Dostal, J; Muecke, G K (1978): Major and trace element abundances of igneous rocks from DSDP Site 37-334 [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.695954, Supplement to: Dostal, J; Muecke, GK (1978): Trace element geochemistry of the peridotite-gabbro-basalt suite from DSDP Leg 37. Earth and Planetary Science Letters, 40(3), 415-422, https://doi.org/10.1016/0012-821X(78)90164-4
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Abstract:
REE abundances in gabbros and peridotites from Site 334 of DSDP Leg 37 show that these rocks are cumulates produced by fractional crystallization of a primitive oceanic tholeiite magma. They may be part of a layered oceanic complex. The REE distributions in the residual liquids left after such a fractionation are similar to those of incompatible element-depleted oceanic tholeiites. The REE data indicate that the basalts which overlie the gabbro-peridotite complex, are not genetically related to plutonic rocks.
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 37.035500 * Longitude: -34.414500
Date/Time Start: 1974-07-14T00:00:00 * Date/Time End: 1974-07-14T00:00:00
Event(s):
37-334 * Latitude: 37.035500 * Longitude: -34.414500 * Date/Time: 1974-07-14T00:00:00 * Elevation: -2619.0 m * Penetration: 376.5 m * Recovery: 98.1 m * Location: North Atlantic/BASIN * Campaign: Leg37 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 27 cores; 253 m cored; 0 m drilled; 38.8 % recovery
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
2 datasets
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Datasets listed in this publication series
- Dostal, J; Muecke, GK (1978): (Table 2) Major element composition of igneous rocks from DSDP Site 37-334. https://doi.org/10.1594/PANGAEA.695953
- Dostal, J; Muecke, GK (1978): (Table 1) Trace element abundances of igneous rocks from DSDP Site 37-334. https://doi.org/10.1594/PANGAEA.695951