A chemical comparison of oceanic ridge, Hawaiian tholeiitic and Hawaiian alkalic basalts
Abundance data (Al"2O"3, TiO"2, Sr. Zr and REE) for two important groups of basalts (oceanic ridge and Hawaiian) are compared. The average concentrations of Al"2O"3, TiO"2 and Zr are quite different for the two groups but extensive overlap also occurs. TiO"2 and Zr...
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| Autor*in: |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
1968 |
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| Reproduktion: |
Elsevier Journal Backfiles on ScienceDirect 1907 - 2002 |
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| Übergeordnetes Werk: |
in: Earth and Planetary Science Letters - Amsterdam : Elsevier, 5(1968), Seite 346-352 |
| Übergeordnetes Werk: |
volume:5 ; year:1968 ; pages:346-352 |
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| 245 | 1 | 2 | |a A chemical comparison of oceanic ridge, Hawaiian tholeiitic and Hawaiian alkalic basalts |
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| 520 | |a Abundance data (Al"2O"3, TiO"2, Sr. Zr and REE) for two important groups of basalts (oceanic ridge and Hawaiian) are compared. The average concentrations of Al"2O"3, TiO"2 and Zr are quite different for the two groups but extensive overlap also occurs. TiO"2 and Zr are inversely covariant with Al"2O"3 for oceanic ridge and Hawaiian basalts. The Al"2O"3 and TiO"2 data are consistent with the experimental data of Green and Ringwood [5] and MacGregor [25] and suggest that the concentrations of Al"2O"3, TiO"2 and Zr in a wide range of basalt types are dependent on the depth of magma segregation. The two basaltic groups are almost completely different in their Sr concentration and REE abundance patterns. The concentrations of Sr and the REE abundance patterns are essentially independent of the concentrations of Al"2O"3, TiO"2 and Zr. The Sr and REE data can be qualitatively explained by assuming varying degrees of partial melting to form the different liquids observed at the surface. | ||
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(DE-627)NLEJ185246559 (DE-599)GBVNLZ185246559 DE-627 ger DE-627 rakwb eng A chemical comparison of oceanic ridge, Hawaiian tholeiitic and Hawaiian alkalic basalts 1968 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Abundance data (Al"2O"3, TiO"2, Sr. Zr and REE) for two important groups of basalts (oceanic ridge and Hawaiian) are compared. The average concentrations of Al"2O"3, TiO"2 and Zr are quite different for the two groups but extensive overlap also occurs. TiO"2 and Zr are inversely covariant with Al"2O"3 for oceanic ridge and Hawaiian basalts. The Al"2O"3 and TiO"2 data are consistent with the experimental data of Green and Ringwood [5] and MacGregor [25] and suggest that the concentrations of Al"2O"3, TiO"2 and Zr in a wide range of basalt types are dependent on the depth of magma segregation. The two basaltic groups are almost completely different in their Sr concentration and REE abundance patterns. The concentrations of Sr and the REE abundance patterns are essentially independent of the concentrations of Al"2O"3, TiO"2 and Zr. The Sr and REE data can be qualitatively explained by assuming varying degrees of partial melting to form the different liquids observed at the surface. Elsevier Journal Backfiles on ScienceDirect 1907 - 2002 Hubbard, N.J. oth in Earth and Planetary Science Letters Amsterdam : Elsevier 5(1968), Seite 346-352 (DE-627)NLEJ177233850 (DE-600)1466659-5 0012-821X nnns volume:5 year:1968 pages:346-352 http://dx.doi.org/10.1016/S0012-821X(68)80063-9 GBV_USEFLAG_H ZDB-1-SDJ GBV_NL_ARTICLE AR 5 1968 346-352 |
