(Plate 3) Manganese nodules and deep-sea sediment core from Pacific Ocean

• Main Author: Nayudu, Y Rammohanroy
• Format: Dataset
• Language: English
• Published: PANGAEA 1964
• Subjects: CHIN02BD; CHIN0ABD-002G; CHINOOK; CHNK-2G; Date/Time of event; DEPTH; sediment/rock; Description; DOWNWIND-H; Dredge; chain bag; DRG; DRG_C; DWHD72; Elevation of event; Event label; FANB01BD; FANBD-25D; FANFARE-B; GC; Gravity corer; Horizon; Latitude of event; Longitude of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Northern_Holiday; North-West Pacific Ocean; NTHL02HO-010PH; NTHL-10; Pacific Ocean; Sample code/label; Sample ID; Spencer F. Baird; Uniform resource locator/link to image; Wired profile sonde; WP; Iceland
• Online Access: https://doi.pangaea.de/10.1594/PANGAEA.856785; https://doi.org/10.1594/PANGAEA.856785

A synoptic review of the studies of well-known occurrences of palagonite tuffs is presented. Included are palagonite tuffs from Iceland, and pillow-lava palagonite complexes from Columbia River basalts and from the central Oregon coast. Additional petrologic and x-ray defraction data for selected samples are presented. Petrologic evidence shows that basaltic glass of aqueous tuffs and breccias consists of sideromelane, which is susceptible to palagonitization. It is shown that palagonitization is a selective alteration process, involving hydration, oxidation and zeolitization. Some of the manganese nodules dredged from the Pacific Ocean floor contain nucleus of palagonite-tuff breccias or of zeolite. A brief megascopic and microscopic description of nodules from the south Pacific, the Mendocino ridge and the 'Horizon' Nodule from the north Pacific is presented. Petrographic studies of palagonite-tuff breccias of manganese nodules and other palagonites suggest that migration and segregation of metallic elements occur during and subsequent to palagonitization. During the palagonitization of sideromelane, nearly 30 percent of sea water is absorbed. The hydration of sideromelane is also accompanied by oxidation of iron and other elements. These oxides may be released either in colloidal form or in true solution and tend to precipitate first from the unstable palagonite.