REE compositional characteristics of Hannuoba basalts
Abstract The Hannuoba basalts are a suite of associated rocks consisting of alkali basalts and tholeiites. The alkali basalts can be divided into the K-rich type and the Na-rich type, while the tholeiites are almost solely of the Na-rich type. These two types of basalt are characterized as being obv...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Shaobing, Li [verfasserIn] |
|---|
| Format: |
Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
1988 |
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| Schlagwörter: |
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| Anmerkung: |
© Institute of Geochemistry, Chinese Academy of Sciences 1988 |
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| Übergeordnetes Werk: |
Enthalten in: Chinese journal of geochemistry - Science in China Press, 1985, 7(1988), 3 vom: Juli, Seite 243-251 |
|---|---|
| Übergeordnetes Werk: |
volume:7 ; year:1988 ; number:3 ; month:07 ; pages:243-251 |
| Links: |
|---|
| DOI / URN: |
10.1007/BF02840966 |
|---|
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| 520 | |a Abstract The Hannuoba basalts are a suite of associated rocks consisting of alkali basalts and tholeiites. The alkali basalts can be divided into the K-rich type and the Na-rich type, while the tholeiites are almost solely of the Na-rich type. These two types of basalt are characterized as being obviously rich in light rare earth elements, as is shown in the chondrite-normalized REE patterns exhibiting positive Eu anomalies. However, significant differences in (La / Yb)N and Eu / Eu* ratios are noticed between these two types of basalt. They seem to have been derived from varying-degree partial melting of mantle rocks. | ||
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10.1007/BF02840966 doi (DE-627)OLC2088096094 (DE-He213)BF02840966-p DE-627 ger DE-627 rakwb eng 550 540 VZ 13 ssgn Shaobing, Li verfasserin aut REE compositional characteristics of Hannuoba basalts 1988 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Institute of Geochemistry, Chinese Academy of Sciences 1988 Abstract The Hannuoba basalts are a suite of associated rocks consisting of alkali basalts and tholeiites. The alkali basalts can be divided into the K-rich type and the Na-rich type, while the tholeiites are almost solely of the Na-rich type. These two types of basalt are characterized as being obviously rich in light rare earth elements, as is shown in the chondrite-normalized REE patterns exhibiting positive Eu anomalies. However, significant differences in (La / Yb)N and Eu / Eu* ratios are noticed between these two types of basalt. They seem to have been derived from varying-degree partial melting of mantle rocks. Partial Melting Alkali Basalt Mantle Rock Olivine Basalt Cenozoic Basalt Delin, Liu aut Zhenjiang, Zhang aut Jianen, Xu aut Enthalten in Chinese journal of geochemistry Science in China Press, 1985 7(1988), 3 vom: Juli, Seite 243-251 (DE-627)130963208 (DE-600)1066729-5 (DE-576)077051459 1000-9426 nnns volume:7 year:1988 number:3 month:07 pages:243-251 https://doi.org/10.1007/BF02840966 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_4012 AR 7 1988 3 07 243-251 |
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10.1007/BF02840966 doi (DE-627)OLC2088096094 (DE-He213)BF02840966-p DE-627 ger DE-627 rakwb eng 550 540 VZ 13 ssgn Shaobing, Li verfasserin aut REE compositional characteristics of Hannuoba basalts 1988 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Institute of Geochemistry, Chinese Academy of Sciences 1988 Abstract The Hannuoba basalts are a suite of associated rocks consisting of alkali basalts and tholeiites. The alkali basalts can be divided into the K-rich type and the Na-rich type, while the tholeiites are almost solely of the Na-rich type. These two types of basalt are characterized as being obviously rich in light rare earth elements, as is shown in the chondrite-normalized REE patterns exhibiting positive Eu anomalies. However, significant differences in (La / Yb)N and Eu / Eu* ratios are noticed between these two types of basalt. They seem to have been derived from varying-degree partial melting of mantle rocks. Partial Melting Alkali Basalt Mantle Rock Olivine Basalt Cenozoic Basalt Delin, Liu aut Zhenjiang, Zhang aut Jianen, Xu aut Enthalten in Chinese journal of geochemistry Science in China Press, 1985 7(1988), 3 vom: Juli, Seite 243-251 (DE-627)130963208 (DE-600)1066729-5 (DE-576)077051459 1000-9426 nnns volume:7 year:1988 number:3 month:07 pages:243-251 https://doi.org/10.1007/BF02840966 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_4012 AR 7 1988 3 07 243-251 |
