995 resultados para 163-990A


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pt. 1. January 19, 20, 23, February 21-23, 29, March 1, 6-10, 1956. 1225 p.--pt. 2. June 4-6, 12, 21, 1956. pp. 1227-1533.

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Mode of access: Internet.

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Hearings held Jan. 26, 1956 - Feb. 5, 1960, pursuant to Senate resolution 18, 84th Cong. [and others] volume 8 has also special subtitle : The finale phase of the Committee's inquiry with reference to overall television allocations.

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Considerable postsedimentational alteration of fine dispersed minerals in Cretaceous sedimentary sequences was found in three deep-sea drillholes (163, 164, 169). Original Fe-montmorillonites formed from basalts were converted during lithification to mixed-layer montmorillonite-hydromicas and then to pure hydromicas (celadonites). An assumption that the minerals were originally of authigenic-diagenetic composition is based on a broad spectrum of other diagenetic minerals present: silica group from opal A to opal CT and quartz, clinoptilolite and palygorskite. In addition, quartz-hydromica ratio is strikingly atypical of aeolian transport.