Not logged in
PANGAEA.
Data Publisher for Earth & Environmental Science

Hailwood, Ernie A; Clement, Bradford M (1991): (Table 1) Polarity transitions of ODP Hole 114-699A. PANGAEA, https://doi.org/10.1594/PANGAEA.734970, In supplement to: Hailwood, EA; Clement, BM (1991): Magnetostratigraphy of sites 699 and 700, East Georgia Basin. In: Ciesielski, PF; Kristoffersen, Y; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 114, 337-357, https://doi.org/10.2973/odp.proc.sr.114.155.1991

Always quote citation above when using data! You can download the citation in several formats below.

RIS CitationBibTeX CitationShow MapGoogle Earth

Project(s):
Coverage:
Latitude: -51.542000 * Longitude: -30.677000
Date/Time Start: 1987-03-20T10:45:00 * Date/Time End: 1987-03-26T15:29:00
Minimum DEPTH, sediment/rock: 10.59 m * Maximum DEPTH, sediment/rock: 464.65 m
Event(s):
114-699A * Latitude: -51.542000 * Longitude: -30.677000 * Date/Time Start: 1987-03-20T10:45:00 * Date/Time End: 1987-03-26T15:29:00 * Elevation: -3716.0 m * Penetration: 518.1 m * Recovery: 356.52 m * Location: South Atlantic Ocean * Campaign: Leg114 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 56 cores; 518.1 m cored; 0 m drilled; 68.8 % recovery
Comment:
Transitions interpolated within coring or sampling gaps can be identified from the associated large range of uncertainty. Boundaries of thin or otherwise poorly defined polarity intervals are indicated by a query
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
DEPTH, sediment/rockDepth sedmGeocode
Standard deviationStd dev±Hailwood, Ernie A
PolarityPolarityHailwood, Ernie Adownward change in polarity
Size:
84 data points

Data

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


Depth sed [m]

Std dev [±]

Polarity
10.590.15N-R
19.590.25R-N
21.190.05N-R
29.450.30R-N
40.690.15N-R
43.99?0.05R-N
53.610.53R-N
58.010.07N-R
60.860.21R-N
62.390.05N-R
68.840.10N-R
70.290.05R-N
87.570.27R-N
91.170.63N-R
92.490.15R-N
94.470.03N-R
115.350.45R-N
116.220.18N-R
118.090.05R-N
118.490.15N-R
119.240.10R-N
127.690.15N-R
137.090.05R-N
142.740.10R-N
143.050.10N-R
143.840.10R-N
145.730.08N-R
146.210.04R-N
156.140.10N-R
166.950.75R-N
182.690.35N-R
189.340.10R-N
192.550.10N-R
193.050.10R-N
195.550.10N-R
197.000.05R-N
198.351.55N-R
208.090.25R-N
216.050.75N-R
284.550.86N-R
434.680.20N-R
464.650.63N-R