BAUMANN, A., RICHTER, H. and SCHOELL, M. (1973). Suakin Deep: brines and hydrothermalsediments in the deepest part of the Red Sea. Geol. Rundschau, 62,684-697.BECKER, K., VON HERZEN, R.P., FRANCIS, T.J.G., ANDERSON, R.N., HONNOREZ, J.,ADAMSON, A.C., ALT, J.C., EMMERMANN, R., KEMPTON, P.D., KINOSHITA, H.,LAVERNE, C., MOTTL, M.J. and NEWMARK, R.L. (1982). In situ electrical resistivityand bulk porosity of the oceanic crust, Costa Rica Rift. Nature, 300,594-598.BEN-AVRAHAM, Z., GARFUNKEL, Z., ALMAGOR, G. and HALL, J.K. (1979a). Continentalbreakup by a leaky transform: the Gulf of Elat (Aqaba). Science, 206,214-216.BEN-AVRAHAM, Z., ALMAGOR, G. and GARFUNKEL, 2. (1979b). Sediments and structure ofthe gulf of Elat (Aqaba) - Northern Red Sea. Sediment. Geol., 23,239-267.BERTIN, J., PEDEUX, J.P. and MAGENHAM, J.C. (1979). Contribution de la gkophysique et del'ocdanographie physique B la recherche et B l'exploration des hues mCtallif6r6es de la MerRouge. In: Proceedings of the International Seminar on Offshore Mineral Resources,Germinal and BRGM, Document BRGM No. 7, Orlbans, 339-366.BEYDOUN, Z.R. (1970). Southern Arabia and northern Somalia: comparative geology. Phil.Trans. R. Soc. Lond., A, 267,75-87.BIGNELL, R.D. and ALI, S.S. (1976). Geochemistry and stratigraphy of Nereus Deep, Red Sea.Geol. Jb., D, 17, 173-186.BISCHOFF, J.L. (1969). Red Sea geothermal brine deposits: their mineralogy, chemistry, andgenesis. In: E.T. Degens and D.A. Ross (eds.), ,,Hot Brines and Recent Heavy MetalDeposits", Springer Verlag, New York, 368-401.BREWER, P.G. and SPENCER, D.W. (1969). A note on the chemical composition of the Red Seabrines. In: E.T. Degens and D.A. Ross (eds.), ,,Hot Brines and Recent Heavy MetalDeposits in the Red Sea", Springer Verlag, New York, 174-179.BROOKS, R.R., KAPLAN, I.R. and PETERSON, M.N.A. (1969). Trace element composition ofRed Sea geothermal brine and interstitial water. In: E.T. Degens and D.A. Ross (eds.), ,,HotBrines and Recent Heavy Metal Deposits in the Red Sea", Springer Verlag, New York,180-203.BROWN, G.F. (1970). Eastern margin of the Red Sea and coastal structures in Saudi Arabia. Phil.Trans. R. Soc. Lond., A, 267, 75-87.BROWN, C. and GIRDLER, R.W. (1982). Structure of the Red Sea at 20"N from gravity data andits implication for continental margins. Nature, 298,51-53.BRYAN, W.B. and MOORE, J.G. (1977). Compositional variations of young basalts in theMid-Atlantic Ridge rift valley near lat. 36"49'N. Bull. Geol. Soc. Amer., 88(4), 556-570.BURKE, K. (1977). Aulacogens and continental breakup. Ann. Rev. Earth Planet. Sci., 5,37 1-396.BURKE, K. (1978). Evolution of continental rift systems in the light of plate tectonics. In: I.B.Ramberg and E.-R. Neumann (eds.), ,,Tectonics and Geophysics of Continental Rifts", E.Reidel Publ. Co., Dordrecht, 1-9.BURKE, K. and DEWEY, J.F. (1973). Plume-generated triple-junctions: key indicators in applyingplate tectonics to old rocks. J. Geol., 81,406-433.318
BURKE, R.A. JR., BROOKS, J.M. and SACKETT, W.M. (1981). Light hydrocarbons in Red Seabrines and sediments. Geochim. Cosmochim. Acta, 45,627-634.CARELLA, R. and SCARPA, N. (1962). Geological results of exploration in Sudan by AGIPMineraria Ltd. 4* Arab. Petr. Congr., Beirut.CLOOS, H. (1939). Hebung, Spaltung, Vulkanismus. Geol. Rundschau, 30,401-527.COCHRAN, J.R. (1981). The Gulf of Aden: Structure and evolution of a young Ocean basin andcontinental margin. J. Geophys. Res., 86,263-287..--COCHRAN, J.R. (1982a). Reply. J. Geophys. Res., 87, 6765-6770. --\COCHRAN, J.R. (1982b). The magnetic quiet zone in the eastern Gulf of Aden: Implications for theearly development of the continental margin. Geophys. J. Roy. Astr. Soc., 68, 171-201.DAVIES, D. and TRAMONTINI, C. (1970). The deep structure of the Red Sea. Phil. Trans. R.Soc. Lond., A, 267, 181-190.DEGENS, E.T. and ROSS, D.A. (1970). The Red Sea hot brines. Scientific American, 222 (40),32-42.DEGENS, E.T. and ROSS, D.A. (1976). Strata-bound metalliferous deposits found in or near activerifts. In: K.H. Wolf (ed.), ,,Handbook of Strata-bound and Stratiform Ore Deposits", Vol.4, Tectonics and Metamorphism, Elsevier, Amsterdam, 165-202.DEGENS, E.T., VON HERZEN, R.P. and WONG, H.K. (1971). Lake Tanganyika: waterchemistry, sediments, geological structure. Naturwissenschaften, 58,229-241.DEUSER, W.G. and DEGENS, E.T. (1969). 018/016 and C13/C12 ratios of fossils from thehot-brine deep area of the central Red Sea. In: E.T. Degens and D.A. Ross (eds.), ,,HotBrines and Recent Heavy Metal Deposits in the Red Sea", Springer Verlag, New York,33 6-347.DEUSER, W.G., ROSS, E.H. and WATERMAN, L.S. (1976). Glacial and pluvial periods: theirrelationship revealed by Pleistocene sediments of the Red Sea and Gulf of Aden. Science,191, 1168.DRAKE, C.L. and GIRDLER, R.W. (1964). A geophysical study of the Red Sea. Geophys. J.Roy. Astr. Soc. Lond., 8, 473-495.EDMOND, J.M., VON DAMM, K.L., McDUFF, R.E. and MEASURES, C.I. (1982). Chemistry ofhot springs on the East Pacific Rise and their effluent dispersal. Nature, 297,187-191.ELTAYEB, M., IZZELDIN, Y., HORN, R. and TIXERONT, M. (1979). Les donnCesgkophysiques de la Mer Rouge centrale: entre 18 et 24'N: leur traitement par la techniqueSigma. In: Proceedings of the International Seminar of Offshore Mineral Resources,Germinal and BRGM, Document BRGM No. 7, Orleans, 367-379.EMERY, K.O., HUNT, J.M. and HAYS, E.E. (1969). Summary of hot brines and heavy metaldeposits in the Red Sea. In: E.T. Degens and D.A. Ross (eds.), ,,Hot Brines and RecentHeavy Metal Deposits in the Red Sea", Springer Verlag, New York, 557-57 1.ERICKSON, A.J. and SIMMONS, G. (1969). Thermal measurements in the Red Sea hot brinepools. In: E.T. Degens and D.A. Ross (eds.), ,,Hot Brines and RecentHeavy Metal Deposits in the Red Sea", Springer Verlag, New York, 114-121.319
