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Carlson, Richard L; Schaftenaar, C H; Moore, R P (1983): (Table 1) Physical properties at DSDP Hole 72-516F [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.811445, Supplement to: Carlson, RL et al. (1983): Causes of compressional-wave anisotropy in calcareous sediments from the Rio Grande Rise. In: Barker, PF; Carlson, RL; Johnson, DA; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 72, 565-576, https://doi.org/10.2973/dsdp.proc.72.124.1983

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Abstract:
Forty indurated sediment samples from Site 516 were studied to determine the cause of acoustic anisotropy in carbonate- bearing deep-sea sediments. Recovered from sub-bottom depths between 388 and 1222 m, the samples have properties exhibiting the following ranges: wet-bulk density, 1.90-2.49 g/cm3; fractional porosity, 0.45-0.14; carbonate content, 33-88%; compressional-wave velocity (at 0.1 kbar pressure), 1.87-4.87 km/s; and anisotropy, 1-13%. Velocities were measured in three mutually perpendicular directions through the same specimen in 29 of the 40 samples studied. Calcite fabric has been estimated by X-ray pole figure goniometry. The major findings of this study are:
1) Carbonate-bearing deep-sea sediments may be regarded as transversely isotropic media with symmetry axes normal to bedding.
2) Calcite c-axes are weakly concentrated in a direction perpendicular to bedding, but the preferred orientation of calcite does not contribute significantly to velocity anisotropy.
3) The properties of bedded and unbedded samples are distinctly different. Unbedded sediments exhibit low degrees of acoustic anisotropy (1-5%). By contrast, bedded samples show higher degrees of anisotropy (to 13%), and anisotropy increases markedly with depth of burial. Thus, bedding must be regarded as the principal cause of acoustic anisotropy in calcareous, deep-sea sediments.
Project(s):
Coverage:
Latitude: -30.276500 * Longitude: -35.285000
Date/Time Start: 1980-03-11T00:00:00 * Date/Time End: 1980-03-11T00:00:00
Minimum DEPTH, sediment/rock: 388 m * Maximum DEPTH, sediment/rock: 1222 m
Event(s):
72-516F * Latitude: -30.276500 * Longitude: -35.285000 * Date/Time: 1980-03-11T00:00:00 * Elevation: -1313.0 m * Penetration: 1270.6 m * Recovery: 690.1 m * Location: South Atlantic/CONT RISE * Campaign: Leg72 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 127 cores; 1092.5 m cored; 9 m drilled; 63.2 % recovery
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
Sample code/labelSample labelCarlson, Richard LDSDP/ODP/IODP sample designation
DEPTH, sediment/rockDepth sedmGeocode – mbsf
Density, wet bulkWBDg/cm3Carlson, Richard LAge model, biofluktuation±1%
Porosity, fractionalPoros fracCarlson, Richard L
Porosity, standard deviationPoros std dev±Carlson, Richard LFractional
Porosity, fractionalPoros fracCarlson, Richard LCalculated from regressions
Porosity, standard deviationPoros std dev±Carlson, Richard LCalculated from regressions
Velocity, compressional waveVpm/sCarlson, Richard L#1, horizontal, at 0.1 kbar, ±1%
Velocity, compressional waveVpm/sCarlson, Richard L#2, horizontal, at 0.1 kbar, ±1%
10 Velocity, compressional waveVpm/sCarlson, Richard LVertical, at 0.1 kbar, ±1%
11 DifferenceDiffCarlson, Richard LDifference of velocities
12 Standard deviationStd dev±Carlson, Richard LDifference of velocities
13 Velocity, compressional wave anisotropyVp anisotropy%Carlson, Richard L±1.2%
14 CarbonatesCarb%Carlson, Richard L±2
15 Bedding/bandingBedding/bandingCarlson, Richard L
Size:
467 data points

Data

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


Sample label
(DSDP/ODP/IODP sample designation)

Depth sed [m]
(mbsf)

WBD [g/cm3]
(±1%, Age model, biofluktuation)

Poros frac

Poros std dev [±]
(Fractional)

