2015
DOI: 10.2204/iodp.proc.347.102.2015
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Methods

Abstract: This chapter documents the primary operational, curatorial, and analytical procedures and methods employed during the offshore and onshore phases of Integrated Ocean Drilling Program (IODP) Expedition 347. This information concerns only shipboard and Onshore Science Party (OSP) methodologies and data as described in the site chapters. Methods for postexpedition research conducted on Expedition 347 samples and data will be described in individual scientific contributions published after the OSP. Detailed drilli… Show more

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Cited by 15 publications
(16 citation statements)
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“…Core recovery was generally good in Hole M0060A, except for a gap between ~101.5 and 117 mbsf and from ~198 mbsf to the base of the hole, where coring alternated between hammer sampling and open-hole intervals. Although all physical property measurements described in "Physical properties" in the Methods chapter (Andrén et al, 2015) were conducted for Site M0060, whole-round core shipboard P-wave velocity data appear to be highly affected by artifacts, similar to those seen at Site M0059 (Little Belt). Discrete Pwave and thermal conductivity data are too sparsely distributed to exhibit any discernable downcore trends, and noncontact electrical resistivity data show little variability.…”
Section: Physical Propertiesmentioning
confidence: 99%
See 1 more Smart Citation
“…Core recovery was generally good in Hole M0060A, except for a gap between ~101.5 and 117 mbsf and from ~198 mbsf to the base of the hole, where coring alternated between hammer sampling and open-hole intervals. Although all physical property measurements described in "Physical properties" in the Methods chapter (Andrén et al, 2015) were conducted for Site M0060, whole-round core shipboard P-wave velocity data appear to be highly affected by artifacts, similar to those seen at Site M0059 (Little Belt). Discrete Pwave and thermal conductivity data are too sparsely distributed to exhibit any discernable downcore trends, and noncontact electrical resistivity data show little variability.…”
Section: Physical Propertiesmentioning
confidence: 99%
“…To achieve the main objectives of the OSP paleomagnetic work, magnetic susceptibility measurements and rudimentary analyses of the natural remanent magnetization (NRM) were made on discrete specimens of known volume and mass (see "Paleomagnetism" in the "Methods" chapter [Andrén et al, 2015]). The discrete samples were taken from Hole M0060A, with a gap in sampling between 116 and 101 mbsf in the mid-lower sections of Unit V because of poor core recovery.…”
Section: Paleomagnetismmentioning
confidence: 99%
“…F18). Although all physical property measurements described in "Physical properties" in the "Methods" chapter (Andrén et al, 2015) were conducted at Site M0063, wholeround core shipboard P-wave data appear to be highly affected by artifacts. Thermal conductivity data are too sparsely distributed to exhibit any discernible downcore trend.…”
Section: Physical Propertiesmentioning
confidence: 99%
“…Magnetic susceptibility measurements and simplified analyses of the natural remanent magnetization (NRM) were made on discrete specimens of known volume and mass (see "Paleomagnetism" in the "Methods" chapter [Andrén et al, 2015]). A total of 216 discrete samples were taken from Hole M0063D at intervals of ~50 cm.…”
Section: Paleomagnetismmentioning
confidence: 99%
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