other major deposits of torbanite are found in Pennsylvania and Illinois, USA, in the Transvaal of South Africa, in the Sydney Basin, New South Wales, Australia, the largest deposit of which is located at Glen Davis, and in Nova Scotia, Canada.
Organic matter (telalginite) in torbanite is derived from lipid-rich microscopic plant remains similar in appearance to the fresh-water colonial green alga Botryococcus braunii. This evidence and extracellular hydrocarbons produced by the alga have led scientists to examine the alga as a source of Permian torbanites and a possible producer of biofuels. Torbanite consists of subordinate amounts of vitrinite and inertinite; however, their occurrence vary depending of deposits.
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