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Abstract

The interpretation of a large amount of multichannel seismic reflection sections recorded during the first Italian geophysical cruises to Antarctica (1978-88, 1988-89), performed by OGS-Trieste, has revealed new and interesting elements about the structure, the stratigraphy and the evolution of the Pacific sector of the Antarctic Platform.

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/content/papers/10.3997/2214-4609.201410887
1991-05-28
2024-04-26
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201410887
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