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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
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
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
Origin of arc-like magmatism at fossil convergent plate boundaries: Geochemical insights from Mesozoic igneous rocks in the Middle to Lower Yangtze Valley, South China - ScienceDirect
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
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
Mesozoic intraplate tectonism of East Asia due to flat subduction of a composite terrane slab - ScienceDirect
A major change in magma sources in late Mesozoic active margin of
Examples of geological events changing the provenance signatures 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
Schematic tectonic diagram showing late Mesozoic-Tertiary evolution of
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