The Open UniversitySkip to content
 

Geochemistry of abyssal peridotites (Mid-Atlantic Ridge, 15 degrees 20 ' N, ODP Leg 209): Implications for fluid/rock interaction in slow spreading environments

Paulick, H.; Bach, W.; Godard, M.; De Hoog, J. C. M.; Suhr, G. and Harvey, Jason (2006). Geochemistry of abyssal peridotites (Mid-Atlantic Ridge, 15 degrees 20 ' N, ODP Leg 209): Implications for fluid/rock interaction in slow spreading environments. Chemical Geology, 234(3-4) pp. 179–210.

DOI (Digital Object Identifier) Link: http://dx.doi.org/10.1016/j.chemgeo.2006.04.011
Google Scholar: Look up in Google Scholar

Abstract

Abyssal peridotite from the 15 degrees 20'N area of the Mid-Atlantic Ridge show complex geochemical variations among the different sites drilled during ODP Leg 209. Major element compositions indicate variable degrees of melt depletion and refertilization as well as local hydrothermal metasomatism. Strongest evidence for melt-rock interactions are correlated Light Rare Earth Element (LREE) and High Field Strength Element (HFSE) additions at Sites 1270 and 1271. In contrast, hydrothermal alteration at Sites 1274, 1272, and 1268 causes LREE mobility associated with minor HFSE variability, reflecting the low solubility of HFSE in aqueous solutions. Site 1274 contains the least-altered, highly refractory, peridotite with strong depletion in LREE and shows a gradual increase in the intensity of isochemical serpentinization; except for the addition of H2O which causes a mass gain of up to 20g/100g. The formation of magnetite is reflected in decreasing Fe2+/Fe3+ ratios. This style of alteration is referred to as rock-dominated serpentinization. In contrast, fluid-dominated serpentinization at Site 1268 is characterized by gains in sulfur and development of U-shaped REE pattern with strong positive Eu anomalies which are also characteristic for hot (350 to 400 degrees C) vent-type fluids discharging from black smoker fields. Serpentinites at Site 1268 were overprinted by talc alteration under static conditions due to interaction with high a(SiO2) fluids causing the development of smooth, LREE enriched patterns with pronounced negative Eu anomalies. These results show that hydrothermal fluid-peridotite and fluid-serpentinite interaction processes are an important factor regarding the budget of exchange processes between the lithosphere and the hydrosphere in slow spreading environments. (c) 2006 Elsevier B.V. All rights reserved.

Item Type: Journal Article
ISSN: 0009-2541
Keywords: Serpentinization; Slow spreading ridges; Abyssal peridotite; Hydrothermal alteration; Geochemistry; Ocean Drilling Program Leg 209
Academic Unit/Department: Science > Environment, Earth and Ecosystems
Interdisciplinary Research Centre: Centre for Earth, Planetary, Space and Astronomical Research (CEPSAR)
Item ID: 16068
Depositing User: Users 8955 not found.
Date Deposited: 12 May 2009 15:21
Last Modified: 02 Dec 2010 20:28
URI: http://oro.open.ac.uk/id/eprint/16068
Share this page:

Altmetrics

Scopus Citations

Actions (login may be required)

View Item
Report issue / request change

Policies | Disclaimer

© The Open University   + 44 (0)870 333 4340   general-enquiries@open.ac.uk