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(DE-627)NLEJ185246559 (DE-599)GBVNLZ185246559 DE-627 ger DE-627 rakwb eng A chemical comparison of oceanic ridge, Hawaiian tholeiitic and Hawaiian alkalic basalts 1968 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Abundance data (Al"2O"3, TiO"2, Sr. Zr and REE) for two important groups of basalts (oceanic ridge and Hawaiian) are compared. The average concentrations of Al"2O"3, TiO"2 and Zr are quite different for the two groups but extensive overlap also occurs. TiO"2 and Zr are inversely covariant with Al"2O"3 for oceanic ridge and Hawaiian basalts. The Al"2O"3 and TiO"2 data are consistent with the experimental data of Green and Ringwood [5] and MacGregor [25] and suggest that the concentrations of Al"2O"3, TiO"2 and Zr in a wide range of basalt types are dependent on the depth of magma segregation. The two basaltic groups are almost completely different in their Sr concentration and REE abundance patterns. The concentrations of Sr and the REE abundance patterns are essentially independent of the concentrations of Al"2O"3, TiO"2 and Zr. The Sr and REE data can be qualitatively explained by assuming varying degrees of partial melting to form the different liquids observed at the surface. Elsevier Journal Backfiles on ScienceDirect 1907 - 2002 Hubbard, N.J. oth in Earth and Planetary Science Letters Amsterdam : Elsevier 5(1968), Seite 346-352 (DE-627)NLEJ177233850 (DE-600)1466659-5 0012-821X nnns volume:5 year:1968 pages:346-352 http://dx.doi.org/10.1016/S0012-821X(68)80063-9 GBV_USEFLAG_H ZDB-1-SDJ GBV_NL_ARTICLE AR 5 1968 346-352 |
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(DE-627)NLEJ185246559 (DE-599)GBVNLZ185246559 DE-627 ger DE-627 rakwb eng A chemical comparison of oceanic ridge, Hawaiian tholeiitic and Hawaiian alkalic basalts 1968 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Abundance data (Al"2O"3, TiO"2, Sr. Zr and REE) for two important groups of basalts (oceanic ridge and Hawaiian) are compared. The average concentrations of Al"2O"3, TiO"2 and Zr are quite different for the two groups but extensive overlap also occurs. TiO"2 and Zr are inversely covariant with Al"2O"3 for oceanic ridge and Hawaiian basalts. The Al"2O"3 and TiO"2 data are consistent with the experimental data of Green and Ringwood [5] and MacGregor [25] and suggest that the concentrations of Al"2O"3, TiO"2 and Zr in a wide range of basalt types are dependent on the depth of magma segregation. The two basaltic groups are almost completely different in their Sr concentration and REE abundance patterns. The concentrations of Sr and the REE abundance patterns are essentially independent of the concentrations of Al"2O"3, TiO"2 and Zr. The Sr and REE data can be qualitatively explained by assuming varying degrees of partial melting to form the different liquids observed at the surface. Elsevier Journal Backfiles on ScienceDirect 1907 - 2002 Hubbard, N.J. oth in Earth and Planetary Science Letters Amsterdam : Elsevier 5(1968), Seite 346-352 (DE-627)NLEJ177233850 (DE-600)1466659-5 0012-821X nnns volume:5 year:1968 pages:346-352 http://dx.doi.org/10.1016/S0012-821X(68)80063-9 GBV_USEFLAG_H ZDB-1-SDJ GBV_NL_ARTICLE AR 5 1968 346-352 |
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(DE-627)NLEJ185246559 (DE-599)GBVNLZ185246559 DE-627 ger DE-627 rakwb eng A chemical comparison of oceanic ridge, Hawaiian tholeiitic and Hawaiian alkalic basalts 1968 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Abundance data (Al"2O"3, TiO"2, Sr. Zr and REE) for two important groups of basalts (oceanic ridge and Hawaiian) are compared. The average concentrations of Al"2O"3, TiO"2 and Zr are quite different for the two groups but extensive overlap also occurs. TiO"2 and Zr are inversely covariant with Al"2O"3 for oceanic ridge and Hawaiian basalts. The Al"2O"3 and TiO"2 data are consistent with the experimental data of Green and Ringwood [5] and MacGregor [25] and suggest that the concentrations of Al"2O"3, TiO"2 and Zr in a wide range of basalt types are dependent on the depth of magma segregation. The two basaltic groups are almost completely different in their Sr concentration and REE abundance patterns. The concentrations of Sr and the REE abundance patterns are essentially independent of the concentrations of Al"2O"3, TiO"2 and Zr. The Sr and REE data can be qualitatively explained by assuming varying degrees of partial melting to form the different liquids observed at the surface. Elsevier Journal Backfiles on ScienceDirect 1907 - 2002 Hubbard, N.J. oth in Earth and Planetary Science Letters Amsterdam : Elsevier 5(1968), Seite 346-352 (DE-627)NLEJ177233850 (DE-600)1466659-5 0012-821X nnns volume:5 year:1968 pages:346-352 http://dx.doi.org/10.1016/S0012-821X(68)80063-9 GBV_USEFLAG_H ZDB-1-SDJ GBV_NL_ARTICLE AR 5 1968 346-352 |
