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Establishment of a Geological Model
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The designations employed and the p
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PART II Chapter 7 Chapter 8 Chapter
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FOREWORD Welcoming remarks and addr
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Introductory remarks by His Excelle
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PARTICIPANTS Mrs. Naomi Atauea, Min
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South Pacific Applied Geoscience Co
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waters, where biological activity i
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At the Workshop, R
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the results of resource assessment
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deposits in the CCZ, illustrating t
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soft and hard. This transparent lay
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athed by cold water, around 4 degre
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export productivity - the part of t
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activity in the CCZ, seabed topogra
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CHAPTER 2 THE INTERNATIONAL SEABED
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eserved area and for their individu
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station, that is, nickel, copper, c
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Figure 9 illustrates the different
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Pioneer investors also provided bat
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order to identify possible discrepa
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Utilizing these statistics, Mr. de
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CHAPTER 3 A RESOURCE MODEL FOR DEEP
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The reserved areas are delimited by
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Figure 5: Bathymetric map of Blocks
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Considering the available data sets
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3,200 million tonnes of nodules (av
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Table 1 Global resource model resul
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22 23 Figure 18: Resource model sho
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unlikely that major decisions will
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geological model (Figure 19) to be,
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Recalling Mr. de Souza’s presenta
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The Resource Model • Array of cel
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Copper grade Figure 33 Cobalt grade
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He further said that, in land‐bas
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lock Block 16 Block 17 Block 18 Blo
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CHAPTER 4 REQUIREMENTS FOR DATA SUB
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Data requirements The Authority rec
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Quality of data to be submitted to
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SUMMARY OF PRESENTATION Mr. Diène
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• The programme of work and any c
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CHAPTER 5 GEOLOGICAL MODEL INPUTS D
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Total sediment thickness. Growth of
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- Page 101 and 102: Figure 1 presents a summary chart o
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- Page 111 and 112: eserved areas. With regard to singl
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- Page 117 and 118: information necessary for the devel
- Page 119 and 120: Ocean floor morphology The CCZ is a
- Page 121 and 122: According to the Geostat analysis (
- Page 123 and 124: Figure 12: Comparison of the reserv
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- Page 127 and 128: From the earlier stages of sediment
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- Page 131 and 132: Figure 25: Manganese and Copper As
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- Page 135 and 136: Copper The copper content of the no
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- Page 143 and 144: Halbach, P., Ozkara, M. and Rehm, E
- Page 145 and 146: Yubko ,V.M. and Lygina, T.I., 2002,
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- Page 171 and 172: layers. Nevertheless, enough organi
- Page 173 and 174: Banerjee, R., Roy, S., Dasgupta, S.
- Page 175 and 176: Professor Cronan said that the larg
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- Page 179 and 180: . Figure 1: Location of survey area
- Page 181 and 182: Figure 3: Schematic core diagram fo
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- Page 185 and 186: The earliest nodule growth around n
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The particle flux in each zone is a
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In area SO‐25‐1 the age of the
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used as marker reflectors for the d
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If one assumes that the total area
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needs to correlate those functions.
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These experts should be invited by
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of the paper for his presentation.
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According to Professor Beiersdorf,
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Professor Hoffert said that a compa
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Figure 1: Location of sectors of Co
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Sediments In the eastern area, thre
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Fe > Mg > Mn to form a series of 5.
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Distribution of the genetic types o
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A gradual increase in contribution
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increases (from 10.3 to 46.8 per ce
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are found. The general north‐sout
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that IOM had been granted pioneer i
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Kotliński, the hydrogenetic, small
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CHAPTER 13 REGIONAL AND LOCAL TREND
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The types of regional zoning made a
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Figure 8b: Scheme of ore accumulati
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other from the north to the south a
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Figure 15: Geomorphological scheme
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Figure 20: Buried downcuttings, str
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topographic feature in the south, w
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测 站 数 180 160 140 120 100 80
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(a) Large amounts of basic volcanic
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Professor Lu identified the main co
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suggest that the organic matter con
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Prospecting criteria Prospecting cr
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According to Dr. Verlaan, the start
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The final element discussed by Dr.
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EXAMPLES OF LOW RATES - - infaunal
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- Very high local species diversity
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Extrapolation yields an estimated 1
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Apparent ranges of polychaete speci
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In addition to studying the three f
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‐ Distribution and diversity of m
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Because deep‐sea benthos are food
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Megafauna, NW Atlantic slope: (a) X
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“Macrofauna” = animals retained
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Characteristics of Deep Seafloor -
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disturbance, from being inundated b
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ought back in samples from the Paci
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Dr. Smith said there were additiona
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CHAPTER 17 POLYMETALLIC NODULES RES
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Bathymetric and nodule distribution
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Resources A resource evaluation was
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He showed the generalized bathymetr
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Dr. Kodagali said that, for the net
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CHAPTER 18 THE CHINA OCEAN MINERAL
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Deposit: Ore: distribution and cove
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Ni‐equivalent abundance The Ni‐
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Result Based on the data and inform
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Table 1: Tonnage and tonnage per un
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Table 6 Resource amount in blocks o
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Compared with other areas in the CC
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CHAPTER 19 POLYMETALLIC NODULE RESO
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3. The Manihiki Plateau, in the nor
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environments and their impact on oc
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Figure 6: Submarine geomorphologic
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The Cook Islands nodules and those
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Table 1 Comparison of the Cook Isla
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structure and large spiral loops Hi
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Glasby, G.P. et.al., 1986, “Geolo
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the major topographic feature of th
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In conclusion, Dr. Clark stressed t
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The group viewed the carbonate comp
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interpretation and analysis of the
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the geological model. In particular
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In terms of nodule data, let me jus
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very intense, and the waters are ne
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• Complete documentation of metho
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young oceanic plate, with the crust
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Volcanic Activity The general struc
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Data Sources Data sources to be inc
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‐ Transparent‐layer materials a
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• Universities and Institutions
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‐ An evaluation of palaeo to rece
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• Distance of seafloor from CCD
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• Collaborate on a regular basis
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Improved resource assessment The im
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With regard to the programme of wor
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group thinking about how it wanted
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perhaps elsewhere; it could also pr
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processes with geological and benth
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Alf Simpson Director SOPAC Secretar