Titlebook: Hot Brines and Recent Heavy Metal Deposits in the Red Sea; A Geochemical and Ge Egon T. Degens,David A. Ross Book 1969 Springer Science+Bus

fibula

Geological Structures of the Red Sea Area Inferred from Satellite Picturesabian-Nubian shield, the sediment-filled Red Sea “graben” system and the marginal sedimentary cover with large areas of volcanic activity..Among five major systems of faults affecting the Arabian-Nubian massif, three systems trending N, NW, and WNW appear to have a profound influence on the structur

sacrum

The Red Sea — A Geophysical Backgrounda pertaining to the latter are summarized. The Red Sea developed in phases, and it is likely that these correspond in time to phases of continental drift. The geophysical data for the Red Sea are summarized in a general résumé and in more detail by considering the Red Sea in three parts, viz. the no

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Structural Effects of Sea-floor Spreading in the Gulf of Aden and the Red Sea on the Arabian Shieldmplexities in the southern Red Sea and Afar Depression (Mohr, 1967), it seems reasonable to infer that the Aden extension of the Indian mid-oceanic ridge splits in this area into two branches: the Red Sea branch to the NNW (Girdler, 1965) and the East African Rift System to the SSW (Mohr, 1968)..Lin

neolith

muster

Magnetic and Gravity Anomalies in the Central Red Seanfirm previous hypotheses that dense, strongly magnetic rocks underlie these areas. The gravity and magnetic anomalies in the immediate vicinity of the hot brine area appear to be part of broad, regional anomaly trends subparallel to the axial trough. It is unlikely that the heavy metal deposits of

laxative

错事

Basalt from the Axial Trough of the Red Seaific gravity between 2.5 and 2.7 and refractive index of 1.607 ±.003. One sample contained laths of plagioclase (An 60–82). The rocks contain no normative nepheline and are poor in K.O (0.2 wt per cent). In these respects they resemble subalkaline oceanic basalts and the basalts of the island of Jeb

Brain-Imaging

Hydrography of the Red Sea Brinesnted. Most papers on this subject have reported “salinity” values derived from volumetric dilution of the sample with distilled water and conductometric measurement of the dilute sample. The errors in this procedure are described, and the true salinity of a number of samples has been measured. Layer

ANA

Temperature Structure of the Red Sea Brines a 44°C water, which starts at a depth of 2,009m and has a thickness of 28m, overlies the bottom 56°C water. The interface between these layers is sharp and only about 5m thick..In the Discovery Deep a 4m thick 36°C water overlies a bottom 44°C water. The interface between these layers is not as sha

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