Physical properties of ODP Leg 178 sites, supplement to: Volpi, Valentina; Camerlenghi, Angelo; Moerz, Tobias; Corubolo, P; Rebesco, Michele; Tinivella, Umberta (2001): Data report: Physical properties relevant to seismic stratigraphic studies, continental rise Sites 1095, 1096, and 1101, ODP Leg 178, Antarctic Peninsula. In: Barker, PF; Camerlenghi, A; Acton, GD; Ramsay, ATS (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 178, 1-36

We have reanalyzed the porosity, bulk density, and seismic velocity information collected from continental rise Sites 1095, 1096, and 1101 during the drilling of Ocean Drilling Program (ODP) Leg 178 (Fig. F1). The purpose is to provide a comprehensive composite digital set of data readily available...

Full description

Bibliographic Details
Main Authors: Volpi, Valentina, Camerlenghi, Angelo, Moerz, Tobias, Corubolo, P, Rebesco, Michele, Tinivella, Umberta
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA - Data Publisher for Earth & Environmental Science 2001
Subjects:
Composite Core
Leg178
Joides Resolution
Ocean Drilling Program ODP
Antarctic
Antarctic Peninsula
Ramsay
Valentina
Antarc*
Online Access:https://dx.doi.org/10.1594/pangaea.735559
https://doi.pangaea.de/10.1594/PANGAEA.735559
Description
Summary:We have reanalyzed the porosity, bulk density, and seismic velocity information collected from continental rise Sites 1095, 1096, and 1101 during the drilling of Ocean Drilling Program (ODP) Leg 178 (Fig. F1). The purpose is to provide a comprehensive composite digital set of data readily available for future studies aimed at well-seismic correlation. The work originates from the occurrence of overlapping sets of physical parameters and acoustic velocity collected by different methods (downhole logging, core logging, laboratory determination, and derivation from seismic data) and from different holes at the same site. These data do not always provide the same information because of difficulties encountered at each specific hole or methodological differences. In addition, a basic correlation between these parameters and onsite multichannel seismic (MCS) data is presented.

Similar Items