Maturation of lower palaeozoic kerogens from North Greenland

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Maturation of lower palaeozoic kerogens from North Greenland. / Bender Koch, C.

I: Organic Geochemistry, Bind 20, Nr. 3, 04.1993, s. 405-413.

Publikation: Bidrag til tidsskrift › Tidsskriftartikel › Forskning › fagfællebedømt

Harvard

Bender Koch, C 1993, 'Maturation of lower palaeozoic kerogens from North Greenland', Organic Geochemistry, bind 20, nr. 3, s. 405-413. https://doi.org/10.1016/0146-6380(93)90128-X

APA

Bender Koch, C. (1993). Maturation of lower palaeozoic kerogens from North Greenland. Organic Geochemistry, 20(3), 405-413. https://doi.org/10.1016/0146-6380(93)90128-X

Vancouver

Bender Koch C. Maturation of lower palaeozoic kerogens from North Greenland. Organic Geochemistry. 1993 apr.;20(3):405-413. https://doi.org/10.1016/0146-6380(93)90128-X

Author

Bender Koch, C. / Maturation of lower palaeozoic kerogens from North Greenland. I: Organic Geochemistry. 1993 ; Bind 20, Nr. 3. s. 405-413.

Bibtex

@article{630b36a11d304e9190d6af73bb61269a,
title = "Maturation of lower palaeozoic kerogens from North Greenland",
abstract = "Kerogen from Cambrian and Silurian sedimentary rocks (immature to postmature) from North Greenland has been studied by elemental analyses (C and H), X-ray diffraction (XRD) and infrared spectroscopy (i.r.). The change in the kerogen's structure [derived from the width of half height (WHH) of the (002) diffraction] and the content of functional groups (from characteristic absorption bands in the infrared spectra) suggest the following main processes of maturation: elimination of aliphatic CH2, CH3 groups (mature zone): elimination of aromatic CH groups [postmature (catagenesis) zone] and rearrangement of C ≠ C bonds [postmature (metagenesis) zone]. The maturity parameters derived from X-ray diffraction (WHH) and infrared spectroscopy (CH/CC-aliphatic/aromatic ratio) are applicable for maturity ranking in the mature to postmature (catagenesis) zones.",
keywords = "kerogen, Lower Palaeozoic, maturation, North Greenland",
author = "{Bender Koch}, C.",
year = "1993",
month = apr,
doi = "10.1016/0146-6380(93)90128-X",
language = "English",
volume = "20",
pages = "405--413",
journal = "Organic Geochemistry",
issn = "0146-6380",
publisher = "Pergamon Press",
number = "3",

}

RIS

TY - JOUR

T1 - Maturation of lower palaeozoic kerogens from North Greenland

AU - Bender Koch, C.

PY - 1993/4

Y1 - 1993/4

N2 - Kerogen from Cambrian and Silurian sedimentary rocks (immature to postmature) from North Greenland has been studied by elemental analyses (C and H), X-ray diffraction (XRD) and infrared spectroscopy (i.r.). The change in the kerogen's structure [derived from the width of half height (WHH) of the (002) diffraction] and the content of functional groups (from characteristic absorption bands in the infrared spectra) suggest the following main processes of maturation: elimination of aliphatic CH2, CH3 groups (mature zone): elimination of aromatic CH groups [postmature (catagenesis) zone] and rearrangement of C ≠ C bonds [postmature (metagenesis) zone]. The maturity parameters derived from X-ray diffraction (WHH) and infrared spectroscopy (CH/CC-aliphatic/aromatic ratio) are applicable for maturity ranking in the mature to postmature (catagenesis) zones.

AB - Kerogen from Cambrian and Silurian sedimentary rocks (immature to postmature) from North Greenland has been studied by elemental analyses (C and H), X-ray diffraction (XRD) and infrared spectroscopy (i.r.). The change in the kerogen's structure [derived from the width of half height (WHH) of the (002) diffraction] and the content of functional groups (from characteristic absorption bands in the infrared spectra) suggest the following main processes of maturation: elimination of aliphatic CH2, CH3 groups (mature zone): elimination of aromatic CH groups [postmature (catagenesis) zone] and rearrangement of C ≠ C bonds [postmature (metagenesis) zone]. The maturity parameters derived from X-ray diffraction (WHH) and infrared spectroscopy (CH/CC-aliphatic/aromatic ratio) are applicable for maturity ranking in the mature to postmature (catagenesis) zones.

KW - kerogen

KW - Lower Palaeozoic

KW - maturation

KW - North Greenland

UR - http://www.scopus.com/inward/record.url?scp=0027334596&partnerID=8YFLogxK

U2 - 10.1016/0146-6380(93)90128-X

DO - 10.1016/0146-6380(93)90128-X

M3 - Journal article

AN - SCOPUS:0027334596

VL - 20

SP - 405

EP - 413

JO - Organic Geochemistry

JF - Organic Geochemistry

SN - 0146-6380

IS - 3

ER -

ID: 240010261