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Main Authors: Dostal, J, Muecke, G K
Format: Dataset Open Access
Language:en
Published: PANGAEA 1978
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Online Access:https://doi.org/10.1594/PANGAEA.695954
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author Dostal, J
Muecke, G K
author_facet Dostal, J
Muecke, G K
collection Datos científicos de ciencias marinas y ambientales
contents 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.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_695954
institution PANGAEA
language en
publishDate 1978
publisher PANGAEA
record_format pangaea
spellingShingle Major and trace element abundances of igneous rocks from DSDP Site 37-334
Dostal, J
Muecke, G K
37-334; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg37; North Atlantic/BASIN
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.
title Major and trace element abundances of igneous rocks from DSDP Site 37-334
topic 37-334; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg37; North Atlantic/BASIN
url https://doi.org/10.1594/PANGAEA.695954