Observational and theoretical studies of the dynamics of mantle plume–mid‐ocean ridge interaction
Hot spot–mid‐ocean ridge interactions cause many of the largest structural and chemical
anomalies in Earth's ocean basins. Correlated geophysical and geochemical anomalies are …
anomalies in Earth's ocean basins. Correlated geophysical and geochemical anomalies are …
13 million years of seafloor spreading throughout the Red Sea Basin
The crustal and tectonic structure of the Red Sea and especially the maximum northward
extent of the (ultra) slow Red Sea spreading centre has been debated—mainly due to a lack …
extent of the (ultra) slow Red Sea spreading centre has been debated—mainly due to a lack …
A catalogue of deep mantle plumes: New results from finite‐frequency tomography
R Montelli, G Nolet, FA Dahlen… - Geochemistry …, 2006 - Wiley Online Library
New finite‐frequency tomographic images of S‐wave velocity confirm the existence of deep
mantle plumes below a large number of known hot spots. We compare S‐anomaly images …
mantle plumes below a large number of known hot spots. We compare S‐anomaly images …
Mid-Cenozoic post-breakup deformation in the 'passive'margins bordering the Norwegian–Greenland Sea
E Lundin, AG Doré - Marine and Petroleum Geology, 2002 - Elsevier
Since the initial breakup of the Norwegian–Greenland Sea in Early Eocene time (Chron
24B, 53.7 Ma), the conjugate 'passive'margins have been subject to compression, extension …
24B, 53.7 Ma), the conjugate 'passive'margins have been subject to compression, extension …
[LIVRE][B] Iceland geodynamics: crustal deformation and divergent plate tectonics
F Sigmundsson - 2006 - books.google.com
This book provides a summary of geodynamic results from Iceland that presently are found
in a great number of scientific articles, but have not been collected before in a book. The …
in a great number of scientific articles, but have not been collected before in a book. The …
Combined trace element and Pb-Nd–Sr-O isotope evidence for recycled oceanic crust (upper and lower) in the Iceland mantle plume
We present the results of a comprehensive major element, trace element and Sr–Nd–Pb–O
isotopic study of post-glacial volcanic rocks from the Neovolcanic zones on Iceland. The …
isotopic study of post-glacial volcanic rocks from the Neovolcanic zones on Iceland. The …
Neogene overflow of northern component water at the Greenland‐Scotland Ridge
HR Poore, R Samworth, NJ White… - Geochemistry …, 2006 - Wiley Online Library
In the North Atlantic Ocean, flow of North Atlantic Deep Water (NADW), and of its ancient
counterpart Northern Component Water (NCW), across the Greenland‐Scotland Ridge …
counterpart Northern Component Water (NCW), across the Greenland‐Scotland Ridge …
Transient convective uplift of an ancient buried landscape
Sedimentary basins in the North Atlantic Ocean preserve a record of intermittent uplift during
Cenozoic times 1. These variations in elevation are thought to result from temperature …
Cenozoic times 1. These variations in elevation are thought to result from temperature …
Interaction between the Mid‐Atlantic Ridge and the Azores hot spot during the last 85 Myr: Emplacement and rifting of the hot spot‐derived plateaus
P Gente, J Dyment, M Maia… - Geochemistry, Geophysics …, 2003 - Wiley Online Library
Multiple‐and single‐beam bathymetric data are compiled over the Azores plateau to
produce a 1 km× 1 km grid between latitudes 32° N and 49° N and longitudes 22° W and …
produce a 1 km× 1 km grid between latitudes 32° N and 49° N and longitudes 22° W and …
Exploring the combined role of eustasy and oceanic island thermal subsidence in sha** biodiversity on the Galápagos
Aim We constructed a series of high‐resolution palaeogeographical models for the
Galápagos archipelago for the last 700 kyr, accommodating thermal subsidence of the …
Galápagos archipelago for the last 700 kyr, accommodating thermal subsidence of the …