| Title | Influence of igneous intrusions on thermal maturity and optical texture: comparison between a bituminous marl and a coal seam of the same maturity |
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| Author | Goodarzi, F; Gentzis, T; Grasby, S E ; Dewing, K |
| Source | International Journal of Coal Geology vol. 198, 2018 p. 183-197, https://doi.org/10.1016/j.coal.2018.09.013 |
| Image |  |
| Year | 2018 |
| Alt Series | Natural Resources Canada, Contribution Series 20180224 |
| Publisher | Elsevier BV |
| Document | serial |
| Lang. | English |
| Media | paper; on-line; digital |
| File format | pdf; html |
| Province | Nunavut; British Columbia |
| NTS | 93L/11; 49G; 49H; 340B |
| Area | Canadian Arctic Archipelago; Ellesmere Island; Fosheim Peninsula; Telkwa River |
| Lat/Long WENS | -88.0000 -80.0000 80.5000 79.0000 |
| Lat/Long WENS | -127.5000 -127.0000 54.7500 54.5000 |
| Subjects | fossil fuels; economic geology; geochemistry; tectonics; petroleum resources; petroleum generation; thermal maturation; coal seams; marls; bitumen; intrusions; dykes; thermal alteration; textural
analyses; microscopic analysis; pyrolysis; organic geochemistry; coke; hydrogen index; reflectance; hydrocarbon generation; petroleum occurrence; oil; metamorphism, contact; tectonic history; thermal history; chlorine; Sverdrup Basin; Murray Harbour
Formation; Hazelton Group; Bulkley Intrusion; Phanerozoic; Mesozoic; Cretaceous; Triassic |
| Illustrations | geoscientific sketch maps; stratigraphic columns; profiles; tables; photomicrographs; plots |
| Program | GEM2: Geo-mapping for Energy and Minerals Western Arctic, High Arctic LIP |
| Released | 2018 09 25 |
| Abstract | The impact of a 120 cm thick dike on dispersed organic matter in the Triassic Marry Harbour (MH) bituminous marl in the Raanes Peninsula, Ellesmere Island, Arctic Canada, was studied using reflected
light microscopy and Rock-Eval pyrolysis. Results were compared to a coal seam of similar maturity that was thermally altered by an igneous intrusion. The MH bituminous marl is mature and within the oil window (Ro=0.94%), whereas the coal is
high-volatile B bituminous rank (Ro=0.80%). Thermal alteration impacted differently the organic-rich marl than the coal seam. Most of the heat generated by the intrusive emplacement in contact with coal is spent transforming coal to coke in the
plastic layer/zone, similar to the process that coal undergoes in industrial coking operations. In contrast, the thermal alteration of sedimentary rocks occurs over longer distances as a result of the absence of a plastic layer/zone. The impact zone
of the 120 cm thick igneous intrusion was greater in the MH bituminous marl, which became thermally altered (Ro=2.34%) at 190 cm from the contact with the dike. On the contrary, the coal became thermally altered (%Ro=5.0%) by a 240 cm alkali-basalt
intrusion (twice the thickness of the MH dike) and its impact zone was only 65 cm. Heat and hot volatile matter produced by the thermal decomposition of organic matter and minerals (carbonate, dehydration of clay minerals) in contact with the igneous
intrusion body is transferred through the sedimentary rock matrix by convection through fractures. This transformation is evident by the occurrence of the pyrolytic carbon at various distances in the fractured MH marl from contact. The hydrogen index
(HI) shows a similar trend to that of the remaining source potential (S2). Both parameters decrease systematically toward the dike, and go through a minimum at 20 cm from the dike contact, as the indigenous organic matter is converted to hydrocarbons
or devolatilized. At the dike contact, both S2 and HI have higher values. These trends are similar to those of the volatile elements H and Cl in the intruded coal seam. The free hydrocarbons (S1) showed a slightly different trend than S2 and HI. It
increased initially from 300 cm and reached a maximum at about 190 cm from the dike contact before decreasing continually and reaching a minimum at 20 cm from the contact. At the dike contact, the S1 increased slightly, similar to the HI and S2. The
presence of oil droplets trapped in carbonate concretions, in combination with the highest value of oil expelled from the source rock (based on S1/TOC) at distance of 190 cm from dike, is an indication of the influence of contact metamorphism on oil
generation locally. Furthermore, it indicates that intrusion of igneous dikes into the bituminous MH marl resulted in an increase of organic matter maturation locally and in hydrocarbon generation. |
| Summary | (Plain Language Summary, not published)
This paper examines differences in styles of alteration in coal and oil shales adjacent to igneous sills. The alteration halo in coal is much less than
in oil shales. |
| GEOSCAN ID | 311305 |
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