The impact of a Neogene basalt intrusion on the optical properties and internal structure of the dispersed organic matter in Carboniferous strata (SW-part USCB)

Adamczyk, Z.; Kokowska-Pawłowska, M.; Komorek, J.; Klupa, A.; Lewandowska, M.; Nowak, J.

doi:10.1515/agp-2018-0002

Artykuł - szczegóły

Tytuł artykułu

The impact of a Neogene basalt intrusion on the optical properties and internal structure of the dispersed organic matter in Carboniferous strata (SW-part USCB)

Autorzy

Adamczyk Z. , Kokowska-Pawłowska M. , Komorek J. , Klupa A. , Lewandowska M. , Nowak J.

Treść / Zawartość

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Identyfikatory

DOI

10.1515/agp-2018-0002

Warianty tytułu

Języki publikacji

Abstrakty

The S-7 borehole log from the Sumina area (USCB Poland) revealed the presence of three basaltic veins originating from a basalt dyke. Coal interlayers in the rocks surrounding the basaltic veins have been coked to form natural coke. Photometric measurements revealed that the optical properties of the studied natural coke samples are characteristic of semi-graphite (Rmax > 9%). The natural coke matrix of all of the analyzed samples has a biaxial negative optical character. Vitrinite in the examined natural coke samples is characterized by a lower optical anisotropy than that of the natural matrix and it has a biaxial positive optical character. Vitrinite in almost all samples taken at locations more distant from the intrusion has a biaxial positive optical character. A reversal of the changes of the true maximum vitrinite reflectance and bireflectance with changing distance from the second basaltic vein has been observed. The temperature regime that acted upon the dispersed organic matter located in the immediate vicinity of the intrusion, estimated on the basis of the selected experimental data, is suggested to be higher than 750°C.

Słowa kluczowe

optical properties natural coke neogenic intrusion carbonisation

właściwości optyczne koks naturalny intruzja neogeniczna karbonizacja

Wydawca

Faculty of Geology of the University of Warsaw
Komitet Nauk Geologicznych PAN

Czasopismo

Acta Geologica Polonica

Rocznik

2018

Tom

Vol. 68, no. 2

Strony

249--262

Opis fizyczny

Bibliogr. 78 poz., rys., tab.

Twórcy

autor

Adamczyk Z.

zdzislaw.adamczyk@polsl.pl

Silesian University of Technology, Faculty of Mining and Geology, Department of Applied Geology, Akademicka 2 Street, 44-100 Gliwice, Poland.

autor

Kokowska-Pawłowska M.

magdalena.kokowska-pawlowska@polsl.pl

Silesian University of Technology, Faculty of Mining and Geology, Department of Applied Geology, Akademicka 2 Street, 44-100 Gliwice, Poland

autor

Komorek J.

joanna.komorek@polsl.pl

Silesian University of Technology, Faculty of Mining and Geology, Department of Applied Geology, Akademicka 2 Street, 44-100 Gliwice, Poland

autor

Klupa A.

aklupa@gig.eu

Central Mining Institute, Plac Gwarków 140-166 Katowice, Poland

autor

Lewandowska M.

malgorzata.lewandowska@polsl.pl

Silesian University of Technology, Faculty of Mining and Geology, Department of Applied Geology, Akademicka 2 Street, 44-100 Gliwice, Poland

autor

Nowak J.

jacek.nowak@polsl.pl

Silesian University of Technology, Faculty of Mining and Geology, Department of Applied Geology, Akademicka 2 Street, 44-100 Gliwice, Poland

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Uwagi

Opracowanie rekordu w ramach umowy 509/P-DUN/2018 ze środków MNiSW przeznaczonych na działalność upowszechniającą naukę (2018).

Typ dokumentu

Bibliografia

Identyfikator YADDA

bwmeta1.element.baztech-52cd9373-b46b-4568-933d-01583606af3c