The Variation of Trace Elements in Steenkool Coal Formation, Bintuni Basin, West Papua, Indonesia
International Journal of Science and Research (IJSR)

International Journal of Science and Research (IJSR)
www.ijsr.net | Open Access | Fully Refereed | Peer Reviewed International Journal

ISSN: 2319-7064

Research Paper | Geology | Indonesia | Volume 6 Issue 12, December 2017

The Variation of Trace Elements in Steenkool Coal Formation, Bintuni Basin, West Papua, Indonesia

Ahmad Helman Hamdani, Johanes Hutabarat

This study analyses of trace elements distribution in coal samples from Steenkool Formation in Bintuni Basin, West Papua. The term, trace elements in coal, refers to as those elements with concentration below 0.1 wt. % (1, 000 ppm) in coal that are generally considered to be inorganic he ash content and depositional environment were controlling the amount of trace elements concentration. The trace elements, calcium and magnesium have the greatest organic affinities, whereas, Mn, Mg and Ca have affinities with the carbonates

Keywords: Trace element, ash contents, depositional environment, coal, Steenkool Formation, Bintuni basin

Edition: Volume 6 Issue 12, December 2017

Pages: 1367 - 1369

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How to Cite this Article?

Ahmad Helman Hamdani, Johanes Hutabarat, "The Variation of Trace Elements in Steenkool Coal Formation, Bintuni Basin, West Papua, Indonesia", International Journal of Science and Research (IJSR), https://www.ijsr.net/search_index_results_paperid.php?id=ART20178745, Volume 6 Issue 12, December 2017, 1367 - 1369

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