Minerals Report - International Seabed Authority
Minerals Report - International Seabed Authority Minerals Report - International Seabed Authority
distances of hundreds of kilometres from a source. These components can be detected in water samples recovered from appropriate depths by standard shipboard water sampling methods. Certain of these metallic mineral particles from black smokers will settle through the water column to the seafloor where the metallic mineral component can be detected in cores of seafloor sediments. The general location of seafloor hot springs can found by following concentration gradients of these metallic signals in the water column and in seafloor sediments. At ranges of tens to several kilometres (thickness of the water column in the deep ocean), shipboard bathymetric and magnetic methods and near-surface towed side-scan sonar can be employed to determine the seafloor setting and detect a characteristic magnetic signature ( 17/ , 18/ ) of either an active or inactive massive sulphide deposit. When within kilometres of the hot springs, various in situ sampling (water, particles, seafloor sediment) and imaging (photos, video, and side-scan sonar) methods can be used on various types of unmanned deep submergence vehicles at altitudes up to tens of meters above the seafloor to locate the massive sulphide deposit. These unmanned deep submergence vehicles comprise Remotely Operated Vehicles (ROV) which are tethered to the ship and controlled though an electrical or electro-fibre optic cable with a real-time video link to the operators, and Autonomous Underwater Vehicles (AUV) which are free-swimming and are programmed to perform imaging, sampling and other measurement procedures. Manned submersibles, also known as Human Occupied Vehicles (HOV), may be used for direct observation, sampling and measurements after the massive sulphide deposit has been targeted (15). 2) Characterizing the deposit: Having found the marine mineral deposit, the next objective is to accurately determine the detailed physical, chemical and, in cases, biological properties of the deposit and its seafloor setting. This may be accomplished using the "nested survey" strategy, which starts with surveying the seafloor setting of the deposit and progressively obtains more detailed information of the deposit itself employing many of the same exploration methods used to find the deposit ( 19/ ). Following through with the case of the deep ocean massive sulphide deposit, the exploration methods described so far provide direct information on that part of the massive sulphide deposit exposed on the seafloor and only indirect information on the portion beneath the seafloor. Recall that in INTERNATIONAL SEABED AUTHORITY 86
describing the active sulphide mound in the TAG hydrothermal field, the surface expression is only the "tip of the iceberg" (Figure 3). Drilling is required to directly determine the third dimension including grade and tonnage of a massive sulphide deposit on the seafloor just as for such as deposit on land. For massive sulphide bodies on land hundreds of holes each tens to hundreds of meters long spaced meters apart may be drilled to recover almost continuous cores of the material penetrated. These cores are used to determine the shape, grade and tonnage of the massive sulphide mound and underlying feeder/stockwork zone (Figure 3). Present capability to drill a massive sulphide body at a water depth of several kilometres in the deep ocean is far more limited. For example, the active sulphide mound in the TAG hydrothermal field is one of only two such mounds that have been drilled to date by the Ocean Drilling Program (ODP). ODP Leg 158 spent two months at sea in 1994 and with formidable technical difficulty drilled 17 holes up to 125 meters long with overall core recovery of 12 percent ( 7/ ). Drilling methods for massive sulphide deposits and associated volcanic rocks in the deep ocean are being improved, but will fall far short of land standards for the foreseeable future. 6. Environmental Considerations Marine organisms are associated with marine mineral deposits and must be considered with reference to exploration and mining activities. Some observations of biodiversity of these organisms in the context of seafloor settings exclusive of and associated with deep ocean hot springs are, as follows: 1) Deep ocean exclusive of hot springs: • Marine species diversity in the deep ocean is comparable to that in tropical rainforests ( 20/ ). • The species diversity of marine life is so high that an investigation found new species in every square meter of seafloor sediment sampled ( 21/ ). INTERNATIONAL SEABED AUTHORITY 87
- Page 44 and 45: athymetric map of the seafloor. A s
- Page 46 and 47: were encouraging. In the course of
- Page 48 and 49: that this matter was sensitive, he
- Page 50 and 51: complete a preliminary evaluation o
- Page 52 and 53: metals - nickel, cobalt, manganese,
- Page 54 and 55: 12. Issues to be taken into account
- Page 56 and 57: entities. Many of them included min
- Page 58 and 59: In this regard, the Secretary-Gener
- Page 60 and 61: According to Dr. Vysotsky, as estim
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- Page 70 and 71: geochemical and geotechnical survey
- Page 72 and 73: of its continental shelf through bi
- Page 74 and 75: also stated, is similar to that of
- Page 76 and 77: Chapter 7 Technical requirements fo
- Page 78 and 79: Table 1: Classification of marine m
- Page 80 and 81: Volcanogenic Metalliferous sediment
- Page 82 and 83: deposits, including massive sulphid
- Page 84 and 85: 3. Marine Minerals Related to Deep
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- Page 90 and 91: Figure 4. A diagrammatic east-west
- Page 92 and 93: and refining of these crusts is mor
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- Page 98 and 99: 6. P.A. Rona, M.D. Hannington, C.V.
- Page 100 and 101: 25. M.J. Cruickshank (1998), Law of
- Page 102 and 103: With regard to marine mineral depos
- Page 104 and 105: Focussing on sites of sea floor min
- Page 106 and 107: scientific journal "Nature". The su
- Page 108 and 109: Professor Rona recalled that the in
- Page 110 and 111: like St. Stephen’s in the Kremlin
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- Page 114 and 115: The reasons why the Red Sea deposit
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- Page 124 and 125: Due to its increased buoyancy at hi
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describing the active sulphide mound in the TAG hydrothermal field, the<br />
surface expression is only the "tip of the iceberg" (Figure 3). Drilling is<br />
required to directly determine the third dimension including grade and<br />
tonnage of a massive sulphide deposit on the seafloor just as for such as<br />
deposit on land. For massive sulphide bodies on land hundreds of holes<br />
each tens to hundreds of meters long spaced meters apart may be drilled<br />
to recover almost continuous cores of the material penetrated. These cores<br />
are used to determine the shape, grade and tonnage of the massive<br />
sulphide mound and underlying feeder/stockwork zone (Figure 3).<br />
Present capability to drill a massive sulphide body at a water depth of<br />
several kilometres in the deep ocean is far more limited. For example, the<br />
active sulphide mound in the TAG hydrothermal field is one of only two<br />
such mounds that have been drilled to date by the Ocean Drilling Program<br />
(ODP). ODP Leg 158 spent two months at sea in 1994 and with<br />
formidable technical difficulty drilled 17 holes up to 125 meters long with<br />
overall core recovery of 12 percent ( 7/ ). Drilling methods for massive<br />
sulphide deposits and associated volcanic rocks in the deep ocean are<br />
being improved, but will fall far short of land standards for the foreseeable<br />
future.<br />
6. Environmental Considerations<br />
Marine organisms are associated with marine mineral deposits and<br />
must be considered with reference to exploration and mining activities. Some<br />
observations of biodiversity of these organisms in the context of seafloor<br />
settings exclusive of and associated with deep ocean hot springs are, as<br />
follows:<br />
1) Deep ocean exclusive of hot springs:<br />
• Marine species diversity in the deep ocean is comparable to<br />
that in tropical rainforests ( 20/ ).<br />
• The species diversity of marine life is so high that an<br />
investigation found new species in every square meter of<br />
seafloor sediment sampled ( 21/ ).<br />
INTERNATIONAL SEABED AUTHORITY 87