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

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A major change in magma sources in late Mesozoic active margin of
Metallogenic type controlled by magma source and tectonic regime: Geochemical comparisons of Mesozoic magmatism between the Middle–Lower Yangtze River Belt and the Dabie Orogen, eastern China - ScienceDirect
A major change in magma sources in late Mesozoic active margin of
Late Cretaceous‐Palaeocene arc magmatism in Bumeicun, Gangdese, southern Tibet: Products of slab rollback of Neo‐Tethyan Ocean? - Liu - 2023 - Geological Journal - Wiley Online Library
A major change in magma sources in late Mesozoic active margin of
Timing of Extensional Faulting Along the Magma-Poor Central and Northern Red Sea Rift Margin—Transition from Regional Extension to Necking Along a Hyperextended Rifted Margin
A major change in magma sources in late Mesozoic active margin of
Modification of Archean lower crust of the North China Craton by magma underplating during the Mesozoic: Evidence from zircon U-Pb-Hf-O isotopes of granulite xenoliths - ScienceDirect
A major change in magma sources in late Mesozoic active margin of
Igneous Rocks
A major change in magma sources in late Mesozoic active margin of
Full article: Tectonic nature of the NE Asian continental margin during the Late Jurassic–Early Cretaceous: constraints from the geochronology and geochemistry of igneous rocks in the NE North China Craton
A major change in magma sources in late Mesozoic active margin of
The following summary of the geology of basalts is modified from the material presented on a web page of an Igneous Petrology course
A major change in magma sources in late Mesozoic active margin of
11.2: The Big Five - Geosciences LibreTexts
A major change in magma sources in late Mesozoic active margin of
Passive margin - Wikipedia
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
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
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