| _version_ | 1867168582591315968 |
|---|---|
| author | Bücker, Christian J Henrys, Stuart A Wonik, Thomas |
| author_facet | Bücker, Christian J Henrys, Stuart A Wonik, Thomas |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | 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 CIROS-1 resulted in a new porosity depth function that is consistent with porosity data from the MSSTS-1 and CRP-1 drillholes. Using existing porosity-velocity equations, it was possible for the first time to obtain reliable velocity information for the upper 700 m of strata off the Victoria Land coast. The calculated synthetic seismograms, based on downhole velocity and density data, fit very well with the existing seismic lines IT90A-71, PD90-12, and NBP9601-89. The quality of the correlation confirms that the average velocity of the top 700 m of strata is about 2 000-2 300 m/s, and not 2 800-3 000 m/s, as was previously assumed. In consequence, these distinctly lower velocities result in shallower depths for the seismic unconformities V3/V4 andV4/V5 and thus may have important implications for further drilling off Cape Roberts. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_54717 |
| institution | PANGAEA |
| language | en |
| publishDate | 1998 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Porosity and sound velocity measured in sediment core CIROS-1 Bücker, Christian J Henrys, Stuart A Wonik, Thomas Butter Point; Calculated; Cape Roberts Project; CIROS; CIROS-1; CRP; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Porosity; Sampling/drilling ice; Velocity, compressional wave 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 CIROS-1 resulted in a new porosity depth function that is consistent with porosity data from the MSSTS-1 and CRP-1 drillholes. Using existing porosity-velocity equations, it was possible for the first time to obtain reliable velocity information for the upper 700 m of strata off the Victoria Land coast. The calculated synthetic seismograms, based on downhole velocity and density data, fit very well with the existing seismic lines IT90A-71, PD90-12, and NBP9601-89. The quality of the correlation confirms that the average velocity of the top 700 m of strata is about 2 000-2 300 m/s, and not 2 800-3 000 m/s, as was previously assumed. In consequence, these distinctly lower velocities result in shallower depths for the seismic unconformities V3/V4 andV4/V5 and thus may have important implications for further drilling off Cape Roberts. |
| title | Porosity and sound velocity measured in sediment core CIROS-1 |
| topic | Butter Point; Calculated; Cape Roberts Project; CIROS; CIROS-1; CRP; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Porosity; Sampling/drilling ice; Velocity, compressional wave |
| url | https://doi.org/10.1594/PANGAEA.54717 |