Permian hydrothermal deposits in the Mino Terrane, central Japan: Implications for hydrothermal plumes in an ancient ocean basin
- 1 April 1991
- journal article
- Published by Elsevier in Sedimentary Geology
- Vol. 71 (1-2) , 59-71
- https://doi.org/10.1016/0037-0738(91)90007-z
Abstract
No abstract availableThis publication has 33 references indexed in Scilit:
- Geochemical characteristics and depositional environments of cherts and associated rocks in the Franciscan and Shimanto TerranesPublished by Elsevier ,2003
- Late Paleozoic geosynclinal basalt and tectonism in the Japanese IslandsPublished by Elsevier ,2003
- Hydrothermal chert and associated siliceous rocks from the northern Pacific their geological significance as indication od ocean ridge activityPublished by Elsevier ,2003
- Manganese Carbonate Bands as an Indicator of Hemipelagic Sedimentary EnvironmentsThe Journal of Geology, 1991
- Hydrothermal silica chimney fields in the Galapagos Spreading Center at 86°WEarth and Planetary Science Letters, 1988
- Compositional Variations in Manganese Micronodules: A Possible Indicator of Sedimentary EnvironmentsThe Journal of Geology, 1987
- Iron and copper enrichment of suspended particles in dispersed hydrothermal plumes along the mid‐Atlantic RidgeGeophysical Research Letters, 1985
- Mesozoic metalliferous sediments from the ophiolites of Ermioni, Greece; analogue to Recent mid-ocean ridge ferromanganese depositsChemical Geology, 1984
- Triassic bedded cherts in central Japan are not pelagicNature, 1982
- Metallogenesis along a fossil oceanic fracture zone: Arakapas fault belt, Troodos Massif, CyprusEarth and Planetary Science Letters, 1978