A major change in magma sources in late Mesozoic active margin of
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Last updated 29 julho 2024
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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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Great Magma Eruptions Had Two Sources - Geology In
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Passive margin - Wikipedia
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Geosciences, Free Full-Text
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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
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Evolution of magma-poor continental margins from rifting to seafloor spreading
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Generation of magmatism under active continental margins: A thermodynamic study of subduction and translithospheric diapirs - ScienceDirect
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Time and Hf isotopic mapping of Mesozoic igneous rocks in the Argun massif, NE China: Implication for crustal architecture and its control on polymetallic mineralization - ScienceDirect
![A major change in magma sources in late Mesozoic active margin of](https://www.researchgate.net/publication/353373879/figure/fig1/AS:1048188769292288@1626919085098/Gagua-Ridge-GR-Philippine-Sea-lava-dataA-Variation-of-total-alkali-Na-2-O-K-2-O.png)
Gagua Ridge (GR, Philippine Sea) lava data.(A) Variation of total
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11.2: The Big Five - Geosciences LibreTexts
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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
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Full article: Evolved Late Mesozoic continental arc: Constraints of detrital zircons from the western East China Sea
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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
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