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(DE-627)NLEJ185246559 (DE-599)GBVNLZ185246559 DE-627 ger DE-627 rakwb eng A chemical comparison of oceanic ridge, Hawaiian tholeiitic and Hawaiian alkalic basalts 1968 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Abundance data (Al"2O"3, TiO"2, Sr. Zr and REE) for two important groups of basalts (oceanic ridge and Hawaiian) are compared. The average concentrations of Al"2O"3, TiO"2 and Zr are quite different for the two groups but extensive overlap also occurs. TiO"2 and Zr are inversely covariant with Al"2O"3 for oceanic ridge and Hawaiian basalts. The Al"2O"3 and TiO"2 data are consistent with the experimental data of Green and Ringwood [5] and MacGregor [25] and suggest that the concentrations of Al"2O"3, TiO"2 and Zr in a wide range of basalt types are dependent on the depth of magma segregation. The two basaltic groups are almost completely different in their Sr concentration and REE abundance patterns. The concentrations of Sr and the REE abundance patterns are essentially independent of the concentrations of Al"2O"3, TiO"2 and Zr. The Sr and REE data can be qualitatively explained by assuming varying degrees of partial melting to form the different liquids observed at the surface. Elsevier Journal Backfiles on ScienceDirect 1907 - 2002 Hubbard, N.J. oth in Earth and Planetary Science Letters Amsterdam : Elsevier 5(1968), Seite 346-352 (DE-627)NLEJ177233850 (DE-600)1466659-5 0012-821X nnns volume:5 year:1968 pages:346-352 http://dx.doi.org/10.1016/S0012-821X(68)80063-9 GBV_USEFLAG_H ZDB-1-SDJ GBV_NL_ARTICLE AR 5 1968 346-352 |
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A chemical comparison of oceanic ridge, Hawaiian tholeiitic and Hawaiian alkalic basalts |
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Abundance data (Al"2O"3, TiO"2, Sr. Zr and REE) for two important groups of basalts (oceanic ridge and Hawaiian) are compared. The average concentrations of Al"2O"3, TiO"2 and Zr are quite different for the two groups but extensive overlap also occurs. TiO"2 and Zr are inversely covariant with Al"2O"3 for oceanic ridge and Hawaiian basalts. The Al"2O"3 and TiO"2 data are consistent with the experimental data of Green and Ringwood [5] and MacGregor [25] and suggest that the concentrations of Al"2O"3, TiO"2 and Zr in a wide range of basalt types are dependent on the depth of magma segregation. The two basaltic groups are almost completely different in their Sr concentration and REE abundance patterns. The concentrations of Sr and the REE abundance patterns are essentially independent of the concentrations of Al"2O"3, TiO"2 and Zr. The Sr and REE data can be qualitatively explained by assuming varying degrees of partial melting to form the different liquids observed at the surface. |
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Abundance data (Al"2O"3, TiO"2, Sr. Zr and REE) for two important groups of basalts (oceanic ridge and Hawaiian) are compared. The average concentrations of Al"2O"3, TiO"2 and Zr are quite different for the two groups but extensive overlap also occurs. TiO"2 and Zr are inversely covariant with Al"2O"3 for oceanic ridge and Hawaiian basalts. The Al"2O"3 and TiO"2 data are consistent with the experimental data of Green and Ringwood [5] and MacGregor [25] and suggest that the concentrations of Al"2O"3, TiO"2 and Zr in a wide range of basalt types are dependent on the depth of magma segregation. The two basaltic groups are almost completely different in their Sr concentration and REE abundance patterns. The concentrations of Sr and the REE abundance patterns are essentially independent of the concentrations of Al"2O"3, TiO"2 and Zr. The Sr and REE data can be qualitatively explained by assuming varying degrees of partial melting to form the different liquids observed at the surface. |
