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Gwenn Peron-Pinvidic
Continental Rifted Margins 2
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Table of Contents
List of Illustrations
Guide
Pages
Страница 6
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Страница 8
Страница 9
1
The West Iberian Margin: Past and Current Research Concepts and Future Challenges
1.1. Introduction: the West Iberian Margin, the “classic” magma-poor margin?
1.2. Structures of the West Iberian Margin
1.2.1.
The Deep Galicia Margin (DGM)
1.2.2.
The Southern Iberia Abyssal Plain (SIAP)
1.2.3.
Conjugated West Iberian and Newfoundland Margins
1.3. Synrift tectono-stratigraphy and age and evolution of extension across the West Iberian Margin
1.4. Current models of development of the West Iberian Margin
1.5. Remaining questions at the West Iberian Margin and other magmapoor margins
Question 1: how is the crust thinned from 20 km to zero km?
Question 2: what is the role of detachments in rifting to breakup and how do they develop?
Question 3: what is the evolution of the lithospheric rheology, strain distribution, melt production and serpentinization during rifting?
1.6. Conclusions and outlook
1.7. References
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