- Page 1 and 2:
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
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REFERENCESAGASSIZ, A. (1903). The c
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PILLAI, C.S.G. (1969b). Studies on
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Table 1.Extent of damage to coral r
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STATUS OF CRITICAL MARINE HABITATS
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OCCURRENCEThe distribution of reefs
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Mining of Reef RockMining of reef r
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-resource. Their significance deriv
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Coating of Aerial Roots by Fine Sed
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associated with the roots (e.g. GOE
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Temperature and SalinityThe effects
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significant numbers in the Red Sea,
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mersas are known to serve as nurser
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BURCHARD, J.E. (1979). Coral fauna
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HIRTH, H.F., KLIKOFF, L.G. and HARP
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MacNAE, W. (1974). Mangrove forests
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RINKEVITCH, B. and LOYA, Y. (1977).
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WALKER, D.I. and ORMOND, R.F.G. (19
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DAMMING AND DIVERSION OF RIVERSIn d
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FUTURE STUDIESWhat can marine scien
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!0OD9 -8 Nc80,a,u-3(dcab(Dbrr)8brr)
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0 0-0 00 O0O 0% LD d- m cu 0 0202
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STORM SURGES IN THE BAY OF BENGAL*T
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low pressure centres over the Bay i
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ACKNOWLEDGEMENTSThe writers wish to
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Table 1.Latitude and longitude of p
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214
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0Poa9nU0m0Yan-I2li7mYUVQk?401mc0mYm
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0In218
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221
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Table 3. Nomenclature used by India
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ANDHRAB A Y OFB E N G A L ,.16'LO 4
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INDIABAY OF-Point CalirnereLanka L-
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pressure in the South Pacific and l
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SWALLOW, J.C. (1983). Arabian Sea c
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234
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236
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scale wind phenomenon that occurs w
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Several two-dimensional models of t
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HARTMANN, M., LANGE, H., SEIBOLD, E
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Y-Model Domaint=6hrs.b-250 0 59 Xw-
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UELEVATIONS (m) ai 18 HOURS L2:-+EL
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HARMONIC CONSTITUENT K,Figure 8. Ob
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Age of Semi-Diurnal Tide (hrs)28".+
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! 5"BOTTOMFigure 13. Predicted mode
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OCEANOGRAPHIC CONDITIONS PELAGIC PR
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Low oxygen content in subsurface wa
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R/V Dr. F. Nansen trawl of 41 m hea
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thermocline temperature decreases s
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Nitrate - NitrogenSimilarly to phos
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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 310 and 311: EYAL, M., EYAL, Y., BARTOV, Y. and
- 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
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- 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
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- 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