Mineral composition of mid-ocean-ridge basalts from ODP Leg 187 sites ...

The chemical compositions of olivine, plagioclase, pyroxene, and spinel in lavas collected during Ocean Drilling Program Leg 187 in the Australian Antarctic Discordance, Southeast Indian Ridge (41°-46°S, 126°-135°E) were analyzed, and modeling of the theoretical equilibrium petrogenetic conditions b...

Full description

Bibliographic Details
Main Author: Sato, Hiroshi
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2004
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.780714
https://doi.pangaea.de/10.1594/PANGAEA.780714
id ftdatacite:10.1594/pangaea.780714
record_format openpolar
spelling ftdatacite:10.1594/pangaea.780714 2024-09-15T17:47:23+00:00 Mineral composition of mid-ocean-ridge basalts from ODP Leg 187 sites ... Sato, Hiroshi 2004 application/zip https://dx.doi.org/10.1594/pangaea.780714 https://doi.pangaea.de/10.1594/PANGAEA.780714 en eng PANGAEA https://dx.doi.org/10.2973/odp.proc.sr.187.202.2004 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Drilling/drill rig Leg187 Joides Resolution Ocean Drilling Program ODP article Collection Supplementary Publication Series of Datasets 2004 ftdatacite https://doi.org/10.1594/pangaea.78071410.2973/odp.proc.sr.187.202.2004 2024-08-01T10:52:43Z The chemical compositions of olivine, plagioclase, pyroxene, and spinel in lavas collected during Ocean Drilling Program Leg 187 in the Australian Antarctic Discordance, Southeast Indian Ridge (41°-46°S, 126°-135°E) were analyzed, and modeling of the theoretical equilibrium petrogenetic conditions between olivine and melt was conducted. The cores of larger olivine phenocrysts, particularly in the isotopic Indian-type mid-ocean-ridge basalt (MORB), are not equilibrated with melt compositions and are considered to be xenocrystic. Larger plagioclase phenocrysts with compositionally reversed zonation are also xenocrystic. The compositions of primary magma were calculated using a "maximum olivine fractionation" model for primitive MORB that should fractionate only olivine. Olivine compositions equilibrated with calculated primary magma and compositions of calculated primary magma suggest that (1) isotopic Pacific-type MORB is more fractionated than Indian-type MORB, (2) Pacific-type MORB was produced by higher ... : Supplement to: Sato, Hiroshi (2004): Mineral compositions of MORB from the Australian Antarctic Discordance (AAD): implications for mantle source characteristics. In: Pedersen, RB; Christie, DM; Miller, DJ (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 187, 1-26 ... Article in Journal/Newspaper Antarc* Antarctic DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Drilling/drill rig
Leg187
Joides Resolution
Ocean Drilling Program ODP
spellingShingle Drilling/drill rig
Leg187
Joides Resolution
Ocean Drilling Program ODP
Sato, Hiroshi
Mineral composition of mid-ocean-ridge basalts from ODP Leg 187 sites ...
topic_facet Drilling/drill rig
Leg187
Joides Resolution
Ocean Drilling Program ODP
description The chemical compositions of olivine, plagioclase, pyroxene, and spinel in lavas collected during Ocean Drilling Program Leg 187 in the Australian Antarctic Discordance, Southeast Indian Ridge (41°-46°S, 126°-135°E) were analyzed, and modeling of the theoretical equilibrium petrogenetic conditions between olivine and melt was conducted. The cores of larger olivine phenocrysts, particularly in the isotopic Indian-type mid-ocean-ridge basalt (MORB), are not equilibrated with melt compositions and are considered to be xenocrystic. Larger plagioclase phenocrysts with compositionally reversed zonation are also xenocrystic. The compositions of primary magma were calculated using a "maximum olivine fractionation" model for primitive MORB that should fractionate only olivine. Olivine compositions equilibrated with calculated primary magma and compositions of calculated primary magma suggest that (1) isotopic Pacific-type MORB is more fractionated than Indian-type MORB, (2) Pacific-type MORB was produced by higher ... : Supplement to: Sato, Hiroshi (2004): Mineral compositions of MORB from the Australian Antarctic Discordance (AAD): implications for mantle source characteristics. In: Pedersen, RB; Christie, DM; Miller, DJ (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 187, 1-26 ...
format Article in Journal/Newspaper
author Sato, Hiroshi
author_facet Sato, Hiroshi
author_sort Sato, Hiroshi
title Mineral composition of mid-ocean-ridge basalts from ODP Leg 187 sites ...
title_short Mineral composition of mid-ocean-ridge basalts from ODP Leg 187 sites ...
title_full Mineral composition of mid-ocean-ridge basalts from ODP Leg 187 sites ...
title_fullStr Mineral composition of mid-ocean-ridge basalts from ODP Leg 187 sites ...
title_full_unstemmed Mineral composition of mid-ocean-ridge basalts from ODP Leg 187 sites ...
title_sort mineral composition of mid-ocean-ridge basalts from odp leg 187 sites ...
publisher PANGAEA
publishDate 2004
url https://dx.doi.org/10.1594/pangaea.780714
https://doi.pangaea.de/10.1594/PANGAEA.780714
genre Antarc*
Antarctic
genre_facet Antarc*
Antarctic
op_relation https://dx.doi.org/10.2973/odp.proc.sr.187.202.2004
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.78071410.2973/odp.proc.sr.187.202.2004
_version_ 1810496649092399104