Geochemistry of ODP Hole 111-504B basalts (Table 2)


Autoria(s): Autio, Laurie K; Sparks, Joel W; Rhodes, JM
Cobertura

LATITUDE: 1.226900 * LONGITUDE: -83.730300 * DATE/TIME START: 1986-10-05T11:45:00 * DATE/TIME END: 1986-10-16T18:15:00 * MINIMUM DEPTH, sediment/rock: 1354.69 m * MAXIMUM DEPTH, sediment/rock: 1553.87 m

Data(s)

28/10/1989

Resumo

Fifty samples of basalt recovered during ODP Leg 111 from the dikes (Layer 2C) of Hole 504B (1350.0-1562.3 m below seafloor) were analyzed by X-ray-fluorescence techniques. All of the samples are highly depleted in magmaphile elements relative to other mid-ocean ridge basalts, with TiO2 = 0.75-1.24 wt%, Na2O = 1.59-2.22 wt%, Zr = 38-64 ppm, Nb = 0.3-1.5 ppm, and Y = 20-30 ppm (for samples containing 0%-2% phenocrysts), but have ratios of highly incompatible elements similar to normal Type I mid-ocean ridge basalts (e.g., Zr/Nb > 30). Abundances of compatible elements are similar to those of typical mid-ocean ridge basalts, with MgO = 7.2-9.2 wt%, Fe2O3* = 9.3-12.5 wt%, Ni = 55-164 ppm, and Cr = 26-388 ppm. Approximately 2% of the samples recovered from the top part of Hole 504B are similar to normal Type I or Type II ocean floor basalts. However, all of the analyzed Leg 111 samples from Hole 504B are depleted basalts. Aphyric dike rocks from Leg 111 are virtually identical to the depleted aphyric samples recovered from the pillow lavas and dikes in the upper 1075 m of Hole 504B during DSDP Legs 69, 70, and 83, with the exception of elements readily altered by seawater (Sr, Rb, and K). These elements reach a maximum in both abundance and variability in the pillow lavas of the upper 571.5 m of Hole 504B and decline to more constant values in the dike system sampled on Legs 83 and 111, apparently as a result of a decrease in porosity and increase in alteration temperatures relative to the pillow lavas. Based on compositional similarities to the vast majority of the pillows and flows, the dikes sampled on Leg 111 appear to be the feeder system for the pillow lavas in the upper part of Hole 504B. The incompatible-element-depleted compositions of the Costa Rica Rift Zone basalts are consistent with multistage melting of a normal mid-ocean ridge source.

Formato

text/tab-separated-values, 1300 data points

Identificador

https://doi.pangaea.de/10.1594/PANGAEA.748376

doi:10.1594/PANGAEA.748376

Idioma(s)

en

Publicador

PANGAEA

Direitos

CC-BY: Creative Commons Attribution 3.0 Unported

Access constraints: unrestricted

Fonte

Supplement to: Autio, Laurie K; Sparks, Joel W; Rhodes, JM (1989): Geochemistry of Leg 111 basalts: intrusive feeders for highly depleted pillows and flows. In: Becker, K; Sakai, H; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 111, 3-16, doi:10.2973/odp.proc.sr.111.111.1989

Palavras-Chave #111-504B; Aluminium oxide; Calcium oxide; Chromium; Comment; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Gallium; Iron oxide, Fe2O3; Joides Resolution; Leg111; Lithologic unit/sequence; Lithology/composition/facies; Magnesium oxide; Manganese oxide; Nickel; Niobium; North Pacific Ocean; Number; Ocean Drilling Program; ODP; ODP sample designation; Phosphorus oxide; Potassium oxide; Rubidium; Sample code/label; Silicon dioxide; Sodium oxide; Strontium; Sum; Titanium oxide; Vanadium; X-ray spectrometry; Yttrium; Zinc; Zirconium
Tipo

Dataset