957 resultados para underwater acoustics
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Mineralogy and geochemistry of low-temperature hydrothermal manifestations occurring on the surface of basalts and in their cracks within a submarine volcano in the north-eastern part of the Kuril deep-sea basin have been studied. The following order of isolation of mineral phases has been found out: Fe-rich sulphides (pyrite) - Fe-rich layered silicates (hydromica of celadonite-nontronite type) - amorphous silica (opal) - Fe-oxyhydroxides (goethite) - Mn-oxyhydroxides (vernadite). Sulphide mineralization is of the phenocryst-stockwork type. Finding of pure barite fragments does not exclude presence of hydrothermal exhalations (smokers) on this volcanic structure.
(Table II.1.11) Lithology of bottom sediments from the underwater Slupsk River foredelta, Baltic Sea
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Geological and geophysical investigations carried out within the Hokkaido Rise showed that intrusives composing outcrops of the crystalline basement on the ocean floor form a continuous series from monzonites and diorite-monzonites to granites with prevalence of granodiorites with stable mineralogical association: biotite - hornblende - K-feldspar. Acidic volcanic rocks are characterized by a similar mineralogical association with almost complete absence of plagioclase-pyroxene species. It seems that the Hokkaido Rise, as well as the marginal oceanic Zenkevich swell as a whole are not primary oceanic structural formations and have undergone a complex and long history of geological development with intense orogenic movements that occurred in Middle Cretaceous and preceded subalkaline basalt outpouring during postorogenic subsidence of the Earth crust.
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"Contract No. DA-22-079-civeng-63-104."
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"Report no. CD-D-15-81."
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Shipping list no.: 97-0340-P.
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Final report; April 1978.
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Final report; April 1978.
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"Report no. CG-D-65-78"--V. 2.
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Mode of access: Internet.
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Mode of access: Internet.
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Architectural acoustics : the effect of a speaker's voice in different directions / by Hugh Tallant, 1913 ([4] leaves : ill. ; 37 cm.) bound at end.