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Suganuma, Yusuke; Ogg, James G (2006): (Table AT2) Late Eocene-Albian palaeomagnetic analysis of ODP Hole 207-1257B [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.775880, In supplement to: Suganuma, Y; Ogg, JG (2006): Campanian through Eocene magnetostratigraphy of Sites 1257-1261, ODP Leg 207, Demerara Rise (western equatorial Atlantic). In: Mosher, DC; Erbacher, J; Malone, MJ (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 207, 1-48, https://doi.org/10.2973/odp.proc.sr.207.102.2006

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Project(s):
Coverage:
Latitude: 9.453630 * Longitude: -54.341800
Date/Time Start: 2003-01-19T22:45:00 * Date/Time End: 2003-01-21T13:20:00
Minimum DEPTH, sediment/rock: 41.66 m * Maximum DEPTH, sediment/rock: 227.61 m
Event(s):
207-1257B * Latitude: 9.453630 * Longitude: -54.341800 * Date/Time Start: 2003-01-19T22:45:00 * Date/Time End: 2003-01-21T13:20:00 * Elevation: -2951.0 m * Penetration: 227.3 m * Recovery: 116.23 m * Location: South Atlantic Ocean * Campaign: Leg207 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 27 cores; 187.3 m cored; 40 m drilled; 62.1 % recovery
Comment:
Sediment depth is given in mcd. Additional comments: Between 1R-2,47 and 1R-3,48: Possible gap of P15 foram zone (uppermost middle Eocene; lower upper Eocene); between 3R-4,36 and 4R-1,67: GAP of 10 meters = C19n/C19r??; 8R-4,84: Was run as 84.042 (label on minicore), but actually should be 84.084 (actual location in Bremen core!); 8-R-3,2: Was run as 83.117 (label on vial), but actually should be 83.002 (actual location in Bremen core!); between 6R-1,118 and 7R-1,14: Gap = gravity flow at boundary; between 4R-3,39 and 4R-4,84: Major gap (lower middle and upper lower Eocene; P7-P10).
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Sample code/labelSample labelSuganuma, YusukeDSDP/ODP/IODP sample designation
2DEPTH, sediment/rockDepth sedmGeocode
3Demag TypeDemag TypeSuganuma, YusukemT/°C; NRM = natural remanent magnetization, AF = alternating-field demagnetization, TT = thermal demagnetization
4DeclinationDecldegSuganuma, YusukeMagnetometer, DC-SQUID, 2G Enterprises
5InclinationIncldegSuganuma, YusukeMagnetometer, DC-SQUID, 2G Enterprises
6ChRM, IntensityIntensity (ChRM)mA/mSuganuma, YusukeMagnetometer, DC-SQUID, 2G Enterprises
7Standard errorStd e±Suganuma, Yusuke
8PolarityPolaritySuganuma, YusukeN or R = well-defined directions computed from at least three vectors, NP or RP = less precise directions computed from only two vectors or a suite of vectors displaying high dispersion, NPP or RPP = samples that did not achieve adequate cleaning during demagnetization but their polarity was obvious, N?? or R?? = uncertain
9CommentCommentSuganuma, Yusuke
Size:
4943 data points

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