Structural stability of marine 10 Å manganates from the Ogasawara (Bonin) Arc: Implication for low-temperature hydrothermal activity
- 1 February 1989
- journal article
- Published by Elsevier in Marine Geology
- Vol. 86 (1) , 41-56
- https://doi.org/10.1016/0025-3227(89)90017-0
Abstract
No abstract availableThis publication has 27 references indexed in Scilit:
- Transformation of Birnessite to Buserite, Todorokite, and Manganite under Mild Hydrothermal TreatmentClays and Clay Minerals, 1987
- Cation exchange in synthetic manganates: I. Alkylammonium exchange in a synthetic phyllomanganateClay Minerals, 1986
- Ore paragenesis of recent hydrothermal deposits at the Cocos-Nazca plate boundary (Galápagos Rift) at 85‡ 51' and 85‡ 55' W: Complex massive sulfide mineralizations, non-sulfidic mineralizations and mineralized basaltsInternational Journal of Earth Sciences, 1986
- A high-temperature hydrothermal deposit on the East Pacific Rise near 7°NEarth and Planetary Science Letters, 1984
- Ferruginous vernadite in an Indian Ocean ferromanganese noduleGeological Magazine, 1984
- Comparison of the characteristics of manganese micronodules from the equatorial and South-West PacificTschermaks Mineralogische und Petrographische Mitteilungen, 1984
- A submarine hydrothermal manganese deposit from the south-west Pacific island arcNature, 1982
- Structural features of todorokite intergrowths in manganese nodulesNature, 1982
- Thermal study on some todorokitesThe Journal of the Japanese Association of Mineralogists, Petrologists and Economic Geologists, 1961
- Birnessite, a new manganese oxide mineral from Aberdeenshire, ScotlandMineralogical Magazine and Journal of the Mineralogical Society, 1956