• Source: Torbanite

Torbanite, also known historically as boghead coal or kerosene shale, 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. A similar mineral, cannel coal, is classified as being a terrestrial form of oil shale, not a lacustrine type.
Torbanite is named after Torbane Hill near Bathgate in West Lothian, Scotland, a major location of occurrence. Torbanite found in Bathgate may have formations of bathvillite found within it. Historically, two other names have been used for torbanite. Boghead coal is named after Boghead estate, also near Bathgate in Scotland. In Australia, the historical name for torbanite was kerosene shale.
Other major deposits of torbanite are found in Pennsylvania and Illinois, US, in Mpumalanga Province in South Africa, in the Sydney Basin of 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 varies depending on deposits.
A rubber-like, elastic, highly-resilient bituminous substance, known as coorongite—classified as an organic-rich sediment and named after the Coorong where it was found—has been identified as a 'peat stage' in the formation of torbanite. It provides evidence of the lacustrine and algal origin of torbanite. Substances very similar to coorongite had other historical names, depending upon the location of the deposits, such as n'hangellite from Portuguese East African (now Mozambique) and marahunite from Brazil.
Torbanite typically comprises 88% carbon and 11% hydrogen. Paraffin oil can be distilled from some forms of torbanite, a process discovered and patented by James Young in 1851.




See also


Cannel coal
Kukersite
Lamosite
Marinite
Tasmanite
Oil shale geology




References

Kata Kunci Pencarian:

• Torbanite
• Stellarton
• Cannel coal
• Oil shale geology
• Kerosene
• James Young (chemist)
• Ermelo, South Africa
• Oil shale
• Oil industry in Scotland
• Second Industrial Revolution