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- W2479427908 abstract "Drilling at each of the five sites in the central Caribbean terminated in basalt or dolerite ranging in age from Coniacian (Sites 146 and 153) to early Campanian (Site 152). The distribution of these occurrences suggests a large basaltic province, and a tentative correlation with Reflector B suggests that these rocks occur over almost the entire Venezuelan Basin, as well as much of the northern Colombian Basin. Further considerations of late Cretaceous igneous occurrences all around the Caribbean suggest that the event which produced these magmas lasted about 10 million years, with more acid differentiates lasting perhaps another 10 million'years at most. Also, igneous events in various Antillean islands and in South and Central America which had been considered peculiar to these areas and the result of local tectonic-magmatic activity are now seen to be interrelated and probably relatively independent of local tectonic events. Finally, the occurrence of these rocks, including the rocks from around the Caribbean and their presumed acid differentiates, may complicate the currently widely accepted views on the dichotomy of island arc and central ocean magmatism." @default.
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- W2479427908 date "1973-12-01" @default.
- W2479427908 modified "2023-10-01" @default.
- W2479427908 title "Basalts and Dolerites of Late Cretaceous Age from the Central Caribbean" @default.
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- W2479427908 doi "https://doi.org/10.2973/dsdp.proc.15.130.1973" @default.
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