New data and interpretations on geological relationships of igneous rocks at Mokka Fiord, Axel Heiberg Island, Nunavut, provide insight into the timing and nature of magmatism associated with the Sverdrup Basin and High Arctic Large Igneous Province (HALIP). Field relationships indicate that the igneous rocks, previously interpreted to be volcanic flows, are most likely an intrusive unit discordant to regional bedding. An intrusive origin helps resolve chronostratigraphic inconsistencies in previous work. The host rocks are palynologically constrained to be late Barremian to late Aptian in age and are interpreted to be Paterson Island or Walker Island member of the Isachsen Formation. If the igneous body is intrusive, itâ s previously repo...
Considerable Late Cretaceous research has focused on Cenomanian to Turonian organic carbon-rich depo...
Late Mesozoic mafic igneous rocks are widespread across the Arctic region, and are collectively refe...
We use new models of crustal structure and the depth of the lithosphere–asthenosphere boundary to ca...
New data and interpretations on geological relationships of igneous rocks at Mokka Fiord, Axel Heibe...
Cretaceous magmatism in the Sverdrup Basin of Arctic Canada is widely considered to be part of the c...
AbstractMafic igneous rocks of Cretaceous age (80–130Ma) scattered around the Arctic Ocean are commo...
The Cretaceous High Arctic Large Igneous Province (HALIP) in Canada, although dominated by tholeiite...
The Cretaceous geological evolution of the Canadian Arctic was marked by voluminous magmatism compri...
Emplacement of Large Igneous Provinces (LIPs) had a major effect on global climate, ocean chemistrie...
Cretaceous High Arctic large igneous province (HALIP) sub-alkaline magmatic rocks in Canada are most...
Since the 1970s, the Alpha-Mendeleev Ridge (AMR) has generally been considered oceanic, with a thick...
More than 50 conspicuous tephra beds occur in the Kanguk Formation of SW Banks Island. Their glass s...
The Strand Fiord Formation is a volcanic unit of early Late Cretaceous age which outcrops on west-ce...
The genesis of the Amerasia Basin in the Arctic Ocean has been difficult to discern due to overprint...
Knowledge about the Arctic tectonic structure has changed in the last decade as a large number of ne...
Considerable Late Cretaceous research has focused on Cenomanian to Turonian organic carbon-rich depo...
Late Mesozoic mafic igneous rocks are widespread across the Arctic region, and are collectively refe...
We use new models of crustal structure and the depth of the lithosphere–asthenosphere boundary to ca...
New data and interpretations on geological relationships of igneous rocks at Mokka Fiord, Axel Heibe...
Cretaceous magmatism in the Sverdrup Basin of Arctic Canada is widely considered to be part of the c...
AbstractMafic igneous rocks of Cretaceous age (80–130Ma) scattered around the Arctic Ocean are commo...
The Cretaceous High Arctic Large Igneous Province (HALIP) in Canada, although dominated by tholeiite...
The Cretaceous geological evolution of the Canadian Arctic was marked by voluminous magmatism compri...
Emplacement of Large Igneous Provinces (LIPs) had a major effect on global climate, ocean chemistrie...
Cretaceous High Arctic large igneous province (HALIP) sub-alkaline magmatic rocks in Canada are most...
Since the 1970s, the Alpha-Mendeleev Ridge (AMR) has generally been considered oceanic, with a thick...
More than 50 conspicuous tephra beds occur in the Kanguk Formation of SW Banks Island. Their glass s...
The Strand Fiord Formation is a volcanic unit of early Late Cretaceous age which outcrops on west-ce...
The genesis of the Amerasia Basin in the Arctic Ocean has been difficult to discern due to overprint...
Knowledge about the Arctic tectonic structure has changed in the last decade as a large number of ne...
Considerable Late Cretaceous research has focused on Cenomanian to Turonian organic carbon-rich depo...
Late Mesozoic mafic igneous rocks are widespread across the Arctic region, and are collectively refe...
We use new models of crustal structure and the depth of the lithosphere–asthenosphere boundary to ca...