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Abrahamsen, Niels; Sager, William W (1994): (Table 1) Estimates of the duration of the Cobb Mountain Event in ODP Leg 135 holes [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.803175, In supplement to: Abrahamsen, N; Sager, WW (1994): Cobb mountain geomagnetic polarity event and transitions in three deep-sea sediment cores from the Lau Basin. In: Hawkins, J; Parson, L; Allan, J; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 135, 737-762, https://doi.org/10.2973/odp.proc.sr.135.122.1994

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Project(s):
Coverage:
Median Latitude: -20.586000 * Median Longitude: -176.829333 * South-bound Latitude: -20.827000 * West-bound Longitude: -176.890000 * North-bound Latitude: -20.222000 * East-bound Longitude: -176.775000
Date/Time Start: 1991-01-09T09:30:00 * Date/Time End: 1991-01-17T16:00:00
Minimum Elevation: -2764.0 m * Maximum Elevation: -2334.0 m
Event(s):
135-837A  * Latitude: -20.222000 * Longitude: -176.823000 * Date/Time Start: 1991-01-09T09:30:00 * Date/Time End: 1991-01-10T11:10:00 * Elevation: -2764.0 m * Penetration: 84 m * Recovery: 83.9 m * Location: South Pacific Ocean * Campaign: Leg135 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 9 cores; 84 m cored; 0 m drilled; 99.9 % recovery
135-838A  * Latitude: -20.827000 * Longitude: -176.890000 * Date/Time Start: 1991-01-12T06:45:00 * Date/Time End: 1991-01-13T16:25:00 * Elevation: -2334.0 m * Penetration: 153.8 m * Recovery: 98.65 m * Location: South Pacific Ocean * Campaign: Leg135 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 20 cores; 153.8 m cored; 0 m drilled; 64.1 % recovery
135-839A  * Latitude: -20.709000 * Longitude: -176.775000 * Date/Time Start: 1991-01-15T22:30:00 * Date/Time End: 1991-01-17T16:00:00 * Elevation: -2629.0 m * Penetration: 218.2 m * Recovery: 98.82 m * Location: South Pacific Ocean * Campaign: Leg135 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 25 cores; 218.2 m cored; 0 m drilled; 45.3 % recovery
Comment:
Data are based upon the reversal stratigraphy between Jaramillo (young) and Cobb Mountain. For Section C3 the deposition rate is corrected for the presence of ca. 1 m of volcaniclastic sediments between 39 and 40 mbsf.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
Event labelEvent
Sample code/labelSample labelAbrahamsen, NielsDSDP/ODP/IODP sample designation
SectionSectAbrahamsen, NielsCobb mountain event
Depth, relativeDepth relmAbrahamsen, Nielsminimum depth of Cobb Mountain event in section
Depth, relativeDepth relmAbrahamsen, Nielsmaximum depth of Cobb Mountain event in section
Sedimentation rateSRcm/kaAbrahamsen, Nielsdeposition rate between end of Jaramillo Subchron = 0.91 Ma and age of Cobb Mountain = 1.12 Ma
Sedimentation rate, standard deviationSR std dev±Abrahamsen, Niels
DurationDurationkaAbrahamsen, Nielsof Cobb Mountain Event
Size:
21 data points

Data

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


Event

Sample label

Sect
(Cobb mountain event)

Depth rel [m]
(minimum depth of Cobb Mountai...)

Depth rel [m]
(maximum depth of Cobb Mountai...)

SR [cm/ka]
(deposition rate between end o...)

SR std dev [±]

Duration [ka]
(of Cobb Mountain Event)
135-837A 135-837A-3H-5C10.841.171.550.0521.3
135-838A 135-838A-3H-6C20.991.301.850.0516.8
135-839A 135-839A-5H-6C30.510.792.500.2012.9