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Bibliographic Details
Main Author: Saunders, Andrew D
Format: Dataset Open Access
Language:en
Published: PANGAEA 1987
Subjects:
Online Access:https://doi.org/10.1594/PANGAEA.802521
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author Saunders, Andrew D
author_facet Saunders, Andrew D
collection Datos científicos de ciencias marinas y ambientales
contents Basalts recovered from Sites 595 and 596 on Mesozoic crust in the southwest Pacific range from olivine-bearing tholeiites to ferrobasalts. Despite having undergone extensive low-grade alteration, which has raised K and Rb abundances, the basalts have consistent interelement ratios of Ti, Zr, Hf, rare-earth elements, Y, Th, Ik, and Nb. La/Ta (-18), Lan/Ybn (0.6), Ti/Zr (115), Zr/Nb (20), and Th/Hf (0.08) ratios all fall within the range of N-type mid-ocean-ridge basalt. The basalts from Sites 595 and 596 indicate that the Mesozoic Pacific crust was derived from a mantle source by processes similar to those operating at the present-day East Pacific Rise.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_802521
institution PANGAEA
language en
publishDate 1987
publisher PANGAEA
record_format pangaea
spellingShingle Geochemistry of DSDP Leg 91 basalts
Saunders, Andrew D
Deep Sea Drilling Project; DSDP
Basalts recovered from Sites 595 and 596 on Mesozoic crust in the southwest Pacific range from olivine-bearing tholeiites to ferrobasalts. Despite having undergone extensive low-grade alteration, which has raised K and Rb abundances, the basalts have consistent interelement ratios of Ti, Zr, Hf, rare-earth elements, Y, Th, Ik, and Nb. La/Ta (-18), Lan/Ybn (0.6), Ti/Zr (115), Zr/Nb (20), and Th/Hf (0.08) ratios all fall within the range of N-type mid-ocean-ridge basalt. The basalts from Sites 595 and 596 indicate that the Mesozoic Pacific crust was derived from a mantle source by processes similar to those operating at the present-day East Pacific Rise.
title Geochemistry of DSDP Leg 91 basalts
topic Deep Sea Drilling Project; DSDP
url https://doi.org/10.1594/PANGAEA.802521