Poros frac
(Calculated from regressions)

Poros std dev [±]
(Calculated from regressions)

Vp [m/s]
(#1, horizontal, at 0.1 kbar, ±1%)

Vp [m/s]
(#2, horizontal, at 0.1 kbar, ±1%)
10 
Vp [m/s]
(Vertical, at 0.1 kbar, ±1%)
11 
Diff
(Difference of velocities)
12 
Std dev [±]
(Difference of velocities)
13 
Vp anisotropy [%]
(±1.2%)
14 
Carb [%]
(±2)
15 
Bedding/banding
72-516F-24-1,17-263881.900.450.011960191050202.679Unbedded sample
72-516F-25-3,44-534012.010.410.0219601960192068Bedded sample
72-516F-26-1,17-254071.990.430.03191040202.165Bedded sample
72-516F-29-1,41-514361.960.460.011940187070203.781Bedded sample
72-516F-32-1,15-254641.990.420.0220702070200070203.474Bedded sample
72-516F-34-1,25-354831.940.440.012000196040202.075Bedded sample
72-516F-41-1,85-935502.000.420.0221802070208050302.189Bedded sample
72-516F-50-1,100-1106362.060.360.0225402580247090303.684Unbedded sample
72-516F-52-3,5-146582.040.390.0223302310227050302.274Unbedded sample
72-516F-55-2,43-536842.080.330.022870280070302.570Unbedded sample
72-516F-58-1,78-887112.220.290.02250024802370120304.976Bedded sample
72-516F-60-4,112-1227262.210.290.0125202400120304.874Bedded sample
72-516F-62-2,48-567402.250.270.02265026402540110304.072Bedded sample
72-516F-70-1,22-327962.300.240.02293029502740200307.065Bedded sample
72-516F-75-4,110-1208382.420.170.0135503250260407.672Bedded sample
72-516F-78-4,1-118642.250.280.0124600243030301.264Unbedded sample
72-516F-79-2,93-1038712.330.240.01296029602750210307.365Bedded sample
72-516F-80-2,32-398792.250.230.0136603600354090402.577Unbedded sample
72-516F-83-2,70-809032.220.290.0231103090308020400.688Unbedded sample
72-516F-84-6,20-309182.200.290.0230503050297080402.682Unbedded sample
72-516F-85-1,20-309202.120.350.0226602700262060302.387Unbedded sample
72-516F-86-2,44-549312.230.280.03300030002900100403.483Unbedded sample
72-516F-87-5,112-1219462.270.260.0230303070300050401.685Unbedded sample
72-516F-90-3,123-1329712.150.330.0227202740268050301.881Unbedded sample
72-516F-91-5,78-879832.270.250.023160310060401.982Unbedded sample
72-516F-93-4,126-13510012.290.250.02247024702270200308.345Bedded sample
72-516F-100-3,44-5310482.310.270.0124302310120305.048Unbedded sample
72-516F-101-2,95-10510532.320.230.02302029902740270309.165Bedded sample
72-516F-102-2,121-13110582.300.230.022630023602703010.652Bedded sample
72-516F-103-3,30-3910632.290.240.01298030302750260308.765Bedded sample
72-516F-105-5,0-1010842.310.240.01305002790260408.857Bedded sample
72-516F-106-3,20-3010902.260.270.01309030602870210406.868Bedded sample
72-516F-107-4,125-13411012.330.220.02300030102750260308.755Bedded sample
72-516F-108-3,114-12411092.330.230.01307031102820270409.059Bedded sample
72-516F-109-3,107-11611132.320.230.013110311027503604012.063Bedded sample
72-516F-113-5,78-8711522.380.190.023630367032803604010.565Bedded sample
72-516F-116-2,110-12011752.400.200.013340341029504304013.134Bedded sample
72-516F-117-4,116-12511872.490.140.01401040103690320508.275Bedded sample
72-516F-119-3,62-7111982.430.160.02418041903950240505.778Bedded sample
72-516F-122-1,77-8612222.480.140.02487048304500350607.451Bedded sample