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

Rea, David K; Leinen, Margaret W (1986): (Table 3) Stratigraphy, sedimentation rates, and mass accumulation rates from DSDP Leg 92 holes [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.792732, Supplement to: Rea, DK; Leinen, MW (1986): Neogene controls on hydrothermal activity and paleoceanography of the Southeast Pacific Ocean. In: Leinen, M; Rea DK; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 92, 597-617, https://doi.org/10.2973/dsdp.proc.92.140.1986

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

Published: 1986 (exact date unknown)DOI registered: 2012-11-14

RIS CitationBibTeX Citation ShareShow MapGoogle Earth

Abstract:
The Glomar Challenger crossed the East Pacific Rise at 19°S on Leg 92 during the austral fall of 1983. The intent of the cruise was to recover sediments and rocks that would reveal the geologic history of seafloor hydrothermal activity as determined by the geochemistry and sedimentation history of hydrothermal material, the advection of sediment pore waters, the nature and history of alteration of seafloor basalt, and the paleoceanography of the southeast Pacific.
Results show that the composition of hydrothermal material is determined by its source and modified by exposure to seawater during transport in the water column. The flux of hydrothermal sediment appears to increase during episodes of tectonic activity and ridge jumps but to be independent of spreading rate. Pore water advection in sediment may occur early in the depositional history of a site, but it does not appear to continue for more than 1 or 1.5 m.y.
The basaltic rocks recovered are mostly low-olivine tholeiites, but those recovered at two sites contain ferrobasalt and alkali basalt. Hole 597C is the deepest penetration by the Deep Sea Drilling Project of fast-spreading crust. Basalts from that hole reveal three stages of alteration: an early deuteric stage, a reducing stage, and a later oxidative stage. K/Ar dates of alteration minerals suggest that alteration continues for 9 to 15 m.y. after the formation of crust.
Paleoceanographic studies have defined the Neogene history of the compensation depth and lysocline, the timing of important changes in atmospheric transport processes, and the nature and age of significant intervals of reworking in the abyssal sediments.
Project(s):
Coverage:
Median Latitude: -19.022220 * Median Longitude: -121.607580 * South-bound Latitude: -19.451500 * West-bound Longitude: -129.770500 * North-bound Latitude: -18.806300 * East-bound Longitude: -116.840800
Date/Time Start: 1983-03-02T00:00:00 * Date/Time End: 1983-03-25T00:00:00
Minimum DEPTH, sediment/rock: 0.50 m * Maximum DEPTH, sediment/rock: 41.25 m
Event(s):
92-597  * Latitude: -18.806300 * Longitude: -129.770500 * Date/Time: 1983-03-02T00:00:00 * Elevation: -4166.0 m * Penetration: 54.7 m * Recovery: 41.8 m * Location: South Pacific Ocean * Campaign: Leg92 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 7 cores; 45.1 m cored; 9.6 m drilled; 92.7 % recovery
92-598  * Latitude: -19.004700 * Longitude: -124.676800 * Date/Time: 1983-03-17T00:00:00 * Elevation: -3699.0 m * Penetration: 52.4 m * Recovery: 41.2 m * Location: South Pacific Ocean * Campaign: Leg92 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 8 cores; 52.4 m cored; 0 m drilled; 78.7 % recovery
92-599  * Latitude: -19.451500 * Longitude: -119.881300 * Date/Time: 1983-03-20T00:00:00 * Elevation: -3654.0 m * Penetration: 46.3 m * Recovery: 34.8 m * Location: South Pacific/PLATEAU * Campaign: Leg92 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 5 cores; 46.3 m cored; 0 m drilled; 75.1 % recovery
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
Event labelEvent
Latitude of eventLatitude
Longitude of eventLongitude
Elevation of eventElevationm
Depth, top/minDepth topmRea, David K
Depth, bottom/maxDepth botmRea, David K
DEPTH, sediment/rockDepth sedmGeocode – mbsf
Sample code/labelSample labelRea, David KDSDP/ODP/IODP sample designation
Sample code/label 2Sample label 2Rea, David KDSDP/ODP/IODP sample designation
10 Sediment thicknessSed thickmRea, David K
11 Nannofossil zoneNannos zoneRea, David K
12 PorosityPoros% volRea, David K
13 Density, dry bulkDBDg/cm3Rea, David K
14 Age, minimum/youngAge minkaRea, David KLeg 92 zonations
15 Age, maximum/oldAge maxkaRea, David KLeg 92 zonations
16 AGEAgeka BPGeocode
17 DurationDurationkaRea, David KLeg 92 zonations
18 Sedimentation rateSRcm/kaRea, David KLeg 92 zonations
19 Accumulation rate, massMARg/cm2/kaRea, David KLeg 92 zonations
20 Age, minimum/youngAge minkaRea, David KZonations from Berggren et al. (1985)
21 Age, maximum/oldAge maxkaRea, David KZonations from Berggren et al. (1985)
22 AGEAgeka BPGeocode
23 DurationDurationkaRea, David KZonations from Berggren et al. (1985)
24 Sedimentation rateSRcm/kaRea, David KZonations from Berggren et al. (1985)
25 Accumulation rate, massMARg/cm2/kaRea, David KZonations from Berggren et al. (1985)
Size:
452 data points

Data

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


Event

Latitude

Longitude

Elevation [m]

Depth top [m]

Depth bot [m]

Depth sed [m]
(mbsf)

