Rare earth geochemistry of Arenig cherts from the Ballantrae Ophiolite and Leadhills Imbricate Zone, southern Scotland: implications for origin and significance to the Caledonian Orogeny-Reference-Cited by-同舟云学术

Rare earth geochemistry of Arenig cherts from the Ballantrae Ophiolite and Leadhills Imbricate Zone, southern Scotland: implications for origin and significance to the Caledonian Orogeny

Published:1999-05 Issue:3 Volume:156 Page:549-560
ISSN:0016-7649
Container-title:Journal of the Geological Society
language:en
Short-container-title:Journal of the Geological Society

Author:

ARMSTRONG H. A.,OWEN A. W.,FLOYD J. D.

Publisher

Geological Society of London

Subject

Geology

Reference62 articles.

1. A Lower Ordovician (Arenig) radiolarian fauna from the Ballantrae Complex, Scotland;Aitchischon;Scottish Journal of Geology,1988

2. Conodonts from the Shinnel Formation, Tweeddale Member (middle Ordovician), Southern Uplands, Scotland;Armstrong;Palaeontology,1997

3. Armstrong H.A. Dean M.T. (1996) Conodonts from Ruddenleys, Lamancha and Crawford, Southern Uplands, Scotland. British Geological Survey Technical Report WH 96/192 R.

4. A new Lower Ordovician conodont faunule from the Northern Belt of the Southern Uplands

5. Evolution of the Northern Belt, Southern Uplands: implications for the Southern Uplands controversy

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