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Abundance data (Al"2O"3, TiO"2, Sr. Zr and REE) for two important groups of basalts (oceanic ridge and Hawaiian) are compared. The average concentrations of Al"2O"3, TiO"2 and Zr are quite different for the two groups but extensive overlap also occurs. TiO"2 and Zr are inversely covariant with Al"2O"3 for oceanic ridge and Hawaiian basalts. The Al"2O"3 and TiO"2 data are consistent with the experimental data of Green and Ringwood [5] and MacGregor [25] and suggest that the concentrations of Al"2O"3, TiO"2 and Zr in a wide range of basalt types are dependent on the depth of magma segregation. The two basaltic groups are almost completely different in their Sr concentration and REE abundance patterns. The concentrations of Sr and the REE abundance patterns are essentially independent of the concentrations of Al"2O"3, TiO"2 and Zr. The Sr and REE data can be qualitatively explained by assuming varying degrees of partial melting to form the different liquids observed at the surface. |
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<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">NLEJ185246559</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20210707012524.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">070506s1968 xx |||||o 00| ||eng c</controlfield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)NLEJ185246559</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)GBVNLZ185246559</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="245" ind1="1" ind2="2"><subfield code="a">A chemical comparison of oceanic ridge, Hawaiian tholeiitic and Hawaiian alkalic basalts</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">1968</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zzz</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">z</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zu</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abundance data (Al"2O"3, TiO"2, Sr. Zr and REE) for two important groups of basalts (oceanic ridge and Hawaiian) are compared. The average concentrations of Al"2O"3, TiO"2 and Zr are quite different for the two groups but extensive overlap also occurs. TiO"2 and Zr are inversely covariant with Al"2O"3 for oceanic ridge and Hawaiian basalts. The Al"2O"3 and TiO"2 data are consistent with the experimental data of Green and Ringwood [5] and MacGregor [25] and suggest that the concentrations of Al"2O"3, TiO"2 and Zr in a wide range of basalt types are dependent on the depth of magma segregation. The two basaltic groups are almost completely different in their Sr concentration and REE abundance patterns. The concentrations of Sr and the REE abundance patterns are essentially independent of the concentrations of Al"2O"3, TiO"2 and Zr. The Sr and REE data can be qualitatively explained by assuming varying degrees of partial melting to form the different liquids observed at the surface.</subfield></datafield><datafield tag="533" ind1=" " ind2=" "><subfield code="f">Elsevier Journal Backfiles on ScienceDirect 1907 - 2002</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Hubbard, N.J.</subfield><subfield code="4">oth</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">in</subfield><subfield code="t">Earth and Planetary Science Letters</subfield><subfield code="d">Amsterdam : Elsevier</subfield><subfield code="g">5(1968), Seite 346-352</subfield><subfield code="w">(DE-627)NLEJ177233850</subfield><subfield code="w">(DE-600)1466659-5</subfield><subfield code="x">0012-821X</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:5</subfield><subfield code="g">year:1968</subfield><subfield code="g">pages:346-352</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">http://dx.doi.org/10.1016/S0012-821X(68)80063-9</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_H</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ZDB-1-SDJ</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_NL_ARTICLE</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">5</subfield><subfield code="j">1968</subfield><subfield code="h">346-352</subfield></datafield></record></collection>
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