A summary of Brunhes paleomagnetic field variability recorded in Ocean Drilling Program cores

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doi: 10.1016/j.pepi.2005.10.009
Author(s): Lund, Steve; Stoner, Joseph S.; Channell, James E. T.; Acton, Gary D.
Author Affiliation(s): Primary:
University of Southern California, Los Angeles, CA, United States
Other:
University of California at Davis, United States
Florida International University, United States
University of Hawaii at Manoa, United States
Oregon State University, United States
University of Florida, United States
Volume Title: ODP contributions to paleomagnetism
Volume Author(s): Sager, William W., editor; Acton, Gary D.; Clement, Bradford M.; Fuller, Michael
Source: ODP contributions to paleomagnetism, edited by William W. Sager, Gary D. Acton, Bradford M. Clement and Michael Fuller. Physics of the Earth and Planetary Interiors, 156(3-4), p.194-204. Publisher: Elsevier, Amsterdam, Netherlands. ISSN: 0031-9201 CODEN: PEPIAM
Note: In English. 71 refs.; illus., incl. 1 table
Summary: The Ocean Drilling Program (ODP) has recovered many long sediment sequences from around the World that contain medium to high-resolution paleomagnetic records of Brunhes age. These records have provided an important new global view of geomagnetic field variability during 'stable' magnetic (dipole) polarity that could not be recovered by conventional terrestrial or deep-sea piston coring. The ODP paleomagnetic records of directional variability can be routinely recovered and used regionally as a very high-resolution relative chronostratigraphic tool (± 200 yr resolution). ODP paleomagnetic records of Brunhes age relative paleointensity have dramatically improved our understanding of global geomagnetic field intensity. These records document the global-scale pattern of paleointensity and demonstrate its use as a high-resolution relative chronostratigraphic tool that under ideal conditions could have a precision of ±500 yr. ODP paleomagnetic records and associated oxygen isotope chronostratigraphies have also greatly improved our understanding of the number and ages of Brunhes geomagnetic field excursions, and their relationship to normal directional secular variation and paleointensity variability. Although significant progress has been made though ODP paleomagnetic studies of Brunhes-aged sediments, it is clear that more work is needed to further resolve and define the detailed global pattern of Brunhes PSV and its relationship to excursions and true polarity reversals. Abstract Copyright (2006) Elsevier, B.V.
Year of Publication: 2006
Research Program: ODP Ocean Drilling Program
Key Words: 18 Geophysics, Solid-Earth; 24 Surficial Geology, Quaternary Geology; Brunhes Chron; Cenozoic; Cores; Leg 172; Magnetic excursions; Magnetic field; Magnetic intensity; Marine sediments; ODP Site 1061; Ocean Drilling Program; Paleomagnetism; Quaternary; Reversals; Secular variations; Sediments; Upper Quaternary
Coordinates: N295831 N295831 W0733600 W0733600
Record ID: 2007053207
Copyright Information: GeoRef, Copyright 2019 American Geosciences Institute. Reference includes data from CAPCAS, Elsevier Scientific Publishers, Amsterdam, Netherlands