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Full page fax print - International Seabed Authority

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An important consideration in the exploration and exploitation of potential crust<br />

resources is the contrast in physical properties between crusts and substrate rocks. Those<br />

comparisons are complicated by the fact that crusts grow on a wide variety of substrates<br />

including breccia, basalt, phosphorite, limestone, hyaloclastite, and mudstone in that<br />

order of abundance. Phosphorite and fresh basalt are strong, competent rocks and<br />

contrast significantly with crusts, which are weak, light-weight, and porous (Table 4); the<br />

other rock types, including altered basalt, may not contrast much in physical properties<br />

with Fe-Mn crusts. In general, crusts are much more porous (mean 60%) than most<br />

substrate rocks and have an extreme amount of specific surface area, which averages<br />

about 300 m 2/g (Table 4), similar to the surface area of silica gel. The surface area<br />

decreases by up to 20% when measured one month after collection of the crust and up to<br />

40% after two months 45. This clearly shows that many physical properties that are<br />

measured a long time after collection of the crusts may not closely approximate in situ<br />

crust properties. The mean wet bulk density of crusts is 1.90 g/cm 3 and the mean dry<br />

bulk density is 1.30 g/cm 3. The P-wave velocity of crusts may be less or more than that of<br />

sedimentary substrate rocks, but is generally less than that of basalt. This variable<br />

contrast will make it difficult to develop sonic devices for measuring in situ crust<br />

thicknesses. The most distinctive property of Fe-Mn crusts is their gamma radiation<br />

level, which averages 475 net counts/min in contrast to sedimentary rock substrates 101<br />

and basalt substrates ( 146; Table 4). Gamma radiation may be a useful tool for crust<br />

exploration under thin-sediment cover and for measuring crust thicknesses in situ.<br />

Table 4. Physical properties of Fe-Mn crusts and substrate rocks, from Hein et al. 37<br />

Physical Properties n<br />

Fe-Mn<br />

Crusts<br />

n<br />

Sed. rock<br />

substrate<br />

<strong>International</strong> <strong>Seabed</strong> <strong>Authority</strong> 51<br />

n<br />

Basalt<br />

substrate<br />

Porosity (volume %)<br />

Range 13 52-66 8 18-47 2 15-37 38<br />

Mean 13 61 8 39 2 26 38<br />

- 41-74 - 7-69 - 7-67 39<br />

- 55 - 35 - - 40<br />

Wet bulk density (g/cm 3 )<br />

Range 13 1.83-2.04 8 2.04-2.57 2 2.22-2.62 38<br />

Mean 13 1.92 8 2.18 2 2.42 38<br />

Range 18 1.90-2.44 7 1.59-2.68 23 2.06-2.66 41<br />

Mean 18 2.00 7 1.90 23 2.34 41<br />

Dry bulk density (g/cm 3 )<br />

Range 13 1.18-1.48 8 1.56-2.38 2 1.84-2.46 38<br />

Mean 13 1.29 8 1.78 2 2.15 38<br />

- 1.31 - - - - 40<br />

Ref.

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