Graphitization during high-grade metamorphism in the southern Bohemian Massif

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Graphitization during high-grade metamorphism in the southern Bohemian Massif. / Rantitsch, Gerd; Linner, Manfred.
In: International journal of coal geology, Vol. 248.2021, No. 1 December, 103864, 01.12.2021.

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Rantitsch G, Linner M. Graphitization during high-grade metamorphism in the southern Bohemian Massif. International journal of coal geology. 2021 Dec 1;248.2021(1 December):103864. Epub 2021 Oct 8. doi: 10.1016/j.coal.2021.103864

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@article{28726cbeb3ac49128431c50dd0a9e915,
title = "Graphitization during high-grade metamorphism in the southern Bohemian Massif",
abstract = "Raman spectroscopy on carbonaceous matter reconstructs the progressive path of graphitization during granulite facies metamorphism in the Variscan collisional belt of the southern Bohemian Massif. In this area, heating to 650–750 °C gradually altered the graphite microstructure, attributed to a metamorphic field gradient. Late low-pressure and high-temperature metamorphism at temperatures above 800 °C as well as advective heat transport due to rising granulite diapirs improved the graphite lattice ordering significantly. Numerical parameters derived from the Raman spectra of carbonaceous matter, in particular the G-band width and the S2-band dispersion map metamorphic field gradients in high-grade metamorphic terrains.",
author = "Gerd Rantitsch and Manfred Linner",
note = "Publisher Copyright: {\textcopyright} 2021 The Authors",
year = "2021",
month = dec,
day = "1",
doi = "10.1016/j.coal.2021.103864",
language = "English",
volume = "248.2021",
journal = "International journal of coal geology",
issn = "0166-5162",
publisher = "Elsevier",
number = "1 December",

}

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TY - JOUR

T1 - Graphitization during high-grade metamorphism in the southern Bohemian Massif

AU - Rantitsch, Gerd

AU - Linner, Manfred

N1 - Publisher Copyright: © 2021 The Authors

PY - 2021/12/1

Y1 - 2021/12/1

N2 - Raman spectroscopy on carbonaceous matter reconstructs the progressive path of graphitization during granulite facies metamorphism in the Variscan collisional belt of the southern Bohemian Massif. In this area, heating to 650–750 °C gradually altered the graphite microstructure, attributed to a metamorphic field gradient. Late low-pressure and high-temperature metamorphism at temperatures above 800 °C as well as advective heat transport due to rising granulite diapirs improved the graphite lattice ordering significantly. Numerical parameters derived from the Raman spectra of carbonaceous matter, in particular the G-band width and the S2-band dispersion map metamorphic field gradients in high-grade metamorphic terrains.

AB - Raman spectroscopy on carbonaceous matter reconstructs the progressive path of graphitization during granulite facies metamorphism in the Variscan collisional belt of the southern Bohemian Massif. In this area, heating to 650–750 °C gradually altered the graphite microstructure, attributed to a metamorphic field gradient. Late low-pressure and high-temperature metamorphism at temperatures above 800 °C as well as advective heat transport due to rising granulite diapirs improved the graphite lattice ordering significantly. Numerical parameters derived from the Raman spectra of carbonaceous matter, in particular the G-band width and the S2-band dispersion map metamorphic field gradients in high-grade metamorphic terrains.

UR - http://www.scopus.com/inward/record.url?scp=85117137028&partnerID=8YFLogxK

U2 - 10.1016/j.coal.2021.103864

DO - 10.1016/j.coal.2021.103864

M3 - Article

VL - 248.2021

JO - International journal of coal geology

JF - International journal of coal geology

SN - 0166-5162

IS - 1 December

M1 - 103864

ER -