EYAL, M., EYAL, Y., BARTOV, Y. and STEINITZ, G. (1981). The tectonic development of thewestern margin of the Gulf of Elat (Aqaba) Rift. Tectonophysics, 80,39-66.FAIRHEAD, J.D. (1973). Crustal structure of the Gulf of Aden and the Red Sea. Tectonophysics,20, 261-267.FAIRHEAD, J.D. and GIRDLER, R.W. (1970). The seismicity of the Red Sea, Gulf of Aden andAfar mangle. Phil. Trans. Roy. Soc. Lond., A, 267,49-74.FAIRHEAD, J.D. and GIRDLER, R.W. (1971). The seismicity of Africa, Geophys. J. Roy. Astr.Soc. Lond., 24, 271-301.FISHER, R.L., BUNCE, E.T., CERNOCK, P.J., GLEGG, D.C., CRONAN, D.S., DAMIANI,V.A., DMITRIEV, L., KINSMAN, D.J.J., ROTH, P.H., THIEDE, J. and VINCENT, E.(1974). Initial Reports of the Deep Sea Drilling Project, 24. U.S. Govt. Printing Office,Washington.FLEISCHER, U. (1969). Investigations of rifts by shipboard magnetic and gravity surveys: Gulf ofAqaba-Red Sea and Reykjanes Ridge. Deutsch. Hydrogr. Z., 22(5), 205-208.FREUND, R. (1970). Plste tectonics of the Red Sea and East Africa. Nature, 228,453.FREUND, R., GARFUNKEL, Z., ZAK, I., GOLDBERG, M., WEISSBROD, T. and DERIN, B.(1970). The shear along the Dead Sea Rift. Phil. Trans. Roy. Soc. Lond., A, 267, 107-130.GASS, I.G. (1970). The evolution of volcanism in the junction area of the Red Sea, Gulf of Adenand Ethiopian rifts. Phil. Trans. Roy. Soc. Lond., A, 267,369-381.GASS, I.G. (1977). The age and extent of the Red Sea oceanic crust. Nature, 265,722-724.GINSBERG, A, MAKRIS, J., FUCHS, K. and PRODEHL, C. (1981). The structure of the crustand upper mantle in the Dead Sea Rift. Tectonophysics, 80,109-19.GIRDLER, R.S. (1969). The Red Sea - a geophysical background. In: E.T. Degens and D.A.Ross (eds.). ,,Hot Brines and Recent Heavy Metal Deposits in the Red Sea", Springer Verlag,New York, 38-58.GIRDLER, R.S. (1978).Comparison of the East African rift system and the Permian Oslo Rift. In:I.B. Ramberg and E.R. Neumann (eds.), ,,Tectonics and Geophysics of Continental Rifts",D. Reidel Publ. Co., Dordrecht, 329-345.GIRDLER, R.S.and DARRACOTT, B.W. (1972). African poles of rotation. Comments Earth Sci.,Geophys., 2, 131-138.GIRDLER, R.S. and EVANS, T.R. (1977). Red Sea heat flow. Geophys. J. Roy. Astr. Soc.Lond., 51, 245-251.GIRDLER, R.S.and STYLES, P. (1974). Two stage Red Sea floor spreading. Nature, 247,7-11.GIRDLER, R.S.and STYLES, P.(1976). Opening of the Red Sea with two poles of rotation - somecomments. Earth Planet. Sci. Lett., 33, 169-172.GIRDLER, R.S.and STYLES, P. (1978). Seafloor spreading in the western Gulf of Aden. Nature,271, 615-617.320
GIRDLER, R.S. and STYLES, P. (1982). Comments on the Gulf of Aden: ,Structure and evolutionof a young ocean basin and continental margin' by J.R. Cochran. J. Geophys. Res., 87,6761 -6763.GIRDLER, R.S. and WHITMARSH, R.B. (1974). Miocene evaporites in Red Sea cores, theirrelevance to the problem of the width and age of oceanic crust beneath the Red Sea. In: R.B.Whitmarsh, P.E. Weser, D.A. Ross et al. (eds.), "Initial Reports of the Deep Sea DrillingProject", U.S. Govt. Printing Office, Washington, 23, 913-921.GIRDLER, R.S., ERICKSON, A.J. and VON HERZEN, R.P. (1974). Downhole temperature andshipboard thermal conductivity measurements aboard R/V Glomar Challenger in the Red Sea(Leg 23). In: Initial Reports of the Deep Sea Drilling Project, U.S. Govt. Printing Office,Washington, 23, 879-886.GIRDLER, R.S., BROWN, C., NOY, D.J.M. and STYLES, P. (1980). A