Iceland Within the Northern Atlantic, Volume 1

Iceland Within the Northern Atlantic, Volume 1
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The volcanic island of Iceland is a unique geological place due both to its position in the middle of the Atlantic Ocean and its repeated glaciations. It has been an accurate recorder of geodynamic and regional climatic evolutions for at least the last 15 million years.<br /><br />This book traces the history of Iceland, which is linked to the opening of the North Atlantic and the reactivation of the ancient suture of the Iapetus Ocean. It gives a view of climate evolution that is partly controlled by the dynamics of the ocean floor and analyzes the movement of the Jan Mayen tectonic plate and the progressive insularization of the Greenland–Faroe Ridge, which gave birth to Iceland. It also tries to understand the formation and migration of the deep Iceland hotspot and the lava flows that have, for millions of years, shaped this island.<br /><br />This book brings together the internal and external geodynamics of our planet to understand how Iceland functions and its role as a recorder of the paleoclimatic evolution of the Northern Hemisphere.

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Группа авторов. Iceland Within the Northern Atlantic, Volume 1

Table of Contents

List of Illustrations

List of Tables

Guide

Pages

Iceland Within the Northern Atlantic 1. Geodynamics and Tectonics

List of Abbreviations

A

B

C

D

E

F

G

H

I

J

K

L

M

N

O

R

S

T

U

W

Preface

Introduction

1. Iceland, in the Lineage of Two Oceans

1.1. Geographic and geodynamic context

1.2. Components of the North Atlantic domain

1.2.1. The Mid-Atlantic Ridge

1.2.2. The North Atlantic Igneous Province

1.2.3. The Icelandic hot spot

1.2.4. The Greenland–Iceland–Faroe Ridge

1.3. Geodynamic characteristics of Iceland

1.3.1. Seismicity

1.3.2. Icelandic volcanism

1.3.3. Eustatism and the Icelandic glaciers

1.4. References

2. Iceland, an Emerging Ocean Rift

2.1. Mid-Atlantic Ridge and Icelandic hot spot interactions

2.2. Present-day deformations in Iceland

2.2.1. Seismicity

2.2.1.1. Seismicity of volcanic zones

2.2.1.2. Seismicity and tectonics

2.2.1.2.1. Seismicity of the TFZ

2.2.1.2.2. Seismicity of the SISZ and Reykjanes Peninsula

2.2.1.3. Interaction between glaciation, tectonics and seismicity

2.2.2. Motions at plate boundaries

2.3. Iceland’s main structural features

2.3.1. The paleo-rifts and the active rift. 2.3.1.1. The paleo-rifts

2.3.1.2. The active volcanic zones

2.3.1.2.1. Meaning of “flank zones”

2.3.1.2.2. Special features of the active rift

2.3.1.2.3. Structures of the active rift

2.3.2. The transform zones

2.3.2.1. The Tjörnes Fracture Zone

2.3.2.1.1. Lineaments of the TFZ

2.3.2.1.2. Deformation partitioning in the TFZ

2.3.2.2. The South Iceland Seismic Zone

2.3.2.2.1. Structures of the SISZ

2.3.2.2.2. Historical seismic faults

2.3.2.2.3. Models for the SISZ

2.3.2.3. Comparison of the two transform zones in terms of geometry and stress state

2.4. Geothermal energy and hydrothermalism. 2.4.1. Geothermal systems

2.4.2. Geysers and hydrothermalism

2.5. References

3. Iceland, a Legacy of North Atlantic History

3.1. Bathymetry of the Northeast Atlantic domain and geoid anomalies

3.2. The North Atlantic and the continental breakup of Laurussia

3.2.1. Passive margins and large igneous provinces

3.2.2. The early beginnings of the opening of the North Atlantic Ocean. 3.2.2.1. Magnetic anomalies, magnetochrons and types of lithosphere

3.2.2.2. Evolution in West Greenland

3.2.2.3. Evolution in East Greenland: a mobile region since the Paleozoic

3.2.3. Thulean magmatism in the Paleocene and the continental breakup of the Northeast Atlantic. 3.2.3.1. Thulean traps

3.2.3.2. Paleogene syn-magmatic breakup

3.2.4. Chronology and kinematics of the opening of the Northeast Atlantic. 3.2.4.1. Age of onset of oceanization in the northeast Atlantic

3.2.4.2. The ocean basins of the Northeast Atlantic

3.2.4.3. The Reykjanes Basin in Southern Iceland

3.2.4.4. The GIFR ridge

3.2.4.5. The extinct Ægir Ridge

3.2.4.6. The Jan Mayen microcontinent and the Kolbeinsey Basin

3.2.5. The Northeast Atlantic region: mantle plume or not?

3.2.5.1. The Icelandic hot spot

3.2.5.2. The mantle plume hypothesis

3.2.5.3. Arguments against the mantle plume model

3.3. The origin of Iceland. 3.3.1. The anomalous crust of the GIFR ridge and the deep structure of Iceland

3.3.2. Icelandic SDRs

3.3.3. Interpretations of GIFR and Iceland

3.3.3.1. The pattern of plate movement over a hot spot

3.3.3.2. A continental axis stretched between Greenland and Europe?

3.4. References

Conclusion

A long and complex history

Plume or no plume, that is the question

An oceanic rift with special characteristics

A still mysterious island

References. Key books

Articles, documents and key theses

Websites

List of Authors

Index. A, B

C

D

E

F

G

H

I

K, L

M

N, O

P

Q, R

S

T

U, V, W

Summary of Volume 2

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Geoscience, Field Director – Yves Lagabrielle Lithosphere-Asthenosphere Interactions, Subject Head – René Maury

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The development of radiometric dating (section 2.4 of Volume 2) allowed us to better constrain both the chronology of the progressive extinction of the paleorifts and also that of the glaciations with respect to the tectonic and paleo-oceanographic evolution of the North Atlantic. The impact of the glacial loading of rifts during periods of extended ice caps could explain pro parte this cyclic evolution linked to rift-jump.

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