𝔖 Bobbio Scriptorium
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Porosity of bituminous coals

Book ID
104276406
Publisher
Elsevier Science
Year
2002
Weight
155 KB
Volume
43
Category
Article
ISSN
0140-6701

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✦ Synopsis

occurrence of weak autoxidation processes has been observed in the coal seam at a depth from 3 to 5 m. Mierinite whose percentage is relatively high has been formed as a result of high temperature processes that take place in the peat. The higher amount of imerinite macerals predetermines the higher oxidative stability of this coal.

02/01272 Peculiarities of gas content and metamorphic changes in coals in the southwest coal region of the Lvov-Volyn Basin

Kruglova, R.L. Geol. Geokhim. Goryuch. Kopalin, 1999, 4, 70-75. (In Ukrainian) Methane content and metamorphism of coal, both regionally and in the stratigraphic section of coal seam, were studied. A close connection of the methane content with the coalification degree and coal depth was established.

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