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Intergovernmental Oceanographic Com
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of the IOC Marine Pollution Monitor
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PageMARGINAL SEASSTORM SURGES IN TH
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Marine PollutionAt present, marine
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THE INDIAN OCEAN --- AN ENVIRONMENT
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The subtropical anticyclonic gyre i
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GEOLOGICALBecause of its asymmetric
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RADIOACTIVE AND THERMAL WASTESIn co
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RESEARCH AND MONITORING ACTIVITIESM
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2-5, Mn 3-7, Zn 8-31, Fe 35-94, Pb
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Localized problems, both short-term
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HOLEMAN, J.N. (1968). The sediment
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UNEP/UNIDO (1982a). Industrial sour
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0-5-24 -I I I I I I I I I 11--25- A
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I*in '0( U N '0- '0 '0 N , p d'0I I
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C'EO IIFigure 6. Observations of oi
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Table 2.Ranges of Dissolved heavy m
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d.2 W2n2 n z0U.IzIO N m mENmIYEE*Ed
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Table 6. Population and related dat
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PROBLEMS IN THE PHYSICAL OCEANOGRAP
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B2: How does the Agulhas Current in
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0Q0mbWbvx(U49
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Figure 6 Average wind stress curl f
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THE DESTRUCTION OF THE TETHYS AND P
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part of the Seychelles-Mascarene bl
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Much of the old Tethys seafloor has
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when there was little or no movemen
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scouring of the sediments by cold b
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CANDE, S.C. and MUTTER, J.C. (1982)
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SHACKLETON, N.J. and KENNETT, J.P.
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0EYNz 10c2XaYWeKB20LuUz a5 cl300 10
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CALCAREOUS FORAMINIFERANANNOFOSSIL
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GEOLOGICAL-GEOPHYSICAL MAPPING OF T
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The latest tectonic generalization
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LE PICHON, X. and HEIRTZLER, J.R. (
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AN EXAMINATION OF THE FACTORS THAT
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is the specific volume anomaly. Po
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circulation. At Nagappattinam, Madr
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Table 1.MarmagaoCochin1969-781958-7
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tFigure 2. An idealized coastal cur
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STATION : BOMBAY~ J , F I M .- , A
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STATION : COCHIN, J , F , M , A , M
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3007STATION : MADRASI J I F , M I A
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STATION : CALCUTTA, J l F , M , A ,
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RED TIDE§ IN THE INDO-WEST PACIFIC
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were observed as early as 1770 duri
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diarrhetic shellfish poisoning (DSP
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GACUTAN, R.Q., TABBU, M.Y., AUJERO,
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Table 1.Clinical symptoms of variou
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Table 3. Fish species implicated in
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FIGURE CAPTIONSFigure la. Trichodes
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(*14aEE15aHH15c120
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MINERAL RESOURCES OF THE INDIAN OCE
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tonnes of monazite. Similar deposit
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Madagascar and the Red Sea. Within
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South Australian Basin: (Figs. 10-1
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Offshore placers are likely to occu
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MILLIMAN, J.D. (1974). Marine Carbo
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Thailand Tin 5560 (1980) NA 4.2 (19
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Table 2. The range (in percent) of
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Table 4. Chemical composition of po
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141FIGURE - 1
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~IT 73qw p' le' IS IFigure 4. Map s
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@A5 3 9 93 3 s 3 m4P 8O C ' . .' ,
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Figure 10. Map showng the abundance
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Figure 14. Map showing the distribu
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IFigure 17. Marine mineral explorat
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central are corals to the integrity
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Very little information is availabl
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leaving little trace of their exist
- Page 156 and 157: REFERENCESAGASSIZ, A. (1903). The c
- Page 158 and 159: PILLAI, C.S.G. (1969b). Studies on
- Page 160 and 161: Table 1.Extent of damage to coral r
- Page 162 and 163: STATUS OF CRITICAL MARINE HABITATS
- Page 164 and 165: OCCURRENCEThe distribution of reefs
- Page 166 and 167: Mining of Reef RockMining of reef r
- Page 168 and 169: -resource. Their significance deriv
- Page 170 and 171: Coating of Aerial Roots by Fine Sed
- Page 172 and 173: associated with the roots (e.g. GOE
- Page 174 and 175: Temperature and SalinityThe effects
- Page 176 and 177: significant numbers in the Red Sea,
- Page 178 and 179: mersas are known to serve as nurser
- Page 180 and 181: BURCHARD, J.E. (1979). Coral fauna
- Page 182 and 183: HIRTH, H.F., KLIKOFF, L.G. and HARP
- Page 184 and 185: MacNAE, W. (1974). Mangrove forests
- Page 186 and 187: RINKEVITCH, B. and LOYA, Y. (1977).
