Full page fax print - International Seabed Authority
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The list of 46 research cruises in Table 3 is not comprehensive and data for a few<br />
cruises completed by the USSR (and later Russia) are not available to the author.<br />
However, based on an estimated 48 research cruises from 1981 through 2001, it is<br />
suggested that minimum expenditures were about US $40 million for ship and associated<br />
scientific operations related to field work, and $50 million for shore-based research, for a<br />
total investment of about $90 million.<br />
2. Fe-Mn CRUST CHARACTERISTICS<br />
2.1. Textures and Physical Properties<br />
Crust surfaces exposed directly to the seafloor are botryoidal, with botryoids<br />
varying in size from microbotryoidal (millimetre size) to botryoidal (centimetre size).<br />
Fresh growth surfaces are characterized by a fractal distribution of botryoids with<br />
extreme surface area. Under conditions of high current flow, the botryoids are modified,<br />
either by smoothing or by accentuation of the relief by erosion around the margins of the<br />
botryoids, in places producing mushroom-shaped forms. With strong uni-directional<br />
flow, the botryoids become polished and fluted. Crusts on the sides of rocks are<br />
commonly more protected from current activity and grow at a slower rate thereby<br />
acquiring very high cobalt contents; textures of those side crusts are very porous and<br />
granular.<br />
Crust profiles vary according to thickness and regional oceanographic<br />
conditions. Thin crusts (80 mm) may have up to 8 distinct macroscopic layers, the lower several<br />
layers of which are commonly phosphatised. In polished thin sections, textures consist of<br />
alternating laminated, columnar, botryoidal, and mottled textures. Columns range in<br />
height from millimetres to 50 mm 34, with detrital grains separating columns and actually<br />
promoting columnar growth 35. Mottled layers are the most porous and detritus-rich.<br />
The various textures probably reflect bottom-water conditions at the time of precipitation<br />
of the oxides. Mottled, columnar, botryoidal, and laminated textures likely represent<br />
progressively decreasing energy in the depositional environment 36.<br />
<strong>International</strong> <strong>Seabed</strong> <strong>Authority</strong> 49