Hirono, Tetsuro (2003): (Table T1) Density, porosity, void ratio, diffusivity and permeability of ODP Site 185-1149 sediments [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.784116, Supplement to: Hirono, T (2003): Data report: Measurement of mass transfer properties with subducted oceanic plate. In: Ludden, JN; Plank, T; Escutia, C (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 185, 1-14, https://doi.org/10.2973/odp.proc.sr.185.002.2003
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Abstract:
The subduction of oceanic plates regulates crustal growth, influences arc volcanism, and refertilizes the mantle. Continental growth occurs by subduction of crustal material (seawater components, marine sediments, and basaltic crust). The geochemical and physical evolution of the Earth's crust depends, in large part, on the fate of subducted material at convergent margins (Armstrong, 1968, doi:10.1029/RG006i002p00175; Karig and Kay, 1981, 10.1098/rsta.1981.0108). The crustal material on the downgoing plate is recycled to various levels in the subduction zone. The recycling process that takes place in the "Subduction Factory" is difficult to observe directly but is clearly illuminated using chemical tracers. Von Huene and Scholl (1991, doi:10.1029/91RG00969) and Plank and Langmuir (1993, doi:10.1038/362739a0) preliminarily calculated a large flux of subducted materials. By mass balancing the chemical tracers and measuring the fractionations that occur between them, the Subduction Factory work and the effect on the Earth's evolution can be estimated. In order to elucidate this mass balance, Ocean Drilling Program Leg 185 drilled two deepwater shales into the oceanic crust situated in the Mariana-Izu Trenches and recovered core samples of incoming oceanic crust. The calculations of mass circulation in the subduction zone, however, did not take into account the mass transfer properties within subducted oceanic crust, although the dewatering fluid and diffused ions may play an important role in various activities such as seismogeneity, serpentine diapiring, and arc volcanism. Thus, this paper focuses on the quantitative measurements of the physical and mass transfer properties of subducted oceanic crust.
Project(s):
Ocean Drilling Program (ODP)
Coverage:
Median Latitude: 31.334975 * Median Longitude: 143.363425 * South-bound Latitude: 31.313200 * West-bound Longitude: 143.351000 * North-bound Latitude: 31.342500 * East-bound Longitude: 143.400400
Date/Time Start: 1999-05-23T15:00:00 * Date/Time End: 1999-06-13T16:15:00
Minimum DEPTH, sediment/rock: 19.50 m * Maximum DEPTH, sediment/rock: 418.41 m
Event(s):
185-1149A * Latitude: 31.342000 * Longitude: 143.351300 * Date/Time Start: 1999-05-23T15:00:00 * Date/Time End: 1999-05-26T07:25:00 * Elevation: -5817.6 m * Penetration: 191.2 m * Recovery: 174.44 m * Location: North Pacific Ocean * Campaign: Leg185 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 23 cores; 191.2 m cored; 0 m drilled; 91.2 % recovery
185-1149B * Latitude: 31.342200 * Longitude: 143.351000 * Date/Time Start: 1999-05-26T07:25:00 * Date/Time End: 1999-06-02T20:00:00 * Elevation: -5817.5 m * Penetration: 445.2 m * Recovery: 32.93 m * Location: North Pacific Ocean * Campaign: Leg185 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 31 core; 284.6 m cored; 151.1 m drilled; 11.6 % recovery
185-1149C * Latitude: 31.342500 * Longitude: 143.351000 * Date/Time Start: 1999-06-02T20:00:00 * Date/Time End: 1999-06-07T03:00:00 * Elevation: -5817.6 m * Penetration: 426.7 m * Recovery: 6.39 m * Location: North Pacific Ocean * Campaign: Leg185 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 8 cores; 76.9 m cored; 0 m drilled; 8.3 % recovery
