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Suganuma, Yusuke; Ogg, James G (2006): (Table AT1) Early Maastrichtian to mid-Campanian palaeomagnetic analysis of ODP Hole 207-1257A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.775879, 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: 9.453830 * Longitude: -54.341960
Date/Time Start: 2003-01-15T14:30:00 * Date/Time End: 2003-01-19T22:45:00
Minimum DEPTH, sediment/rock: 157.28 m * Maximum DEPTH, sediment/rock: 175.46 m
Event(s):
207-1257A * Latitude: 9.453830 * Longitude: -54.341960 * Date/Time Start: 2003-01-15T14:30:00 * Date/Time End: 2003-01-19T22:45:00 * Elevation: -2951.0 m * Penetration: 284.7 m * Recovery: 216.05 m * Location: South Atlantic Ocean * Campaign: Leg207 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 31 core; 284.7 m cored; 0 m drilled; 75.9 % recovery
Comment:
Sediment depth is given in mcd.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
Sample code/labelSample labelSuganuma, YusukeDSDP/ODP/IODP sample designation
DEPTH, sediment/rockDepth sedmGeocode
Demag TypeDemag TypeSuganuma, YusukemT/°C; NRM = natural remanent magnetization, AF = alternating-field demagnetization, TT = thermal demagnetization
DeclinationDecldegSuganuma, YusukeMagnetometer, DC-SQUID, 2G Enterprises
InclinationIncldegSuganuma, YusukeMagnetometer, DC-SQUID, 2G Enterprises
ChRM, IntensityIntensity (ChRM)mA/mSuganuma, YusukeMagnetometer, DC-SQUID, 2G Enterprises
Standard errorStd e±Suganuma, Yusuke
PolarityPolaritySuganuma, YusukeN or R = well-defined directions computed from at least three vectors, NP = less precise directions computed from only two vectors or a suite of vectors displaying high dispersion, NPP = samples that did not achieve adequate cleaning during demagnetization but their polarity was obvious, N?? = uncertain
CommentCommentSuganuma, Yusuke
Size:
374 data points

Data

Download dataset as tab-delimited text — use the following character encoding:


Sample label

Depth sed [m]

Demag Type

Decl [deg]

Incl [deg]

Intensity (ChRM) [mA/m]

Std e [±]

Polarity

Comment
207-1257A-18X-1, 118157.28NRM 0165.368.50.076900.09indeterminate or N-type
207-1257A-18X-1, 118157.28AF 50164.076.80.033700.07Linear, no indication of R
207-1257A-18X-1, 118157.28TT 150188.872.90.025600.04N?
207-1257A-18X-1, 118157.28TT 200175.774.30.018700.07
207-1257A-18X-1, 118157.28TT 240143.974.50.016000.05
207-1257A-18X-1, 118157.28TT 270149.473.40.014800.09
207-1257A-18X-1, 118157.28TT 300163.975.50.011400.18
207-1257A-18X-1, 118157.28TT 330180.476.90.011900.09
207-1257A-18X-1, 118157.28TT 360160.774.60.011700.08
207-1257A-18X-1, 118157.28TT 400187.470.50.013300.07
207-1257A-18X-3, 110160.20NRM 0149.883.90.034200.13
207-1257A-18X-3, 110160.20AF 50186.082.40.010600.22Steep down, indeterminate
207-1257A-18X-3, 110160.20TT 150184.367.30.006740.17
207-1257A-18X-3, 110160.20TT 150173.463.30.006880.26
207-1257A-18X-3, 110160.20TT 200218.265.10.004380.27Weak after 150°C
207-1257A-18X-3, 110160.20TT 200222.661.50.004110.29Stable DII, no decay
207-1257A-18X-3, 110160.20TT 240217.460.30.004250.19N?
207-1257A-18X-3, 110160.20TT 240208.659.60.004380.18
207-1257A-18X-3, 110160.20TT 300216.959.60.003650.16
207-1257A-18X-3, 110160.20TT 300204.966.10.003480.17
207-1257A-18X-5, 133163.39NRM 0177.278.10.057500.01
207-1257A-18X-5, 133163.39AF 50210.780.50.014200.05
207-1257A-18X-5, 133163.39TT 150132.777.80.013500.29
207-1257A-18X-5, 133163.39TT 150130.873.00.010100.06Steep down, indeterminate
207-1257A-18X-5, 133163.39TT 200110.061.10.009720.17
207-1257A-18X-5, 133163.39TT 200109.062.70.010000.07NPP
207-1257A-18X-5, 133163.39TT 240125.050.40.006250.21
207-1257A-18X-5, 133163.39TT 240118.948.80.007040.16
207-1257A-18X-5, 133163.39TT 270126.242.50.006280.35Seems linear => N??
207-1257A-18X-5, 133163.39TT 270123.743.30.006040.40
207-1257A-18X-5, 133163.39TT 300136.859.10.004590.43Weak, high errors
207-1257A-18X-5, 133163.39TT 300146.662.20.004670.30
207-1257A-18X-5, 133163.39TT 330139.555.90.004110.38
207-1257A-18X-5, 133163.39TT 330135.552.20.003740.40
207-1257A-18X-5, 133163.39TT 360139.542.60.003190.53
207-1257A-18X-5, 133163.39TT 400108.852.50.004860.25
207-1257A-18X-5, 133163.39TT 400108.654.00.004510.36
207-1257A-18X-7, 24165.30NRM 0117.352.60.048200.06Relatively strong, and low-angle
207-1257A-18X-7, 24165.30AF 50107.929.60.025000.13Looks N-type
207-1257A-18X-7, 24165.30TT 150121.219.10.022100.07N (Suganuma had NP, but Jim decided to lean towards his comments)
207-1257A-18X-7, 24165.30TT 200129.422.20.015700.07
207-1257A-18X-7, 24165.30TT 240128.822.50.014300.05
207-1257A-18X-7, 24165.30TT 300130.526.70.012300.04
207-1257A-19X-1, 136166.86NRM 0151.2-29.10.029200.08
207-1257A-19X-1, 136166.86AF 50137.6-56.60.029400.04Begins NEGATIVE
207-1257A-19X-1, 136166.86TT 150166.0-63.00.024500.04
207-1257A-19X-1, 136166.86TT 200174.2-65.90.019600.08General behavior looks N
207-1257A-19X-1, 136166.86TT 240153.2-63.50.015900.04Weird
207-1257A-19X-1, 136166.86TT 270167.3-64.10.017400.12indeterminate
207-1257A-19X-1, 136166.86TT 300181.2-63.20.015900.09
207-1257A-19X-1, 136166.86TT 330200.9-61.90.012800.09
207-1257A-19X-1, 136166.86TT 360184.8-70.60.009810.13
207-1257A-19X-1, 136166.86TT 400199.3-65.70.009280.11
207-1257A-20X-1, 26175.46NRM 0345.153.50.162000.10
207-1257A-20X-1, 26175.46AF 50346.937.70.081700.11Nice N, essentially stable Decl NRM to 240°C
207-1257A-20X-1, 26175.46TT 150343.038.10.060800.07N
207-1257A-20X-1, 26175.46TT 200341.637.10.055500.10
207-1257A-20X-1, 26175.46TT 240340.838.60.053900.05
207-1257A-20X-1, 26175.46TT 300334.735.20.044600.06