geophysical survey ofthe westernmost Gulf of Aden. Phil. Trans. Roy. Soc. Lond., Ser. A, 298, 1-43.HAENEL, R. (1972). Heat flow measurements in the red Sea and the Gulf of Aden. 2. Geophys.,38, 1035-1047.HENDRICKS, R.L., REISBICK, F.B., MAHAFFEY, E.J., ROBERTS, D.B. and PETERSON,M.N.A. (1969). Chemical composition of sediments and interstitial brines from the Atlantis11, Discovery and Chain Deeps. In: E.T. Degens and D.A. Ross (eds.), ,,Hot Brines andRecent Heavy Metal Deposits in the Red Sea", Springer Verlag, New York, 407-440.HUNT, J.M., HAYS, E.E., DEGENS, E.T. and ROSS, D.A. (1967). Red Sea: detailed survey ofhot brine areas. Science, 156,514-516.HUTCHINSON, R.W. and ENGELS, G.G. (1972). Tectonic evolution in the southern Red Sea andits possible significance to older rifted continental margins. Geol. Soc. Amer. Bull., 83,2989-3002.ILLIES, J.H. and FUCHS, K. (Eds.), (1974). Approaches to Taphrogenesis. Schweizerbart,Stuttgart, 460 pp.ILLIES, J.H. and MUELLER, S (Eds.), (1970). Graben Problems. Schweizerbart, Stuttgart, 316PP.KLEMME, H.D. (1975). Geothermal gradients, heat flow, and hydrocarbon recovery. In: A.G.Fischer and S. Judson (eds.), ,,Petroleum and Global Tectonics", Princeton Univ. Press,New Jersey, 25 1-304.LAUGHTON, A.S. (1970). A new bathymetric chart of the Red Sea. Phil. Trans. Roy. Soc. Lond.,A, 267, 21-22.LAUGHTON, A.S. and TRAMONTINI, C. (1970). Recent studies of the crustal structure of theGulf of Aden. Tectonophysics, 8, 359-375.LAUGHTON, A.S., WHITMARSH, R.B. and JONES, M.T. (1970). The evolution of the Gulf ofAden. Phil. Trans. Roy. Soc. Lond., A, 267,227-266.LE PICHON, X. and FRANCHETEAU, J. (1978). Plate tectonic analysis of the Red Sea - Gulf ofAden area. Tectonophysics, 46,369-406.LE .PICHON, X., FRANCHETEAU, J. and BONNIN, J. (1973). Plate Tectonics. Elsevier,Amsterdam, 300 pp.321
- Page 1 and 2:
Intergovernmental Oceanographic Com
- Page 3 and 4:
of the IOC Marine Pollution Monitor
- Page 5:
PageMARGINAL SEASSTORM SURGES IN TH
- Page 9 and 10:
Marine PollutionAt present, marine
- Page 11 and 12:
THE INDIAN OCEAN --- AN ENVIRONMENT
- Page 13 and 14:
The subtropical anticyclonic gyre i
- Page 15 and 16:
GEOLOGICALBecause of its asymmetric
- Page 17 and 18:
RADIOACTIVE AND THERMAL WASTESIn co
- Page 19 and 20:
RESEARCH AND MONITORING ACTIVITIESM
- Page 21 and 22:
2-5, Mn 3-7, Zn 8-31, Fe 35-94, Pb
- Page 23 and 24:
Localized problems, both short-term
- Page 25 and 26:
HOLEMAN, J.N. (1968). The sediment
- Page 28 and 29:
UNEP/UNIDO (1982a). Industrial sour
- Page 30 and 31:
0-5-24 -I I I I I I I I I 11--25- A
- Page 32 and 33:
I*in '0( U N '0- '0 '0 N , p d'0I I
- Page 34:
C'EO IIFigure 6. Observations of oi
- Page 38 and 39:
Table 2.Ranges of Dissolved heavy m
- Page 40 and 41:
d.2 W2n2 n z0U.IzIO N m mENmIYEE*Ed
- Page 42 and 43:
Table 6. Population and related dat
- Page 44 and 45:
PROBLEMS IN THE PHYSICAL OCEANOGRAP
- Page 46:
B2: How does the Agulhas Current in
- Page 50 and 51:
0Q0mbWbvx(U49
- Page 52 and 53:
Figure 6 Average wind stress curl f
- Page 54 and 55:
THE DESTRUCTION OF THE TETHYS AND P
- Page 56 and 57:
part of the Seychelles-Mascarene bl
- Page 58 and 59:
Much of the old Tethys seafloor has
- Page 60 and 61:
when there was little or no movemen
- Page 62 and 63:
scouring of the sediments by cold b
- Page 64 and 65:
CANDE, S.C. and MUTTER, J.C. (1982)
- Page 66:
SHACKLETON, N.J. and KENNETT, J.P.
