- Abstract:
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The Port Askaig Formation (PAF) is a diamictite-bearing succession in the Dalradian Supergroup of Scotland that provides an excellent archive of a Cryogenian glaciation in the Garvellach Islands and Islay, Argyll. The formation is ~1100 m thick, comprises 5 members and includes 47 diamictite beds, interbedded with siltstones, dolostones and sandstones. Here we document seven features of the PAF that indicate its relative stratigraphic completeness. There are gradual, progressive changes up-se...
Expand abstract - Publication status:
- Published
- Peer review status:
- Peer reviewed
- Version:
- Accepted Manuscript
- Files:
-
-
(pdf, 205.2KB)
-
- Publisher copy:
- 10.1016/j.precamres.2017.12.005
-
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- Publisher:
- Elsevier Publisher's website
- Journal:
- Precambrian Research Journal website
- Volume:
- 319
- Pages:
- 65-78
- Publication date:
- 2017-12-05
- Acceptance date:
- 2017-12-03
- DOI:
- ISSN:
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0301-9268
- Pubs id:
-
pubs:812795
- URN:
-
uri:b2b09adb-5c72-41dc-a12d-c8b4b132d788
- UUID:
-
uuid:b2b09adb-5c72-41dc-a12d-c8b4b132d788
- Local pid:
- pubs:812795
- Copyright holder:
- Elsevier B.V.
- Copyright date:
- 2017
- Notes:
-
Copyright © 2017 Elsevier B.V. This is the accepted manuscript version of the article. The final version is available online from Elsevier at: https://doi.org/10.1016/j.precamres.2017.12.005
Journal article
Indicators of relative completeness of the glacial record of the Port Askaig Formation, Garvellach Islands, Scotland
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