Banerjee, Neil R. and Honnorez, Jose (2004): Low-temperature alteration of upper oceanic crust from the Ontong Java Plateau, Leg 192; alteration and vein logs

Leg/Site/Hole:
ODP 192
ODP 192 1183
ODP 192 1185
ODP 192 1186
ODP 192 1187
Identifier:
2005-004703
georefid

10.2973/odp.proc.sr.192.103.2004
doi

Creator:
Banerjee, Neil R.
University of Alberta, School of Earth and Ocean Sciences, Edmonton, AB, Canada
author

Honnorez, Jose
University of Hawaii at Manoa, United States
author

Identification:
Low-temperature alteration of upper oceanic crust from the Ontong Java Plateau, Leg 192; alteration and vein logs
2004
In: Fitton, J. Godfrey, Mahoney, John J., Wallace, Paul J., Antretter, Maria J., Banerjee, Neil R., Bergen, James A., Cairns, Graeme, Castillo, Paterno R., Chambers, Lynne M., Chazey, William J., III, Coffin, Millard F., Godard, Marguerite M., Hall, Stuart A., Honnorez, Jose, Ingle, Stephanie P., Kroenke, Loren W., MacLeod, Kenneth G., Naruse, Hajime, Neal, Clive R., Ogg, James G., Riisager, Peter, Sano, Takahashi, Sikora, Paul J., van der Werff, Wietze, White, Rosalind V., Zhao, Xixi, Proceedings of the Ocean Drilling Program; scientific results; basement drilling of the Ontong Java Plateau; covering Leg 192 of the cruises of the drilling vessel JOIDES Resolution; Apra Harbor, Guam, to Apra Harbor, Guam; Sites 1183-1187; 8 September-7 November 2000
Texas A&M University, Ocean Drilling Program, College Station, TX, United States
192
This paper presents alteration data for basalts from Ocean Drilling Program (ODP) Sites 1183, 1185, 1186, and 1187 drilled on the Ontong Java Plateau during Leg 192. The entire sequence of recovered basaltic basement has undergone low-temperature water-rock interactions. Alteration and vein logs were compiled for each hole from visual core descriptions made aboard the ship. These logs quantify the alteration types, provide a consistent alteration characterization of the samples, and provide a method for estimation of downhole variations in basalt alteration and vein abundance/mineralogy. The three main alteration types identified include gray basalt, black or dusky green halos, and brown or olive halos. Secondary minerals, in order of decreasing abundance, include phyllosilicates, calcite, pyrite, chalcedony, quartz, Fe oxyhydroxides, and zeolites. Veins commonly contain smectite and/or celadonite, Fe oxyhydroxide or pyrite, and calcite. Alteration of basalts from the Ontong Java Plateau is similar to that observed from other Deep Sea Drilling Program/ODP sites drilled into the upper oceanic crust.
English
Coverage:Geographic coordinates:
North:0.5600
West:157.0100East: 161.4000
South:-1.1100

Igneous and metamorphic petrology; alteration; basalts; cores; crust; glasses; haloes; igneous rocks; Leg 192; low temperature; mineral composition; Ocean Drilling Program; oceanic crust; ODP Site 1183; ODP Site 1185; ODP Site 1186; ODP Site 1187; Ontong Java Plateau; Pacific Ocean; phenocrysts; temperature; upper crust; veins; volcanic rocks; water-rock interaction; West Pacific; X-ray diffraction data;

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