(Table 1) Paleomagnetic characteristics of sediments from ODP Leg 164 sites

• Main Author: Hiroki, Yoshihisa
• Format: Dataset
• Language: English
• Published: PANGAEA 2000
• Subjects: 164-994C; 164-995A; 164-997A; Demag Type; DEPTH; sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Elevation of event; Event label; Joides Resolution; Latitude of event; Leg164; Longitude of event; Magnetometer; cryogenic; 2G Enterprises 750; Nicaraguan Rise; North Atlantic Ocean; NRM; Declination; Declination after demagnetization; Inclination; Inclination after demagnetization; Intensity; Intensity after demagnetization; Ocean Drilling Program; ODP; Polarity; Sample code/label; Sample comment; North Atlantic
• Online Access: https://doi.pangaea.de/10.1594/PANGAEA.804536; https://doi.org/10.1594/PANGAEA.804536

The Blake Ridge, offshore South Carolina, was drilled at three sites, Sites 994, 995, and 997, during Ocean Drilling Program Leg 164. During the cruise, shipboard paleomagnetic measurements were performed to establish a magnetostratigraphy to refine age dates of the sediments. Shipboard measurements yielded a preliminary reversal stratigraphy (Shipboard Scientific Party, 1996, doi:10.2973/odp.proc.ir.164.1996). The routine paleomagnetic measurements of continuous core sections with the pass-through cryogenic magnetometer after alternating field (AF) demagnetization at 20 mT showed downhole inclination profiles with negative and positive intervals in the sections recovered with the advanced hydraulic piston corer (APC). The cryogenic results agreed with the results from analysis of discrete samples. The reversal stratigraphy was constructed based on the cryogenic and discrete sample results. Although the primary reversal stratigraphy was constructed for each site during the cruise, the boundaries of magnetic polarity zones were poorly constrained because there were insufficient polarity measurements obtained from the discrete sample analysis (Only one or two samples per core were made in the intervals recovered with the APC; fewer were made in the intervals cored with the extended core barrel [XCB]. Each core is 9.5 m). Therefore, I conducted shore-based paleomagnetic analyses to determine more precise locations of the magnetic polarity zones and reversals for the APC-cored intervals at Sites 994, 995, and 997. In this report, I describe progressive AF demagnetization behavior of the samples and present paleomagnetic declination, inclination, and intensity data before and after AF demagnetization. Magnetic polarity zones are defined for the APC-cored intervals of Sites 994, 995, and 997, and these are presented with nannofossil data and interpreted nannofossil zonations (Okada, 2000, doi:10.2973/odp.proc.sr.164.232.2000).