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(Table 1) Anisotropy of magnetic susceptibility and paleomagnetic results for...
The fabric of fine-grained sediments from the deep-sea terrace on the landward side of the Japan Trench, cored during Ocean Drilling Program Leg 186, was analyzed using the... -
(Appendix A3) Bulk magnetic susceptibility of ODP Site 178-1095A
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(Table 2) Susceptibility and anisotropy of the susceptibility of core samples...
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(Table 2) Sediment analyses of ODP Hole 119-745B
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(Table B) Results of analysis of Bermuda Rise sediment core CH89-9P
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(Table A) Results of inter-depositional environment analysis
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(Table 4) Magnetic anisoteopy of ODP Hole 134-829A
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(Table T2) Magnetic susceptibility and AMS characteristics of ODP Site 185-11...
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(Table 2) Magnetic properties of basalts recovered at ODP Hole 107-655B
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(Table 1) Magnetic properties of basalts recovered at ODP Hole 107-651A
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(Table 2) Sedimentology of the Pliocene section of the DSDP Gardar Drift Site...
Ages based on magnetic reversal stratigraphy using the timescale of Cande and Kent (1995, doi:10.1029/94JB03098) -
(Table 1) Sedimentology of the Pliocene section of the DSDP Feni Drift Site 9...
Ages younger than 8 Ma based on magnetic reversal stratigraphy using the timescale of Cande and Kent (1995, doi:10.1029/94JB03098), older than 8 Ma determined using the... -
(Table T1) Magnetic anisotropy of samples from ODP Hole 180-1117A
At Site 1117, drilled during Leg 180 of the Ocean Drilling Program in the Woodlark Basin, we cored a fault zone and recovered fault gouge, mylonitized and brecciated gabbros,...
