untitled


Erratum for ‘Devonian (c. 388–375 Ma) Horn River Group of
Mackenzie Platform (NW Canada) is an open-shelf succession
recording oceanic anoxic events’, Journal of the Geological Society,
London, 176, 29-45

P. Kabanov
Geological Survey of Canada Calgary, Calgary, AB T2L 2A7, Canada

PK, 0000-0002-6289-5351
Correspondence: kabanovp@gmail.com

The original caption of Figure 3 did not list the section names
correctly. In the below figure, the numbering in 3a has been updated

and the caption contains the names of all of the sections. PC in 3b
has also been defined.

Figure 3. (a) Geographical spread of the Horn River Group (on NWT side) and Canol Formation (on Yukon side) between 64 and 68°N; crosses are
outcrops: (1, Trail River (TR in (b)); 2, Rumbly Creek; 3, Turnabout Creek; 4, Powell Creek, and 5, Prohibition Creek); palaeogeographic areas: WOB,
Western off-bank area; BAT, bank-and-trough area; SOB, southern off-bank area. (b) Cross-section (black line (a)) levelled at the top of Hume Formation;
wells from west to east: Cranswick YT A-42, Cranswick A-22, S. Ramparts I-77, N. Ramparts A-59, Ramparts River F-46, Hume River I-66, Hume River
D-53, Carcajou L-24, Maida Creek F-57, Hoosier F-27, NWB is Norman Wells oilfield, Little Bear N-09, Bluefish A-49, and Bracket Lake C-21.
Stratigraphic members in SOB: ( fc) Francis Creek, ( ps) Prohibition Creek, (vc) Vermillion Creek; (dc) Dodo Canyon, (ml) Mirror Lake, and (lc) Loon
Creek. NRTF is Norman Range thrust fault (other tectonic elements are not shown). The Canol Formation in WOB area is provisionally subdivided into (1)
lower, (2) middle, and (3) lower traceable units or information members (Cross-section B-B’ in supplementary material). (PC) on (b) is projection of the
Powell Creek outcrop (stratotype of Canol Formation).

© 2019 The Author(s). Published by The Geological Society of London. All rights reserved. For permissions: http://www.geolsoc.org.uk/permissions.
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Erratum Journal of the Geological Society

Published online December 20, 2019 https://doi.org/10.1144/jgs2019-205 | Vol. 177 | 2020 | p. 231

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