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Event label | Event | ||||
| 2 | Sample code/label | Sample label | Hirono, Tetsuro | DSDP/ODP/IODP sample designation | ||
| 3 | DEPTH, sediment/rock | Depth sed | m | Geocode – mbsf | ||
| 4 | Lithology/composition/facies | Lithology | Hirono, Tetsuro | |||
| 5 | Density, wet bulk | WBD | g/cm3 | Hirono, Tetsuro | ||
| 6 | Porosity | Poros | % vol | Hirono, Tetsuro | ||
| 7 | Void Ratio description | Void Ratio | Hirono, Tetsuro | |||
| 8 | Water content, wet mass | Water wm | % | Hirono, Tetsuro | ||
| 9 | Resistivity, electrical | Resist electr | Ohm m | Hirono, Tetsuro | ||
| 10 | Permeability | Permeab | cm/s | Hirono, Tetsuro | ||
| 11 | Diffusion coefficient | Diff coeff | 10-6 cm2/s | Hirono, Tetsuro | Calculated | of iodine (I-) |
| 12 | Diffusion coefficient | Diff coeff | 10-6 cm2/s | Hirono, Tetsuro | Calculated | of potassium (K+) |
| 13 | Velocity, compressional wave | Vp | m/s | Hirono, Tetsuro | ||
| 14 | Computer tomograph value | CT value | Hirono, Tetsuro | X-ray computed tomography (CT) | air = -1000, Water = 0 |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
156 data points
Data
| 1 Event | 2 Sample label (DSDP/ODP/IODP sample designation) | 3 Depth sed [m] (mbsf) | 4 Lithology | 5 WBD [g/cm3] | 6 Poros [% vol] | 7 Void Ratio | 8 Water wm [%] | 9 Resist electr [Ohm m] | 10 Permeab [cm/s] | 11 Diff coeff [10-6 cm2/s] (of iodine (I-), Calculated) | 12 Diff coeff [10-6 cm2/s] (of potassium (K+), Calculated) | 13 Vp [m/s] | 14 CT value (air = -1000, Water = 0, X-ray...) |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 185-1149A | 185-1149A-3H-4 | 19.50 | Clay | 1.46 | 72.9 | 2.69 | 51.2 | 68.65 | 0.0000014400 | 1.380000 | 1.350000 | 1532 | 696 |
| 185-1149A | 185-1149A-8H-4 | 67.10 | Clay | 1.43 | 74.8 | 2.97 | 53.5 | 73.83 | 0.0000002520 | 1.370000 | 1.210000 | 1515 | 832 |
| 185-1149A | 185-1149A-13H-4 | 114.60 | Clay | 1.33 | 80.9 | 4.24 | 62.5 | 33.66 | 0.0000000751 | 0.910000 | 0.875000 | 1554 | 640 |
| 185-1149A | 185-1149A-17H-2 | 149.60 | Pelagic clay | 1.36 | 60.8 | 1.55 | 45.7 | 32.20 | 0.0000000027 | 0.625000 | 0.477000 | 1522 | 944 |
| 185-1149B | 185-1149B-3R-1 | 171.70 | Pelagic clay | 1.50 | 70.8 | 2.43 | 48.5 | 49.68 | 0.0000000004 | 0.537000 | 0.379000 | 1508 | 1328 |
| 185-1149B | 185-1149B-18R-1 | 302.81 | Chert | 2.33 | 5.1 | 0.05 | 2.2 | 3665.33 | 0.0000000000 | 0.000612 | 0.000405 | 4946 | 2000 |
| 185-1149B | 185-1149B-27R-1 | 387.60 | Chalk | 2.21 | 32.9 | 0.49 | 15.2 | 80.47 | 0.0000000609 | 0.494000 | 0.324000 | 2172 | 2016 |
| 185-1149B | 185-1149B-29R-3 | 410.58 | Basalt | 2.69 | 6.4 | 0.07 | 2.5 | 632.70 | 0.0000000000 | 0.000597 | 0.000655 | 4606 | 2781 |
| 185-1149B | 185-1149B-30R-2 | 418.33 | Basalt | 2.59 | 9.0 | 0.1 | 3.5 | 355.93 | 0.0000000000 | 0.001580 | 0.001300 | 4840 | 2641 |
| 185-1149C | 185-1149C-6R-1 | 312.87 | Porcellanite | 2.19 | 8.0 | 0.09 | 3.7 | 3491.46 | 0.0000000002 | 0.015200 | 0.014100 | 3219 | 1797 |
| 185-1149C | 185-1149C-8R-1 | 388.67 | Marl | 2.37 | 24.7 | 0.33 | 10.7 | 135.65 | 0.0000000217 | 0.448000 | 0.253000 | 2356 | 1828 |
| 185-1149C | 185-1149C-11R-1 | 418.41 | Basalt | 2.31 | 8.1 | 0.09 | 3.6 | 459.77 | 0.0000000001 | 0.003520 | 0.005710 | 5167 | 2016 |
| 185-1149D | 185-1149D-8R-1 | 330.13 | Basalt | 2.77 | 5.9 | 0.06 | 2.2 | 427.46 | 0.0000000001 | 0.000701 | 0.000659 | 4569 | 1828 |