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- W2087237777 abstract "Based on gravity data, the high grade igneous mafic/ultramafic rocks and metasediments at Cabo-Ortegal have recently been interpreted as a Precambrian autochthonous basement which extends far below the low-grade Paleozoic series (Van Overmeeren, 1975). The same gravity data, however, also agree with another model which is consistent with an allochthonous position of the high-grade rocks. On the basis of this new gravity model and of recent geological data (mainly the evidence of ophiolitic melanges in the low-grade Paleozoic series, the Paleozoic age of the high grade mafic/ultramafic rocks and also the general considerations about the Variscan belt), we suggest that the Cabo-Ortegal massif forms part of a large nappe emplaced during a Variscan obduction." @default.
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- W2087237777 date "1979-08-01" @default.
- W2087237777 modified "2023-09-27" @default.
- W2087237777 title "Is the mafic/ultramafic massif of Cabo-Ortegal (northwest Spain) a nappe emplaced during a Variscan obduction? — A new gravity interpretation" @default.
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- W2087237777 doi "https://doi.org/10.1016/0040-1951(79)90138-0" @default.
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