Kodolányi, János; Pettke, Thomas (2011): (Table 2) Trace element composition of serpentine and seprentine-hydroxide phase intergrowth, DSDP Hole 84-566C [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.779346, In 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 citation above when using data! You can download the citation in several formats below.
Related to:
Kodolányi, János; Pettke, Thomas; Spandler, Carl; Kamber, Balz S; Gméling, Katalin (2012): Geochemistry of ocean floor and fore-arc serpentinites: Constraints on the ultramafic input to subduction zones. Journal of Petrology, 53(2), 235-270, https://doi.org/10.1093/petrology/egr058
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 12.814000 * Longitude: -90.692200
Date/Time Start: 1982-01-24T00:00:00 * Date/Time End: 1982-01-24T00:00:00
Minimum DEPTH, sediment/rock: 117.45 m * Maximum DEPTH, sediment/rock: 117.45 m
Event(s):
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 * Method/Device: Drilling/drill rig (DRILL) * Comment: 5 cores; 46.7 m cored; 19.1 m drilled; 11.4 % recovery
Parameter(s):
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
224 data points