The Central Atlantic magmatic province (CAMP): A review
Abstract The Central Atlantic magmatic province (CAMP) consists of basic rocks emplaced
as shallow intrusions and erupted in large lava flow fields over a land surface area in excess …
as shallow intrusions and erupted in large lava flow fields over a land surface area in excess …
[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 …
[HTML][HTML] End-Triassic mass extinction started by intrusive CAMP activity
The end-Triassic extinction is one of the Phanerozoic's largest mass extinctions. This
extinction is typically attributed to climate change associated with degassing of basalt flows …
extinction is typically attributed to climate change associated with degassing of basalt flows …
[HTML][HTML] A new plumbing system framework for mantle plume-related continental Large Igneous Provinces and their mafic-ultramafic intrusions
The magmatic components of continental Large Igneous Provinces (LIPs) include flood
basalts and their plumbing system of giant mafic dyke swarms (radiating, linear, and the …
basalts and their plumbing system of giant mafic dyke swarms (radiating, linear, and the …
Gondwana Large Igneous Provinces: plate reconstructions, volcanic basins and sill volumes
Gondwana was an enormous supertarrane. At its peak, it represented a landmass of about
100× 10 6 km 2 in size, corresponding to approximately 64% of all land areas today …
100× 10 6 km 2 in size, corresponding to approximately 64% of all land areas today …
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 …
Deep CO2 in the end-Triassic Central Atlantic Magmatic Province
Abstract Large Igneous Province eruptions coincide with many major Phanerozoic mass
extinctions, suggesting a cause-effect relationship where volcanic degassing triggers global …
extinctions, suggesting a cause-effect relationship where volcanic degassing triggers global …
[HTML][HTML] The evolution of the subcontinental mantle beneath the Central Iberian Zone: Geochemical tracking of its mafic magmatism from the Neoproterozoic to the …
Continental lithosphere is modified over eons in response to large-scale tectonic processes,
such as rifting and collisions. The lithospheric mantle beneath central Iberia was affected by …
such as rifting and collisions. The lithospheric mantle beneath central Iberia was affected by …
Supercontinental inheritance and its influence on supercontinental breakup: The C entral A tlantic M agmatic P rovince and the breakup of P angea
Abstract The Central Atlantic Magmatic Province (CAMP) is the large igneous province (LIP)
that coincides with the breakup of the supercontinent Pangea. Major and trace element data …
that coincides with the breakup of the supercontinent Pangea. Major and trace element data …
Zircon petrochronology in large igneous provinces reveals upper crustal contamination processes: new U–Pb ages, Hf and O isotopes, and trace elements from the …
Zircon occasionally crystallizes in evolved melt pockets in mafic large igneous province (LIP)
magmas, and in these cases, it is used to provide high-precision age constraints on LIP …
magmas, and in these cases, it is used to provide high-precision age constraints on LIP …