A review of Wilson Cycle plate margins: A role for mantle plumes in continental break-up along sutures?

SJH Buiter, TH Torsvik - Gondwana Research, 2014 - Elsevier
Abstract The Wilson Cycle theory that oceans close and reopen along the former suture is a
fundamental concept in plate tectonics. It was named after J. Tuzo Wilson who recognised …

Crustal structure and tectonic model of the Arctic region

O Petrov, A Morozov, S Shokalsky, S Kashubin… - Earth-Science …, 2016 - Elsevier
We present a new model of the crustal and tectonic structure of the Arctic region north of 60°
N latitude, constrained as a part of the international Atlas of Geological Maps of the …

[HTML][HTML] Marine 187Os/188Os isotope stratigraphy reveals the interaction of volcanism and ocean circulation during Oceanic Anoxic Event 2

ADC Du Vivier, D Selby, BB Sageman, I Jarvis… - Earth and Planetary …, 2014 - Elsevier
High-resolution osmium (Os) isotope stratigraphy across the Cenomanian–Turonian
Boundary Interval from 6 sections for four transcontinental settings has produced a record of …

[PDF][PDF] Does large igneous province volcanism always perturb the mercury cycle? Comparing the records of Oceanic Anoxic Event 2 and the end-Cretaceous to other …

LME Percival, HC Jenkyns, TA Mather… - American Journal of …, 2018 - ajsonline.org
Mercury (Hg) is increasingly being used as a sedimentary tracer of Large Igneous Province
(LIP) volcanism, and supports hypotheses of a coincidence between the formation of several …

The Eurekan deformation in the Arctic: an outline

K Piepjohn, W von Gosen… - Journal of the Geological …, 2016 - lyellcollection.org
The evolution of the Eurekan deformation zones in the Arctic is closely related to the
development of the circum-Greenland plate boundaries in Early Cenozoic times (53–34 Ma) …

The tectonic evolution of the Arctic since Pangea breakup: Integrating constraints from surface geology and geophysics with mantle structure

GE Shephard, RD Müller, M Seton - Earth-Science Reviews, 2013 - Elsevier
The tectonic evolution of the circum-Arctic, including the northern Pacific, Siberian and North
American margins, since the Jurassic has been punctuated by the opening and closing of …

An appraisal of the ages of Phanerozoic large igneous provinces

Q Jiang, F Jourdan, HKH Olierook, RE Merle - Earth-Science Reviews, 2023 - Elsevier
Large igneous provinces (LIPs) are the products of exceptional magmatic events that played
important roles in tectonic plate reorganizations, environmental crises, energy resource …

On the origin of the Amerasia Basin and the High Arctic Large Igneous Province—results of new aeromagnetic data

A Døssing, HR Jackson, J Matzka, I Einarsson… - Earth and Planetary …, 2013 - Elsevier
The history of the 2.5 million km2 Amerasia Basin (sensu lato) is in many ways the least
known in the global tectonic system. Radically different hypotheses proposed to explain its …

[HTML][HTML] Cenozoic uplift and erosion of the Norwegian Barents Shelf–A review

APE Lasabuda, NS Johansen, JS Laberg… - Earth-Science …, 2021 - Elsevier
Uplift and erosion are complex phenomena in terms of their governing processes, precise
timing and exact magnitude. The intricate relationship between different geodynamic …

Sedimentary mercury enrichments as a marker for submarine large igneous province volcanism? Evidence from the Mid‐Cenomanian event and Oceanic Anoxic …

JD Scaife, M Ruhl, AJ Dickson… - Geochemistry …, 2017 - Wiley Online Library
Abstract Oceanic Anoxic Event 2 (OAE 2), during the Cenomanian‐Turonian transition (∼
94 Ma), was the largest perturbation of the global carbon cycle in the mid‐Cretaceous and …