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10.1007/BF02840966 doi (DE-627)OLC2088096094 (DE-He213)BF02840966-p DE-627 ger DE-627 rakwb eng 550 540 VZ 13 ssgn Shaobing, Li verfasserin aut REE compositional characteristics of Hannuoba basalts 1988 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Institute of Geochemistry, Chinese Academy of Sciences 1988 Abstract The Hannuoba basalts are a suite of associated rocks consisting of alkali basalts and tholeiites. The alkali basalts can be divided into the K-rich type and the Na-rich type, while the tholeiites are almost solely of the Na-rich type. These two types of basalt are characterized as being obviously rich in light rare earth elements, as is shown in the chondrite-normalized REE patterns exhibiting positive Eu anomalies. However, significant differences in (La / Yb)N and Eu / Eu* ratios are noticed between these two types of basalt. They seem to have been derived from varying-degree partial melting of mantle rocks. Partial Melting Alkali Basalt Mantle Rock Olivine Basalt Cenozoic Basalt Delin, Liu aut Zhenjiang, Zhang aut Jianen, Xu aut Enthalten in Chinese journal of geochemistry Science in China Press, 1985 7(1988), 3 vom: Juli, Seite 243-251 (DE-627)130963208 (DE-600)1066729-5 (DE-576)077051459 1000-9426 nnns volume:7 year:1988 number:3 month:07 pages:243-251 https://doi.org/10.1007/BF02840966 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_4012 AR 7 1988 3 07 243-251 |
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10.1007/BF02840966 doi (DE-627)OLC2088096094 (DE-He213)BF02840966-p DE-627 ger DE-627 rakwb eng 550 540 VZ 13 ssgn Shaobing, Li verfasserin aut REE compositional characteristics of Hannuoba basalts 1988 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Institute of Geochemistry, Chinese Academy of Sciences 1988 Abstract The Hannuoba basalts are a suite of associated rocks consisting of alkali basalts and tholeiites. The alkali basalts can be divided into the K-rich type and the Na-rich type, while the tholeiites are almost solely of the Na-rich type. These two types of basalt are characterized as being obviously rich in light rare earth elements, as is shown in the chondrite-normalized REE patterns exhibiting positive Eu anomalies. However, significant differences in (La / Yb)N and Eu / Eu* ratios are noticed between these two types of basalt. They seem to have been derived from varying-degree partial melting of mantle rocks. Partial Melting Alkali Basalt Mantle Rock Olivine Basalt Cenozoic Basalt Delin, Liu aut Zhenjiang, Zhang aut Jianen, Xu aut Enthalten in Chinese journal of geochemistry Science in China Press, 1985 7(1988), 3 vom: Juli, Seite 243-251 (DE-627)130963208 (DE-600)1066729-5 (DE-576)077051459 1000-9426 nnns volume:7 year:1988 number:3 month:07 pages:243-251 https://doi.org/10.1007/BF02840966 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_4012 AR 7 1988 3 07 243-251 |
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10.1007/BF02840966 doi (DE-627)OLC2088096094 (DE-He213)BF02840966-p DE-627 ger DE-627 rakwb eng 550 540 VZ 13 ssgn Shaobing, Li verfasserin aut REE compositional characteristics of Hannuoba basalts 1988 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Institute of Geochemistry, Chinese Academy of Sciences 1988 Abstract The Hannuoba basalts are a suite of associated rocks consisting of alkali basalts and tholeiites. The alkali basalts can be divided into the K-rich type and the Na-rich type, while the tholeiites are almost solely of the Na-rich type. These two types of basalt are characterized as being obviously rich in light rare earth elements, as is shown in the chondrite-normalized REE patterns exhibiting positive Eu anomalies. However, significant differences in (La / Yb)N and Eu / Eu* ratios are noticed between these two types of basalt. They seem to have been derived from varying-degree partial melting of mantle rocks. Partial Melting Alkali Basalt Mantle Rock Olivine Basalt Cenozoic Basalt Delin, Liu aut Zhenjiang, Zhang aut Jianen, Xu aut Enthalten in Chinese journal of geochemistry Science in China Press, 1985 7(1988), 3 vom: Juli, Seite 243-251 (DE-627)130963208 (DE-600)1066729-5 (DE-576)077051459 1000-9426 nnns volume:7 year:1988 number:3 month:07 pages:243-251 https://doi.org/10.1007/BF02840966 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_4012 AR 7 1988 3 07 243-251 |
