Saved in:
| Main Authors: | , , , , |
|---|---|
| Format: | Dataset Open Access |
| Language: | en |
| Published: |
PANGAEA
2023
|
| Subjects: | |
| Online Access: | https://doi.org/10.1594/PANGAEA.961645 |
| Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
| _version_ | 1867170120763179008 |
|---|---|
| author | Hein, James R Fleishman, C L Morgenson, Lisa A Bloomer, Sherman H Stern, Robert J |
| author_facet | Hein, James R Fleishman, C L Morgenson, Lisa A Bloomer, Sherman H Stern, Robert J |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | During R/V T. Thompson cruise TT-192 around the the Mariana and Volcano Volcanic Arcs 60% of the dredge recoveries contained ferromanganese deposits. Substrate rocks consisted of intermediate to mafic volcanic rocks, volcaniclastic rocks, volcanic breccia, and minor limestone. Volcaniclastic rocks were dominantly sandstone but ranged from mudstone to conglomerate. Ferromanganese deposits occur in five ways: Yellow-brown to black ferromanganese encrustations on rocks; brown, grey, and black ferromanganese oxides cementing volcaniclastic sandstone; stratiform, stratabound Mn oxide rich layers that are pale to dark grey, rarely brownish-grey, with a submetallic luster; cobbles of dark grey submetallic, irregularly shaped masses of manganese (Mn nodules ?) and weatehered black cobbles rich in magnetite. A selection of these deposits was chemically analysed including major and minor elements, rare earth elements, and platinum-group elements. The chemistry determination was done by Induction Coupled Plasma analyses done by J. G. Crock, and K. Kennedy at the U.S. Geological Survey laboratories in Reston, Denver and Menlo Park respectively. Water and CO2 determinations were done by wet chemical techniques. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_961645 |
| institution | PANGAEA |
| language | en |
| publishDate | 2023 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Chemical composition of ferromanganese deposits from the Mariana and Volcano volcanic arcs Hein, James R Fleishman, C L Morgenson, Lisa A Bloomer, Sherman H Stern, Robert J Aluminium; Arsenic; Barium; Cadmium; Calcium; Carbon dioxide; Cerium; Chromium; Cobalt; Copper; Deposit type; DEPTH, sediment/rock; DISTANCE; Dredge; DRG; Dysprosium; Elevation of event; Erbium; Europium; Event label; Gadolinium; Geochemistry; HalbachD36; Holmium; Identification; Induction-coupled plasma technique; Iron; Lanthanum; Latitude of event; Lead; Lithology/composition/facies; Longitude of event; Lutetium; Magnesium; Manganese; manganese micronodule; manganese nodule; Marianas; Molybdenum; Neodymium; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; ocean; Pacific Ocean; Palladium; Phosphorus; Platinum; Potassium; Praseodymium; Rhodium; Samarium; Sample code/label; Sediment; Silicon; Sodium; Strontium; Terbium; Thomas G. Thompson (1964); Thulium; Titanium; TT192; TT192-D11; TT192-D12; TT192-D13; TT192-D15; TT192-D20; TT192-D21; TT192-D27B; TT192-D28; TT192-D3; TT192-D33; TT192-D36; TT192-D37; TT192-D41; TT192-D42; TT192-D44; TT192-D51; TT192-D52; TT192-D54; TT192-D55; TT192-D56; TT192-D57; TT192-D58; TT192-D59; TT192-D71; TT192-D73; TT192-D8; Vanadium; Water in rock; Wet chemistry; Ytterbium; Yttrium; Zinc During R/V T. Thompson cruise TT-192 around the the Mariana and Volcano Volcanic Arcs 60% of the dredge recoveries contained ferromanganese deposits. Substrate rocks consisted of intermediate to mafic volcanic rocks, volcaniclastic rocks, volcanic breccia, and minor limestone. Volcaniclastic rocks were dominantly sandstone but ranged from mudstone to conglomerate. Ferromanganese deposits occur in five ways: Yellow-brown to black ferromanganese encrustations on rocks; brown, grey, and black ferromanganese oxides cementing volcaniclastic sandstone; stratiform, stratabound Mn oxide rich layers that are pale to dark grey, rarely brownish-grey, with a submetallic luster; cobbles of dark grey submetallic, irregularly shaped masses of manganese (Mn nodules ?) and weatehered black cobbles rich in magnetite. A selection of these deposits was chemically analysed including major and minor elements, rare earth elements, and platinum-group elements. The chemistry determination was done by Induction Coupled Plasma analyses done by J. G. Crock, and K. Kennedy at the U.S. Geological Survey laboratories in Reston, Denver and Menlo Park respectively. Water and CO2 determinations were done by wet chemical techniques. |
| title | Chemical composition of ferromanganese deposits from the Mariana and Volcano volcanic arcs |
| topic | Aluminium; Arsenic; Barium; Cadmium; Calcium; Carbon dioxide; Cerium; Chromium; Cobalt; Copper; Deposit type; DEPTH, sediment/rock; DISTANCE; Dredge; DRG; Dysprosium; Elevation of event; Erbium; Europium; Event label; Gadolinium; Geochemistry; HalbachD36; Holmium; Identification; Induction-coupled plasma technique; Iron; Lanthanum; Latitude of event; Lead; Lithology/composition/facies; Longitude of event; Lutetium; Magnesium; Manganese; manganese micronodule; manganese nodule; Marianas; Molybdenum; Neodymium; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; ocean; Pacific Ocean; Palladium; Phosphorus; Platinum; Potassium; Praseodymium; Rhodium; Samarium; Sample code/label; Sediment; Silicon; Sodium; Strontium; Terbium; Thomas G. Thompson (1964); Thulium; Titanium; TT192; TT192-D11; TT192-D12; TT192-D13; TT192-D15; TT192-D20; TT192-D21; TT192-D27B; TT192-D28; TT192-D3; TT192-D33; TT192-D36; TT192-D37; TT192-D41; TT192-D42; TT192-D44; TT192-D51; TT192-D52; TT192-D54; TT192-D55; TT192-D56; TT192-D57; TT192-D58; TT192-D59; TT192-D71; TT192-D73; TT192-D8; Vanadium; Water in rock; Wet chemistry; Ytterbium; Yttrium; Zinc |
| url | https://doi.org/10.1594/PANGAEA.961645 |