- Page 71 and 72:
0EYNz 10c2XaYWeKB20LuUz a5 cl300 10
- Page 75:
CALCAREOUS FORAMINIFERANANNOFOSSIL
- Page 79 and 80:
GEOLOGICAL-GEOPHYSICAL MAPPING OF T
- Page 81 and 82:
The latest tectonic generalization
- Page 83 and 84:
LE PICHON, X. and HEIRTZLER, J.R. (
- Page 85 and 86:
AN EXAMINATION OF THE FACTORS THAT
- Page 87 and 88:
is the specific volume anomaly. Po
- Page 89 and 90:
circulation. At Nagappattinam, Madr
- Page 91 and 92:
Table 1.MarmagaoCochin1969-781958-7
- Page 93 and 94:
tFigure 2. An idealized coastal cur
- Page 95 and 96:
STATION : BOMBAY~ J , F I M .- , A
- Page 97 and 98:
STATION : COCHIN, J , F , M , A , M
- Page 99 and 100:
3007STATION : MADRASI J I F , M I A
- Page 101 and 102:
STATION : CALCUTTA, J l F , M , A ,
- Page 103 and 104:
RED TIDE§ IN THE INDO-WEST PACIFIC
- Page 105 and 106:
were observed as early as 1770 duri
- Page 107 and 108:
diarrhetic shellfish poisoning (DSP
- Page 109 and 110:
GACUTAN, R.Q., TABBU, M.Y., AUJERO,
- Page 111 and 112:
Table 1.Clinical symptoms of variou
- Page 113 and 114:
Table 3. Fish species implicated in
- Page 115 and 116:
FIGURE CAPTIONSFigure la. Trichodes
- Page 118 and 119:
(*14aEE15aHH15c120
- Page 120 and 121:
MINERAL RESOURCES OF THE INDIAN OCE
- Page 122 and 123:
tonnes of monazite. Similar deposit
- Page 124 and 125:
Madagascar and the Red Sea. Within
- Page 126 and 127:
South Australian Basin: (Figs. 10-1
- Page 128 and 129:
Offshore placers are likely to occu
- Page 130 and 131:
MILLIMAN, J.D. (1974). Marine Carbo
- Page 132 and 133:
Thailand Tin 5560 (1980) NA 4.2 (19
- Page 134 and 135:
Table 2. The range (in percent) of
- Page 136 and 137:
Table 4. Chemical composition of po
- Page 138 and 139:
141FIGURE - 1
- Page 140 and 141:
~IT 73qw p' le' IS IFigure 4. Map s
- Page 142 and 143:
@A5 3 9 93 3 s 3 m4P 8O C ' . .' ,
- Page 144 and 145:
Figure 10. Map showng the abundance
- Page 146 and 147:
Figure 14. Map showing the distribu
- Page 148 and 149:
IFigure 17. Marine mineral explorat
- Page 150 and 151:
central are corals to the integrity
- Page 152 and 153:
Very little information is availabl
- Page 154 and 155:
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)
- Page 196 and 197:
0 0-0 00 O0O 0% LD d- m cu 0 0202
- Page 198 and 199:
STORM SURGES IN THE BAY OF BENGAL*T
- Page 200 and 201:
low pressure centres over the Bay i
- Page 202 and 203:
ACKNOWLEDGEMENTSThe writers wish to
- Page 204 and 205:
Table 1.Latitude and longitude of p
- Page 207 and 208:
214
- Page 209 and 210:
0Poa9nU0m0Yan-I2li7mYUVQk?401mc0mYm
- Page 211 and 212:
0In218
- Page 214 and 215:
221
- Page 216 and 217:
Table 3. Nomenclature used by India
- Page 218 and 219:
ANDHRAB A Y OFB E N G A L ,.16'LO 4
- Page 220 and 221:
INDIABAY OF-Point CalirnereLanka L-
- Page 222 and 223:
pressure in the South Pacific and l
- Page 224 and 225:
SWALLOW, J.C. (1983). Arabian Sea c
- Page 226 and 227:
234
- Page 228 and 229:
236
- Page 230 and 231:
scale wind phenomenon that occurs w
- Page 232 and 233:
Several two-dimensional models of t
- Page 234 and 235:
HARTMANN, M., LANGE, H., SEIBOLD, E
- Page 236 and 237:
Y-Model Domaint=6hrs.b-250 0 59 Xw-
