1997
DOI: 10.1016/s0166-5162(97)00010-4
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Properties of a lacustrine subbituminous (k1) seam, with special reference to the contact metamorphism, Soma-Turkey

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Cited by 59 publications
(33 citation statements)
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“…In general, the findings from the current study, which recognises carbonates, quartz and clays as the dominant minerals, are similar to those reported by Kisch and Taylor (1966), Podwysocki and Dutcher (1971), Ward et al (1989), Merritt (1990), Kwienciń-ska et al (1992), Karayigit and Whateley (1997), Querol et al (1997) and Finkelman et al (1998).…”
Section: Coal Mineralogysupporting
confidence: 92%
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“…In general, the findings from the current study, which recognises carbonates, quartz and clays as the dominant minerals, are similar to those reported by Kisch and Taylor (1966), Podwysocki and Dutcher (1971), Ward et al (1989), Merritt (1990), Kwienciń-ska et al (1992), Karayigit and Whateley (1997), Querol et al (1997) and Finkelman et al (1998).…”
Section: Coal Mineralogysupporting
confidence: 92%
“…Previous studies of the interaction between coal and igneous intrusions have recognised three to four zones based on coal geochemistry (Ward et al, 1989;Goodarzi and Cameron, 1990;Kwiencińska et al, 1992;Karayigit and Whateley, 1997). Variations in the chemistry of the coal approaching the intrusion in the drill core samples from Dartbrook indicate the presence of three zones (Fig.…”
Section: Geochemical Trends In Coalmentioning
confidence: 98%
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“…Golab (2003) and Golab and Carr (2004) used XRD analysis to show the mineralogy of the coal varies with distance from the fingers of the dyke with dawsonite, ankerite, quartz, albite, kaolinite, and mixed-layer clays dominant. Ankerite, albite, muscovite, siderite, and andalusite are restricted to the heated coal with the first The suite of minerals associated with the Dartbrook dykes and aureole, especially the carbonates, quartz and clay minerals have been consistently identified in other dyke-coal associations by other workers such as Kisch and Taylor (1966), Podwysocki and Dutcher (1971), Ward et al (1989), Merritt (1990), Kwiencińska et al (1992), Watkins (1996), Karayigit and Whateley (1997), Querol et al (1997) and Finkelman et al (1998).…”
Section: Roman Road Dykementioning
confidence: 88%
“…Despite high S and pyrite concentrations being common in marine-influenced coals, they are also reported from intermontane basins formed during the Alpine Orogenese in circum-Mediterranean mobile belts (e.g., Querol et al 1995;Karayigit and Whateley 1997;Markic and Sachsenhofer 1997;Taylor et al 1998;Siavalas et al 2009). It seems that sulphur-rich karstic aquifers supplied the palaeomire with freshwater causing neutral to alkaline conditions (Siavalas et al 2009).…”
Section: Palaeoenvironmental Reconstructionmentioning
confidence: 99%