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Hauptverfasser: Iyer, S D, Mukhopadhyay, R, Popko, D C
Format: Dataset Open Access
Sprache:en
Veröffentlicht: PANGAEA 2007
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Online-Zugang:https://doi.org/10.1594/PANGAEA.670932
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author Iyer, S D
Mukhopadhyay, R
Popko, D C
author_facet Iyer, S D
Mukhopadhyay, R
Popko, D C
collection Datos científicos de ciencias marinas y ambientales
contents We report the occurrence of ferrobasalts recovered from the Central Indian Ocean Basin crust generated at the Southeast Indian Ridge during a phase of moderate to fast spreading accretion (~110-190 mm/yr, full rate).The rocks are rich in plagioclase, FeO* (13/19 %), and TiO2 (2.27/2.76 %), poor in olivine and MgO (3.44/6.20%), and associated with topographic highs and increased amplitude magnetic anomalies corresponding to chrons A25 and A24. We suggest that secon dary eruptions from ancient N-MORB magma, which may have been trapped at a shallow depth in a horizon of neutral buoyancy, could have produced the ferrobasalts.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_670932
institution PANGAEA
language en
publishDate 2007
publisher PANGAEA
record_format pangaea
spellingShingle Major and trace element composition in the Central Indian Ocean Basin ferrobasalts (Table 2, 3)
Iyer, S D
Mukhopadhyay, R
Popko, D C
Aluminium oxide; Barium; Calcium oxide; Chromium; CIOB; Cobalt; Copper; Depth, bathymetric; DEPTH, sediment/rock; Dredge; DRG; Indian Ocean; Iron oxide, FeO; LATITUDE; Lithology/composition/facies; LONGITUDE; Magnesium oxide; Manganese oxide; Nickel; Phosphorus pentoxide; Potassium oxide; Sample code/label; Sample comment; Silicon dioxide; Sodium oxide; Titanium dioxide; Vanadium; Yttrium; Zinc; Zirconium
We report the occurrence of ferrobasalts recovered from the Central Indian Ocean Basin crust generated at the Southeast Indian Ridge during a phase of moderate to fast spreading accretion (~110-190 mm/yr, full rate).The rocks are rich in plagioclase, FeO* (13/19 %), and TiO2 (2.27/2.76 %), poor in olivine and MgO (3.44/6.20%), and associated with topographic highs and increased amplitude magnetic anomalies corresponding to chrons A25 and A24. We suggest that secon dary eruptions from ancient N-MORB magma, which may have been trapped at a shallow depth in a horizon of neutral buoyancy, could have produced the ferrobasalts.
title Major and trace element composition in the Central Indian Ocean Basin ferrobasalts (Table 2, 3)
topic Aluminium oxide; Barium; Calcium oxide; Chromium; CIOB; Cobalt; Copper; Depth, bathymetric; DEPTH, sediment/rock; Dredge; DRG; Indian Ocean; Iron oxide, FeO; LATITUDE; Lithology/composition/facies; LONGITUDE; Magnesium oxide; Manganese oxide; Nickel; Phosphorus pentoxide; Potassium oxide; Sample code/label; Sample comment; Silicon dioxide; Sodium oxide; Titanium dioxide; Vanadium; Yttrium; Zinc; Zirconium
url https://doi.org/10.1594/PANGAEA.670932