A major change in magma sources in late Mesozoic active margin of
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Last updated 29 março 2025


Large Igneous Province thermogenic greenhouse gas flux could have initiated Paleocene-Eocene Thermal Maximum climate change

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A major change in magma sources in late Mesozoic active margin of the circum‐Sea of Japan domain: Geochemical constraints from late Paleozoic to Paleogene mafic dykes in the Sergeevka belt, southern Primorye

A major change in magma sources in late Mesozoic active margin of the circum‐Sea of Japan domain: Geochemical constraints from late Paleozoic to Paleogene mafic dykes in the Sergeevka belt, southern Primorye

Full article: Geochronology and geochemistry of late Jurassic–Early Cretaceous volcanic rocks in the southern Great Xing'an range, NE China: constraints for late Mesozoic tectono-magmatic evolution

A major change in magma sources in late Mesozoic active margin of the circum‐Sea of Japan domain: Geochemical constraints from late Paleozoic to Paleogene mafic dykes in the Sergeevka belt, southern Primorye

Constraining the sub-arc, parental magma composition for the giant Altiplano-Puna Volcanic Complex, northern Chile

Schematic tectonic scenarios showing accretion and amalgamation

The following summary of the geology of basalts is modified from the material presented on a web page of an Igneous Petrology course

Subduction initiation triggered the Caribbean large igneous province

Sketch of two end-member continental-margins with accretionary orogens

Geodynamic evolution of the Arctic in the Mesozoic: (a) Late

Igneous Rocks
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