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Volumn 29, Issue 4, 1996, Pages 235-258

Origin and significance of high nickel and chromium concentrations in pliocene lignite of the Kosovo Basin, Serbia

Author keywords

[No Author keywords available]

Indexed keywords

AUTHIGENIC MINERAL; CHROMIUM; DETRITAL MINERAL; GEOCHEMISTRY; LIGNITE; NICKEL; PLIOCENE; PROVENANCE;

EID: 0029667685     PISSN: 01665162     EISSN: None     Source Type: Journal    
DOI: 10.1016/0166-5162(95)00031-3     Document Type: Article
Times cited : (64)

References (15)
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  • 3
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    • Trace metal analyses of fractions of a DMSO extract of Kosovo Basin coal
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  • 4
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    • R.W. Bryers and K.S. Vorres (Editors), Feb. 22-26, 1988
    • Djekic, S.V., 1988. Behavior of mineral matter in the coal of Kosovo, Yugoslavia, during the utility boiler combustion process. In: R.W. Bryers and K.S. Vorres (Editors), Mineral Matter and Ash Deposition from Coal. Engineering Foundational Conf. (Feb. 22-26), 1988, pp. 529-543.
    • (1988) Mineral Matter and Ash Deposition from Coal. Engineering Foundational Conf. , pp. 529-543
    • Djekic, S.V.1
  • 5
    • 0024530469 scopus 로고
    • Reconnaissance study of mineral matter and trace elements in greek lignites
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    • (1989) Chem. Geol. , vol.76 , pp. 107-130
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  • 7
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    • Lichte, F.E., Golightly, D.W. and Lamothe, P.J., 1987. Inductively coupled plasma-atomic emission spectrometry. In: P.A. Baedecker (Editor), Methods for Geochemical Analysis. US Geol. Surv. Bull., 1770: B1-B10.
    • (1987) US Geol. Surv. Bull. , vol.1770
    • Lichte, F.E.1    Golightly, D.W.2    Lamothe, P.J.3
  • 8
    • 0002398524 scopus 로고
    • β-kerolite-pimelite series from Goles Mountain, Yugoslavia
    • Jerusalem
    • Maksimović, Z., 1966. β-Kerolite-Pimelite series from Goles Mountain, Yugoslavia. Proc. Int. Clay Conf. (Jerusalem), Vol. 1, pp. 97-105.
    • (1966) Proc. Int. Clay Conf. , vol.1 , pp. 97-105
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  • 10
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    • Chromium and nickel
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  • 11
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    • Hidrotermalno-egzogena lezista silikatnih ruda nikla i kobalta glavice i cikatova
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  • 13
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* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.