Sample label

Sample label 2
10 
Sed thick [m]
11 
Nannos zone
12 
Poros [% vol]
13 
DBD [g/cm3]
14 
Age min [ka]
(Leg 92 zonations)
15 
Age max [ka]
(Leg 92 zonations)
16 
Age [ka BP]
17 
Duration [ka]
(Leg 92 zonations)
18 
SR [cm/ka]
(Leg 92 zonations)
19 
MAR [g/cm2/ka]
(Leg 92 zonations)
20 
Age min [ka]
(Zonations from Berggren et al...)
21 
Age max [ka]
(Zonations from Berggren et al...)
22 
Age [ka BP]
23 
Duration [ka]
(Zonations from Berggren et al...)
24 
SR [cm/ka]
(Zonations from Berggren et al...)
25 
MAR [g/cm2/ka]
(Zonations from Berggren et al...)
92-597 -18.8063-129.7705-41660.01.50.7592-597-1-1,15092-597-1-1,1501.5<CN3/480.70.5110142007100142000.0110.0050142007100142000.0110.005
92-597-18.8063-129.7705-41661.54.12.8092-597-1-2,092-597-1-3,1102.6CN3 + 470.80.77414200170001570028000.0930.07214200172001570030000.0870.067
92-597-18.8063-129.7705-41664.115.59.8092-597-1-3,11092-597-3-1,13011.4CN261.31.02617000187001810017000.6710.68817200190001810018000.6330.650
92-597-18.8063-129.7705-416615.519.217.3592-597-3-1,13092-597-3-4,503.7CNIc58.01.11318700220002060033000.1120.12519000222002060032000.1160.129
92-597-18.8063-129.7705-416619.227.823.5092-597-3-4,5092-597-4-3,1008.6CNla + b60.31.05220000248002350028000.3070.32322200248002350026000.3310.348
92-597-18.8063-129.7705-416627.854.741.2592-597-4-3,10092-597-CC26.9CP19b63.20.9752480028300267003500>0.769>0.7502480028600267003800>0.708>0.690
92-598 -19.0047-124.6768-36990.01.00.5092-598-1-1,092-598-1-1,1001.0<CN13-1577.40.5990188094018800.0530.0320188094018800.0530.032
92-598-19.0047-124.6768-36991.04.72.8592-598-1-1,10092-598-1-4,203.7CN10-1274.80.66818805400364035200.1050.07018805400364035200.1050.070
92-598-19.0047-124.6768-36994.76.45.5592-598-1-4,2092-598-2-1,201.7CN9b66.60.88554006700605013000.1310.11654006700605013000.1310.116
92-598-19.0047-124.6768-36996.49.07.7092-598-2-1,2092-598-2-2,1302.6CN9a67.80.85367008100740014000.1860.15967008100740014000.1860.159
92-598-19.0047-124.6768-36999.012.410.7092-598-2-2,13092-598-2-5,203.4CN8a + b67.90.85181009200865011000.3090.26381009200865011000.3090.263
92-598-19.0047-124.6768-369912.416.014.2092-598-2-5,2092-598-3-1,203.6CN7a + b66.60.8859200107001060015000.2400.2129200120001060028000.1290.114
92-598-19.0047-124.6768-369916.017.016.5092-598-3-1,2092-598-3-1,1201.0CN668.50.83510700120001225013000.0770.0641200012500122505000.2000.167
92-598-19.0047-124.6768-369917.029.723.3592-598-3-1,12092-598-4-3,13012.7CN5a + b72.40.73112000142001335022000.5770.42212500142001335017000.7470.546
92-598-19.0047-124.6768-369929.752.441.0592-598-4-3,13092-598-CC22.7CN3-474.80.66814200170001570028000.811>0.5421420017200157003000>0.757>0.505
92-599 -19.4515-119.8813-36540.01.00.5092-599-1-1,092-599-1-1,1001.0CN13-1563.30.97302880144018800.0530.0521440
92-599-19.4515-119.8813-36541.02.81.9092-599-1-1,092-599-1-1,1301.8CN11-1264.00.95418803700279018200.0990.0942790
92-599-19.4515-119.8813-36542.811.97.3592-599-1-2,13092-599-2-3,1009.1CN1066.20.89637005400455017000.5350.4794550
92-599-19.4515-119.8813-365411.930.821.3592-599-2-3,10092-599-4-3,7018.9CN9b70.80.77454006700605013001.4541.1256050
92-599-19.4515-119.8813-365430.834.832.8092-599-4-3,7092-599-4-6,204.0CN9a70.70.77667008100740014000.2860.2227400
92-599-19.4515-119.8813-365434.840.837.8092-599-4-6,2092-599-CC6.0CN8b70.70.776810086008350500>1.200>0.9318350
92-600C -18.9283-116.8408-33980.04.42.2092-600C-1-1,092-600C-1-3,1404.4CN13-1568.20.8430188094018800.2520.212940
92-600C-18.9283-116.8408-33984.44.84.6092-600C-1-3,14092-600C-1-4,300.4CN1266.80.88018803500269016200.0250.0222690
92-600C-18.9283-116.8408-33984.86.35.5592-600C-1-4,3092-600C-1-5,301.5CN1167.90.8513500370036002000.7500.6383600
92-600C-18.9283-116.8408-33986.319.012.6592-600C-1-5,3092-600C-CC12.7CN10c + d72.60.7263700460041509001.411>1.0244150
92-601 -18.9203-116.8685-34330.08.04.0092-601-1-1,092-601-1-6,368.0CN13-1566.30.8930188094018800.4260.380940
92-601-18.9203-116.8685-34338.08.98.4592-601-1-6,3692-601-1-6,1260.9CN1266.70.88218803500269016200.0560.0492690
92-601-18.9203-116.8685-34338.910.59.7092-601-1-6,12692-601-2-1,701.6CN1168.30.8403500370036002000.8000.6723600
92-601-18.9203-116.8685-343310.520.415.4592-601-2-1,7092-601-CC9.9CN10c + d71.70.750370046004150900>1.100>0.8254150