Ordovician ocean plate stratigraphy and thrust duplexes of the Ballantrae Complex, SW Scotland: Implications for the pelagic deposition rate and forearc accretion in the closing Iapetus Ocean-Reference-Cited by-同舟云学术

Ordovician ocean plate stratigraphy and thrust duplexes of the Ballantrae Complex, SW Scotland: Implications for the pelagic deposition rate and forearc accretion in the closing Iapetus Ocean

Published:2015-11 Issue: Volume:662 Page:312-327
ISSN:0040-1951
Container-title:Tectonophysics
language:en
Short-container-title:Tectonophysics

Author:

Fujisaki Wataru,Asanuma Hisashi,Suzuki Kazue,Sawaki Yusuke,Sakata Shuhei,Hirata Takafumi,Maruyama Shigenori,Windley Brian F.

Funder

Ministry of Education, Culture, Sports, Science and Technology, Japan

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference67 articles.

1. A Lower Ordovician (Arenig) radiolarian fauna from the Ballantrae Complex, Scotland;Aitchison;Scott. J. Geol.,1998

2. 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;Armstrong;J. Geol. Soc. Lond.,1999

3. Comment on ‘Age and origin of Ballantrae ophiolite and its significance to the Caledonian orogeny and the Ordovician time scale’ by Bluck et al. (1980);Barrett;Geology,1982

4. Geology of a continental margin 1: the Ballantrae Complex;Bluck,1978

5. The Ballantrae Complex;Bluck,1992

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