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A major change in magma sources in late Mesozoic active margin of

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Last updated 08 junho 2024
A major change in magma sources in late Mesozoic active margin of
A major change in magma sources in late Mesozoic active margin of
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
A rapid change in magma plumbing taps porphyry copper deposit-forming magmas
A major change in magma sources in late Mesozoic active margin of
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
Minerals, Free Full-Text
A major change in magma sources in late Mesozoic active margin of
Late Magmatic Activity in the Tarim Large Igneous Province: Evidence from the Puchang Granites
A major change in magma sources in late Mesozoic active margin of
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
Geology of the North Sea - Wikipedia
A major change in magma sources in late Mesozoic active margin of
Plate tectonics - Island Arcs, Subduction, Volcanism
A major change in magma sources in late Mesozoic active margin of
La vs. La/Sm (a), Yb vs. La/Yb (b) and Yb vs. Tb/Yb (c) diagrams of the
A major change in magma sources in late Mesozoic active margin of
Full article: Geochemistry of Late Mesozoic volcanic rocks in the central Great Xing'an Range, NE China: petrogenesis and crustal growth in comparison with adjacent areas
A major change in magma sources in late Mesozoic active margin of
Minerals, Free Full-Text
A major change in magma sources in late Mesozoic active margin of
Generation of late Mesozoic felsic volcanic rocks in the Hailar Basin, northeastern China in response to overprinting of multiple tectonic regimes
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