A major change in magma sources in late Mesozoic active margin of
Por um escritor misterioso
Last updated 21 fevereiro 2025
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Sketch of two end-member continental-margins with accretionary orogens
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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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Offshore-onshore tectonomagmatic correlations: Towards a Late Mesozoic non-Andean-type Cathaysian continental margin - 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
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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
Location map of Late Mesozoic volcanic areas in Central Asia
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Rio Grande rift - Wikipedia
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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
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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

Map of the continental margin of eastern North America (ENAM) showing
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Mesozoic intraplate tectonism of East Asia due to flat subduction of a composite terrane slab - ScienceDirect
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Large Igneous Province thermogenic greenhouse gas flux could have initiated Paleocene-Eocene Thermal Maximum climate change
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Rifted margins classification and forcing parameters
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Full article: Complex magma sources of late Mesozoic granites along the southern margin of the North China Craton: constraints from geochemistry and geochronology of the massive Heyu and Lantian plutons
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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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