Porosity and sound velocity measured in sediment core CIROS-1

The CIROS-1 drillhole, which in 1986 reached a depth of 700 m below the seafloor, is still the only deep hole that can provide information on the velocity structure of the upper crust in McMurdo Sound and the Ross Sea, Antarctica. A careful review and quality control of the downhole logging data of...

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Bibliographic Details
Main Authors: Bücker, Christian J, Henrys, Stuart A, Wonik, Thomas
Format: Dataset
Language:English
Published: PANGAEA 1998
Subjects:
CRP
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.54717
https://doi.org/10.1594/PANGAEA.54717