Mineralogical characteristics of Suhostrel bituminous coal, SW Bulgaria

Author:

Zdravkov Alexander,Yanchev Denislav

Abstract

The mineralogical composition of the Suhostrel bituminous coal was studied using optical microscopy, XRD and SEM-EDS analyses. Clay minerals (mostly kaolinite and mica), quartz and locally albite, are the dominant minerals. Their characteristics indicate predominant terrigenous origin and together with a poor accessory mineral association (rutile/anatase, monazite, zircon) argue for a major detrital input from low grade metamorphic and weathered intrusive/pegmatitic rocks.

Publisher

Bulgarian Geological Society

Subject

General Medicine

Reference8 articles.

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2. Kortenski, J. 1988. Mineral and chemical composition of the inorganic component of the “Suchostrel” coal deposit. – Ann. High Inst. Min. Geol., 34, 297–309 (in Bulgarian with English and Russian abstracts).

3. Stefanov, Y., A. Chatalov. 2008a. Petrographic composition of the Paleogene clastic rocks from the Padesh Basin and provenance analysis. II. Provenance analysis. – Ann. Uni. Sofia, 101, 1-géol., 57–77 (in Bulgarian with English abstract).

4. Stefanov, Y., A. Chatalov. 2008b. Mineral composition of the clay fraction in the Paleogene shales from the Padesh Basin, southwestern Bulgaria – In: “60 Years Geology in the Sofia University “St. Kliment Ohridski”, 145–150 (in Bulgarian with English abstract).

5. Ward, C.R. 1989. Minerals in bituminous coals of the Sydney basin (Australia) and the Illinois basin (U.S.A.). – Int. J. Coal Geol., 13, 455–479; https://doi.org/10.1016/0166-5162(89)90104-3.

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