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[HTML][HTML] Tracing volcanic emissions from the Central Atlantic Magmatic Province in the sedimentary record
The end-Triassic mass extinction (ETME) is thought to have been caused by voluminous,
pulsed volcanic activity of the Central Atlantic Magmatic Province (CAMP). Over the last …
pulsed volcanic activity of the Central Atlantic Magmatic Province (CAMP). Over the last …
Cenozoic mountain building and topographic evolution in Western Europe: impact of billions of years of lithosphere evolution and plate kinematics
The architecture and tectono-magmatic evolution of the lithosphere of Europe are the result
of a succession of subduction, rifting and inputs from plumes that have modified the …
of a succession of subduction, rifting and inputs from plumes that have modified the …
The central atlantic magmatic province (CAMP) in Morocco
Abstract The Central Atlantic Magmatic Province (CAMP) is a large igneous province (LIP)
composed of basic dykes, sills, layered intrusions and lava flows emplaced before Pangea …
composed of basic dykes, sills, layered intrusions and lava flows emplaced before Pangea …
New constraints on the age, geochemistry, and environmental impact of High Arctic Large Igneous Province magmatism: Tracing the extension of the Alpha Ridge …
Abstract The High Arctic Large Igneous Province (HALIP) represents extensive Cretaceous
magmatism throughout the circum-Arctic borderlands and within the Arctic Ocean (eg, the …
magmatism throughout the circum-Arctic borderlands and within the Arctic Ocean (eg, the …
Revised stratigraphic framework for the lower Anti-Atlas supergroup based on U–Pb geochronology of magmatic and detrital zircons (Zenaga and Bou Azzer-El …
U–Pb geochronology of magmatic and detrital zircons (Zenaga and Bou Azzer-El Graara
inliers, Anti-Atlas Belt, Morocco) and a reassessment of the published constraints suggest a …
inliers, Anti-Atlas Belt, Morocco) and a reassessment of the published constraints suggest a …
[HTML][HTML] Anthropogenic-scale CO2 degassing from the Central Atlantic Magmatic Province as a driver of the end-Triassic mass extinction
The climatic and environmental impact of exclusively volcanic CO 2 emissions is assessed
during the main effusive phase of the Central Atlantic Magmatic Province (CAMP), which is …
during the main effusive phase of the Central Atlantic Magmatic Province (CAMP), which is …
High Arctic Large Igneous Province alkaline rocks in Canada: evidence for multiple mantle components
Abstract The Cretaceous High Arctic Large Igneous Province (HALIP) in Canada, although
dominated by tholeiites (135–90 Ma), contains two main groups of alkaline igneous rocks …
dominated by tholeiites (135–90 Ma), contains two main groups of alkaline igneous rocks …
The magmatic architecture of continental flood basalts I: Observations from the Deccan Traps
Flood basalts are some of the largest magmatic events in Earth history, with intrusion and
eruption of millions of km3 of basaltic magma over a short time period (∼ 1–5 Ma). A typical …
eruption of millions of km3 of basaltic magma over a short time period (∼ 1–5 Ma). A typical …
Volcanism as a prime cause of mass extinctions: Retrospectives and perspectives
G Racki - 2020 - pubs.geoscienceworld.org
In recent models of earth-system crises, the correlation between the major Phanerozoic
mass extinctions and large igneous provinces has been well established. Specifically …
mass extinctions and large igneous provinces has been well established. Specifically …
Geochemical systematics of High Arctic Large Igneous Province continental tholeiites from Canada—evidence for progressive crustal contamination in the plumbing …
Abstract Cretaceous High Arctic large igneous province (HALIP) sub-alkaline magmatic
rocks in Canada are mostly evolved (MgO 2–7 wt%), sparsely plagioclase+ …
rocks in Canada are mostly evolved (MgO 2–7 wt%), sparsely plagioclase+ …