Trace element geochemistry of the peridotite-gabbro-basalt suite from DSDP Leg 37

Details Trace element geochemistry of the peridotite-gabbro-basalt suite from DSDP Leg 37 Trace element geochemistry of the peridotite-gabbro-basalt suite from DSDP Leg 37

Aug 1978

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1978e%26psl..40..415d&link_type=abstract

Earth and Planetary Science Letters, Volume 40, Issue 3, p. 415-422.

Computer Science

6

Scientific paper

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.

Affiliated with

Also associated with

No associations

Rating

Trace element geochemistry of the peridotite-gabbro-basalt suite from DSDP Leg 37 does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

If you have personal experience with Trace element geochemistry of the peridotite-gabbro-basalt suite from DSDP Leg 37, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Trace element geochemistry of the peridotite-gabbro-basalt suite from DSDP Leg 37 will most certainly appreciate the feedback.

Rate now

Comments { 0 }

Profile ID: LFWR-SCP-O-944333