Peak areas and heights for minerals of ODP Leg 113-696B (Table 1)

Seismic data acquired over the eastern shelf and margin of the South Orkney microcontinent, Antarctica, have shown a high-amplitude reflection lying at a sub-bottom two-way traveltime (TWT) of 0.5-0.8 s. There appear to be two causes for the reflection which apply in different parts of the shelf. Th...

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Bibliographic Details
Main Author: Lonsdale, Malcolm J
Format: Dataset
Language:English
Published: PANGAEA 1990
Subjects:
-
ODP
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.753957
https://doi.org/10.1594/PANGAEA.753957