A major change in magma sources in late Mesozoic active margin of
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Major element variation diagrams, with SiO2 as fractionation index, for
Provenance evolution during passive- to active-margin transition unraveled from an accretionary complex from the Bangong-Nujiang suture zone: Insights into Early Mesozoic Meso-Tethys subduction and source-area tectonics - ScienceDirect
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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
South China Sea documents the transition from wide continental rift to continental break up
La vs. La/Sm (a), Yb vs. La/Yb (b) and Yb vs. Tb/Yb (c) diagrams of the
Full article: Evolved Late Mesozoic continental arc: Constraints of detrital zircons from the western East China Sea
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: Geochemical, mineralogical and chronological studies of mafic-intermediate dykes in the Jiaodong Peninsula: implications for Late Mesozoic mantle source metasomatism and lithospheric thinning of the eastern North China Craton
Subduction initiation triggered the Caribbean large igneous province
The following summary of the geology of basalts is modified from the material presented on a web page of an Igneous Petrology course
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