Kodolányi, János; Pettke, Thomas (2011): Geochemistry of serpentenites from DSDP Hole 84-566C. PANGAEA, https://doi.org/10.1594/PANGAEA.779350, Supplement to: Kodolányi, J; Pettke, T (2011): Loss of trace elements from serpentinites during fluid-assisted transformation of chrysotile to antigorite - An example from Guatemala. Chemical Geology, 284(3-4), 351-362, https://doi.org/10.1016/j.chemgeo.2011.03.016
Always quote above citation when using data! You can download the citation in several formats below.
We studied a unique chrysotile–antigorite serpentinite, drilled on Deep Sea Drilling Project Leg 84 (Site 566) in the Guatemala forearc. Our in situ major and trace element data provide new constraints on possible reactions and associated trace element mobilisation during shallow serpentinite subduction.
Chrysotile of the studied serpentinite, formed by the hydration of an upper mantle peridotite precursor, is partially replaced by antigorite (alone) which also occurs in 0.5 mm wide unoriented veins crosscutting the rock. Based on textural relationships and the P–T–X stability of the rock forming phases, the replacement of chrysotile by antigorite occurred at T < 300 °C, due to interaction between the chrysotile–serpentinite and an aqueous fluid. A comparison of the chemical compositions of reactant and product phases reveals that about 90% of the Cl, more than 80% of the B and about 50% of the Sr hosted originally by chrysotile was lost during fluid-assisted chrysotile-to-antigorite transformation and accompanying partial dehydration, and documents the much lower affinity of antigorite for trace element uptake than that of chrysotile.
The fluid-assisted chrysotile-to-antigorite transformation and associated trace element loss documented here can occur in the shallow (< 30 km) region of subduction zones. This transformation decreases notably the Cl and B inventory of subducting serpentinites, which are regarded as one of the most important carriers of these elements into subduction zones. The evolution of serpentinites during initial subduction stages thus appears to be critical in the recycling of specific trace elements such as B or Cl from forearc to subarc depths.
Latitude: 12.814000 * Longitude: -90.692200
Date/Time Start: 1982-01-24T00:00:00 * Date/Time End: 1982-01-24T00:00:00
84-566C * Latitude: 12.814000 * Longitude: -90.692200 * Date/Time: 1982-01-24T00:00:00 * Elevation: -3661.0 m * Penetration: 136.6 m * Recovery: 5.3 m * Location: North Pacific * Campaign: Leg84 * Basis: Glomar Challenger * Device: Drilling/drill rig (DRILL) * Comment: 5 cores; 46.7 m cored; 19.1 m drilled; 11.4 % recovery
Datasets listed in this Collection
- Kodolányi, J; Pettke, T (2011): (Appendix A) Major element composition of serpentine, brucite, Fe- and Cl-rich hydroxide pseudomorphs and vein fillings of DSDP Hole 84-566C serpentinite. https://doi.org/10.1594/PANGAEA.779348
- Kodolányi, J; Pettke, T (2011): (Table 2) Trace element composition of serpentine and seprentine-hydroxide phase intergrowth, DSDP Hole 84-566C. https://doi.org/10.1594/PANGAEA.779346