Titlebook: Continental Flood Basalts; J. D. Macdougall Book 1988 Springer Science+Business Media Dordrecht 1988 China.petrogenesis.volcanism

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https://doi.org/10.1007/978-3-211-72456-9 south of latitude 14°S and dominantly of Lower Jurassic age. Almost everywhere the volcanic members rest on sedimentary rocks of the Karoo Supergroup, an intercratonic basinal sequence of Late Carboniferous to Triassic age (e.g. see Tankard et al., 1982). This review will cover those igneous rocks

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The Ethiopian Flood Basalt Province, spreading zones. Prolific eruption of basalt and subordinate other lavas during Tertiary time has built up a subaerial volcanic pile, typically 500–1500 m thick and locally attaining 3000 m. This eruptive process was particularly active during mid-Tertiary, and was renewed in Afar some 5 My ago. Th

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The North Atlantic Tertiary Province, interchangeably to refer to ensialic lavas and associated central intrusive complexes, largely erupted or emplaced in the Paleocene and Eocene, and associated with the process of rifting which led to the opening of the North Atlantic Ocean.

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Deccan Traps,to the Late Cretaceous-Early Tertiary. Not surprisingly, the youngest of these, the Deccan plateau (derived from a Sanskrit word meaning “south” or “southern”) is by far the best-preserved and most extensive, presently occupying some half a million square kilometers of western and central India and