AFRP20: New P‐Wavespeed Model for the African Mantle Reveals Two Whole‐Mantle Plumes Below East Africa and Neoproterozoic Modification of the Tanzania …

A Boyce, ID Bastow, S Cottaar… - Geochemistry …, 2021 - Wiley Online Library
Africa's Cenozoic tectonism is often attributed to mantle plumes, particularly below East
Africa, but their morphology, number, location, and impact on the African lithosphere are …

Seismic tomographic imaging of the Eastern Mediterranean mantle: implications for terminal‐stage subduction, the uplift of Anatolia, and the development of the North …

R Kounoudis, ID Bastow, CS Ogden… - Geochemistry …, 2020 - Wiley Online Library
Abstract The Eastern Mediterranean captures the east‐west transition from active
subduction of Earth's oldest oceanic lithosphere to continental collision, making it an ideal …

Model update May 2016: Upper‐mantle heterogeneity beneath North America from travel‐time tomography with global and USArray data

S Burdick, FL Vernon, V Martynov… - Seismological …, 2017 - pubs.geoscienceworld.org
ABSTRACT P‐wave travel‐time residuals from USArray helped improve the scale and
consistency with which the mantle beneath North America is resolved. Beginning in 2008 …

Concurrent MORB-type and ultrapotassic volcanism in an extensional basin along the Laurentian Iapetus margin: Tectonomagmatic response to Ordovician arc …

D Gasser, T Grenne, F Corfu, R Bøe, TS Røhr… - …, 2022 - pubs.geoscienceworld.org
Arc-continent collision, followed by subduction polarity flip, occurs during closure of oceanic
basins and contributes to the growth of continental crust. Such a setting may lead to a highly …

Variations in Seismic Wave Speed and VP/VS Ratio in the North American Lithosphere

EM Golos, H Fang… - Journal of Geophysical …, 2020 - Wiley Online Library
Seismic wave speed is controlled by a number of factors, including temperature and
chemical composition, as well as the presence of volatiles and partial melt. Tomography …

The Laramide orogeny: Current understanding of the structural style, timing, and spatial distribution of the classic foreland thick-skinned tectonic system

AB Weil, A Yonkee - 2023 - pubs.geoscienceworld.org
The Laramide foreland belt comprises a broad region of thick-skinned, contractional
deformation characterized by an anastomosing network of basement-cored arches and …

The upper mantle structure of northwestern Canada from teleseismic body wave tomography

C Estève, P Audet, AJ Schaeffer… - Journal of …, 2020 - Wiley Online Library
Abstract The Northern Canadian Cordillera (NCC) is an actively deforming orogenic belt in
northwestern Canada. Geochemical and geophysical data show that the NCC is underlain …

Variable modification of continental lithosphere during the Proterozoic Grenville orogeny: Evidence from teleseismic P-wave tomography

A Boyce, ID Bastow, EM Golos, S Rondenay… - Earth and Planetary …, 2019 - Elsevier
Cratons, the ancient cores of the continents, have survived thermal and mechanical erosion
over multiple Wilson cycles, but the ability of their margins to withstand modification during …

A new P‐wave tomographic model (CAP22) for North America: Implications for the subduction and cratonic metasomatic modification history of western Canada and …

A Boyce, MV Liddell, S Pugh, J Brown… - Journal of …, 2023 - Wiley Online Library
Our understanding of the present‐day state and evolution of the Canadian and Alaskan
mantle is hindered by a lack of absolute P‐wavespeed constraints that provide …

Seismic high attenuation region observed beneath southern New England from teleseismic body wave spectra: Evidence for high asthenospheric temperature without …

MT Dong, WH Menke - Geophysical Research Letters, 2017 - Wiley Online Library
Seismic attenuation exhibits strong geographic variability in northeastern North America,
with the highest values associated with the previously recognized Northern Appalachian …