- Page 188 and 189: WALKER, D.I. and ORMOND, R.F.G. (19
- Page 190 and 191: DAMMING AND DIVERSION OF RIVERSIn d
- Page 192 and 193: FUTURE STUDIESWhat can marine scien
- Page 194 and 195: !0OD9 -8 Nc80,a,u-3(dcab(Dbrr)8brr)
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- Page 202 and 203: ACKNOWLEDGEMENTSThe writers wish to
- Page 204 and 205: Table 1.Latitude and longitude of p
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- Page 215 and 216: IIIIIIIIIIIIIIIIIIIIII3rFIIojoa222
- Page 217 and 218: Table 4. Maximum possible storm sur
- Page 219 and 220: Figure 2.Frequency of severe cyclon
- Page 221 and 222: CIRCULATION AND PHYSICAL PROCESSES
- Page 223 and 224: In the Arabian Sea dissolved oxygen
- Page 225 and 226: Table 1.Distribution of the depth o
- Page 227 and 228: 61' 63' 65' 67'25'I I I I I61' 63O
- Page 229 and 230: A REVIEW OF THE PHYSICAL OCEANOGRAP
- Page 231 and 232: PHYSICAL OCEANOGRAPHIC PROPERTIESTh
- Page 233 and 234: This current is weaker and narrower
- Page 235 and 236: IIFigure 1.Geography and bathymetry
- Page 237 and 238: 4l 2-4 1 .1. 4- ---- --.2./*--I,0°
- Page 239 and 240: I R A NARABIA26"-24'-INNER GULF, KA
- Page 241 and 242: K:Diutide. ....... ....._ ..... ..
- Page 243 and 244: Figure 11. The probable circulation
- Page 245 and 246: FISHERY RESOURCES IN THE NORTH ARAB
- Page 247 and 248: BASIC OCEANOGRAPHIC FEATURES OF THE
- Page 249 and 250: Simultaneously, rather extensive fi
- Page 251 and 252: ~~Table 1 Physical chemical propert
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EXPLOITABLE LIVING RESOURCESThe fir
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Table 3. Seasonal variations in sta
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It is logical to expect that such h
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DHULKED, M.H. (1962). Observations
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KREY, J. and BABENARD (1976). Phyto
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SMITH, S.L. (1982). The northwester
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c0*rlUaUII)hU.rl?.rlUU3a0.4a0‘rlP
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GmEakU0U0Cn I4: aUkm .u u-aw nLU0,t
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282
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1984 -1985 AIMu kalla---- Nov-- Feb
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aIVI030cH \'YNlEO 08'000 0 0dOJ286
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na288
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-mE-*’=0 c>0zmNt0c0nWU0Iv)2It33aU
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d............... . ..LL '..,.. . I.
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W0-5:izU0v,PIIMI I I I0InIn(UO/o 3n
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WEATHER IMONSOONSJ I SOLAR RADIATIO
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RED SEA BIOLOGICAL OCEANOGRAPHY AND
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Benthic studies in the deep waters
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WEIKERT, H. (1982). The vertical di
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SiO4(,urnoi/I)0 5 10 15 20 25 30PO4
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THE CRUST BENEATH THE RED SEA - GUL
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generally weak or lacking, the only
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the Bouguer gravity reaches only 90
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Such an isotopic composition has le
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Since no major shear, spreading, or
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~5) continued thinning and rifting
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BURKE, R.A. JR., BROOKS, J.M. and S
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GIRDLER, R.S. and STYLES, P. (1982)
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QUENNELL, A.M. (1958). The structur
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Figure 1.Simplified morphology and
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QA.7 o 2.7*oPlia‘PlrihPlia 7c tMi
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v)CdQIE-30LIYiJr0,dQ,rnUQIaT dIIT I
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37.19'vv22'06'N01 37.36' EJ 2.522 '
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N-c-0-c.I333
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Figure 11.Isochrons in m.y. deduced
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337c&!C0
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SEDIMENTARY STRUCTURE OF THE NORTHE
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On the African side, Precambrian sh
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length the Red Sea is characterized
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SUGGESTIONS FOR FUTURE RESEARCH IN
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GUILCHER, A. (1979). Les rivages co
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Concentration96Aqaba*AI-Ghardaqa**3
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Figure 1. Geologic map of the north
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35 O 34O 33O 32' 3 l o30°SINAI?go!
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356
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1 In 35" 4003I4 50Oceanographer dee
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only a partial inflow of Indian Oce
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wind reef margins, are required. Th
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4.5.6.7.8.9.10.11.F12.13.14.What is
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SMITH, J.J.B. (1950). The sea fishe