Oceanic residual depth measurements, the plate cooling model, and global dynamic topography
MJ Hoggard, J Winterbourne… - … Research: Solid Earth, 2017 - Wiley Online Library
Convective circulation of the mantle causes deflections of the Earth's surface that vary as a
function of space and time. Accurate measurements of this dynamic topography are …
function of space and time. Accurate measurements of this dynamic topography are …
NE Canada Rifted Margin Composite Tectono-Sedimentary Element, Baffin Bay, Davis Strait and Labrador Sea
Abstract The NE Canada Rifted Margin (NCRM) Composite Tectono-Sedimentary Element
(CTSE) developed during a long and complex history that produced two tectono …
(CTSE) developed during a long and complex history that produced two tectono …
Circum-Arctic Lithosphere Evolution (CALE) Transect C: displacement of the Arctic Alaska–Chukotka microplate towards the Pacific during opening of the Amerasia …
This paper synthesizes the framework and geological evolution of the Arctic Alaska–
Chukotka microplate (AACM), from its origin as part of the continental platform fringing …
Chukotka microplate (AACM), from its origin as part of the continental platform fringing …
Breakup volcanism and plate tectonics in the NW Atlantic
Passive margins are the locus of tectonic and magmatic processes leading to the formation
of highly variable along-strike and conjugate margins structures. Using extensive new …
of highly variable along-strike and conjugate margins structures. Using extensive new …
Crustal structure of Baffin Bay from constrained three-dimensional gravity inversion and deformable plate tectonic models
Mesozoic to Cenozoic continental rifting, breakup and spreading between North America
and Greenland led to the opening, from south to north, of the Labrador Sea and eventually …
and Greenland led to the opening, from south to north, of the Labrador Sea and eventually …
Evolution of Labrador Sea–Baffin Bay: plate or plume processes?
Breakup between Greenland and Canada resulted in oceanic spreading in the Labrador
Sea and Baffin Bay. These ocean basins are connected through the Davis Strait, a …
Sea and Baffin Bay. These ocean basins are connected through the Davis Strait, a …
[HTML][HTML] Shelf-break glaciation and an extensive ice shelf beyond northwest Greenland at the Last Glacial Maximum
CL Batchelor, DW Krawczyk, E O'Brien, J Mulder - Marine Geology, 2024 - Elsevier
The analysis of seafloor glacial landforms can provide important constraints on the past
behaviour of ice sheets, including their extent at the Last Glacial Maximum and the controls …
behaviour of ice sheets, including their extent at the Last Glacial Maximum and the controls …
[PDF][PDF] Tectonostratigraphy and evolution of the West Greenland continental margin.
U Gregersen, PC Knutz, H Nøhr-Hansen… - Bulletin of the …, 2019 - researchgate.net
Large structural highs and sedimentary basins are identified from mapping of the West
Greenland continental margin from the Labrador Sea to the Baffin Bay. We present a new …
Greenland continental margin from the Labrador Sea to the Baffin Bay. We present a new …
The crustal structure of the continental margin east of the Falkland Islands
CM Schimschal, W Jokat - Tectonophysics, 2018 - Elsevier
Abstract The 1500 km long Falkland Plateau is the most prominent morphological structure
in the southern South Atlantic Ocean, which crustal composition and development is mainly …
in the southern South Atlantic Ocean, which crustal composition and development is mainly …
[HTML][HTML] The crustal structure in the Northwest Atlantic region from receiver function inversion–Implications for basin dynamics and magmatism
Abstract The Labrador Sea and Baffin Bay form an extinct Palaeogene oceanic spreading
system, divided by a major continental transform, the Davis Strait, with the whole region …
system, divided by a major continental transform, the Davis Strait, with the whole region …