- Page 238 and 239:
UELEVATIONS (m) ai 18 HOURS L2:-+EL
- Page 240 and 241:
HARMONIC CONSTITUENT K,Figure 8. Ob
- Page 242 and 243:
Age of Semi-Diurnal Tide (hrs)28".+
- Page 244 and 245:
! 5"BOTTOMFigure 13. Predicted mode
- Page 246 and 247:
OCEANOGRAPHIC CONDITIONS PELAGIC PR
- Page 248 and 249:
Low oxygen content in subsurface wa
- Page 250 and 251:
R/V Dr. F. Nansen trawl of 41 m hea
- Page 252 and 253:
thermocline temperature decreases s
- Page 254 and 255:
Nitrate - NitrogenSimilarly to phos
- Page 256 and 257:
The maximum standing stocks in the
- Page 258 and 259:
By April/May the demersal stocks ha
- Page 260 and 261: in 6 months when spawning occurs. T
- Page 262 and 263: REFERENCES3BANSE, K. (1968). Hydrog
- Page 264 and 265: GILSON, H.C., (1937). The nitrogen
- Page 266 and 267: ROYAL SOCIETY (1963). International
- Page 268 and 269: APPENDIX:REGIONAL COOPERATIVE INVES
- Page 270 and 271: 20 015 20 25FEBOC015 20 25 30 35M A
- Page 272 and 273: W0-8w0-Inww[r3a+eW281
- Page 274 and 275: B35 36 a7 XlO+ 35 36 a7- Mar--- Fob
- Page 276 and 277: a, A
- Page 278 and 279: ...... :'I. .. ,... .. 8.*.. ... ._
- Page 280 and 281: ASTAT.Si -Si (OH14 in p M - d ~ n -
- Page 282 and 283: YU0IwYY->02(33-1 II 1amLyY>02(33amL
- Page 284 and 285: I I I I I10 Ic L0U0mI(dw -rlo u0w m
- Page 286 and 287: III I I I0. 1....w'3...-0U-J..,....
- Page 288 and 289: 297
- Page 290 and 291: clearly is too low. Because of low
- Page 292 and 293: KARBE, L., THIEL, H., WEIKERT, H. a
- Page 294 and 295: 50010001 scoOxygen (rnl/l)0I1I2I3I4
- Page 296 and 297: c1 oc50C10001500_j_///.///II:I? 0:3
- Page 298 and 299: THE RED SEAPHYSIOGRAPHYThe Red Sea
- Page 300 and 301: intensity of magnetization which co
- Page 302 and 303: 1969; SEARLE and ROSS, 1975). This
- Page 304 and 305: y normal faulting. This is most int
- Page 306 and 307: South of 19"N, the McKENZIE pole no
- Page 308 and 309: BAUMANN, A., RICHTER, H. and SCHOEL
- Page 312 and 313: LEWIS, B.T.R. (1983). The process o
- Page 314 and 315: TARLING, D.H. and MITCHELL, J.G. (1
- Page 316 and 317: mC- 1000- 2000- 3000E0Figure 2.Sche
- Page 318 and 319: -20b-0,20wFigure 4. Seismicity and
- Page 320 and 321: kmaFigure 6. Summary of seismic ref
- Page 322 and 323: kQ)Um 5U0c04 3N 4COQ)k3M*rlk332
- Page 324 and 325: 5 b'o w-Y EO'i Ii04!I 0I0I334
- Page 326 and 327: II,'{34/,'0SOMALIAND: N. DANAKILFig
- Page 328 and 329: spreadingvulcanismmblock faultingII
- Page 330 and 331: SUPERFICIAL SEDIMENTS OF NORTHERN R
- Page 332 and 333: normally sorted, with median diamet
- Page 334 and 335: EL-SAYED (1983) used the trace meta
- Page 336 and 337: BEHAIRY, AKA. (1983). Marine transg
- Page 338 and 339: SHUKRI, N.M. (1953). Bottom deposit
- Page 340 and 341: Table 2 Heavy metal concentrations
- Page 342 and 343: EGYPTEl-Morgan 1Bargan IBargan 2Yub
- Page 344 and 345: Figure 4. Distribution of minerals
- Page 346 and 347: ARAGONITEHIGH HG-CALCITEFigure 6. T
- Page 348 and 349: MARINE LIVING RESOURCES OF THE RED
- Page 350 and 351: This elevated productivity may resu
- Page 352 and 353: REVELLE (1981) mentioned that the p
- Page 354 and 355: FISHELSON, L. (1964). Observation o