139736eo.pdf (20MB) - Japan Oceanographic Data Center
139736eo.pdf (20MB) - Japan Oceanographic Data Center 139736eo.pdf (20MB) - Japan Oceanographic Data Center
kmaFigure 6. Summary of seismic refraction profilesin the Red Sea. Velocities are in kms-l. Shaded area marks region of detailedseismic refraction survey. Earthquakeepicenters are shown by blackdots, and 1000 m isobath as a continuousline. Crustal thickness in km is givenas large, underlined numbers.330
37.19'vv22'06'N01 37.36' EJ 2.522 '03' N38'38'EE0 ~2.522'44' NE-22*00'N38'27'Er22'44'N0, 37.19.EO2I '!r50O- km2.520'46'N37'42'E20.53.N38'58'Ea0-1 -2-3-bFigure 7.a) Seismic reflection profiles over the central RedSea transverse to the axial trough. Reflector S isindicated by a heavy line. After SEARLE and ROSS(1975). Vertical scale is in seconds of two-way traveltime. b) Seismic reflection profile with a 2:lverticalexaggeration showing a piercement dome of Miocene saltpossibly triggered by normal faulting from below. Tsrepresents Miocene salt, and Td the Mio-Pliocene seriesof clastics and coral reefs, bounded by an unconformityat the base. After LOWEL 5 2. (1975).331
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- 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 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 322 and 323: kQ)Um 5U0c04 3N 4COQ)k3M*rlk332
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- 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
37.19'vv22'06'N01 37.36' EJ 2.522 '03' N38'38'EE0 ~2.522'44' NE-22*00'N38'27'Er22'44'N0, 37.19.EO2I '!r50O- km2.520'46'N37'42'E20.53.N38'58'Ea0-1 -2-3-bFigure 7.a) Seismic reflection profiles over the central RedSea transverse to the axial trough. Reflector S isindicated by a heavy line. After SEARLE and ROSS(1975). Vertical scale is in seconds of two-way traveltime. b) Seismic reflection profile with a 2:lverticalexaggeration showing a piercement dome of Miocene saltpossibly triggered by normal faulting from below. Tsrepresents Miocene salt, and Td the Mio-Pliocene seriesof clastics and coral reefs, bounded by an unconformityat the base. After LOWEL 5 2. (1975).331
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