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Abstract The Hannuoba basalts are a suite of associated rocks consisting of alkali basalts and tholeiites. The alkali basalts can be divided into the K-rich type and the Na-rich type, while the tholeiites are almost solely of the Na-rich type. These two types of basalt are characterized as being obviously rich in light rare earth elements, as is shown in the chondrite-normalized REE patterns exhibiting positive Eu anomalies. However, significant differences in (La / Yb)N and Eu / Eu* ratios are noticed between these two types of basalt. They seem to have been derived from varying-degree partial melting of mantle rocks. © Institute of Geochemistry, Chinese Academy of Sciences 1988 |
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Abstract The Hannuoba basalts are a suite of associated rocks consisting of alkali basalts and tholeiites. The alkali basalts can be divided into the K-rich type and the Na-rich type, while the tholeiites are almost solely of the Na-rich type. These two types of basalt are characterized as being obviously rich in light rare earth elements, as is shown in the chondrite-normalized REE patterns exhibiting positive Eu anomalies. However, significant differences in (La / Yb)N and Eu / Eu* ratios are noticed between these two types of basalt. They seem to have been derived from varying-degree partial melting of mantle rocks. © Institute of Geochemistry, Chinese Academy of Sciences 1988 |
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Abstract The Hannuoba basalts are a suite of associated rocks consisting of alkali basalts and tholeiites. The alkali basalts can be divided into the K-rich type and the Na-rich type, while the tholeiites are almost solely of the Na-rich type. These two types of basalt are characterized as being obviously rich in light rare earth elements, as is shown in the chondrite-normalized REE patterns exhibiting positive Eu anomalies. However, significant differences in (La / Yb)N and Eu / Eu* ratios are noticed between these two types of basalt. They seem to have been derived from varying-degree partial melting of mantle rocks. © Institute of Geochemistry, Chinese Academy of Sciences 1988 |
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<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000naa a22002652 4500</leader><controlfield tag="001">OLC2088096094</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230303045039.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">230303s1988 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/BF02840966</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2088096094</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)BF02840966-p</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="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="a">540</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">13</subfield><subfield code="2">ssgn</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Shaobing, Li</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">REE compositional characteristics of Hannuoba basalts</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">1988</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Institute of Geochemistry, Chinese Academy of Sciences 1988</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract The Hannuoba basalts are a suite of associated rocks consisting of alkali basalts and tholeiites. The alkali basalts can be divided into the K-rich type and the Na-rich type, while the tholeiites are almost solely of the Na-rich type. These two types of basalt are characterized as being obviously rich in light rare earth elements, as is shown in the chondrite-normalized REE patterns exhibiting positive Eu anomalies. However, significant differences in (La / Yb)N and Eu / Eu* ratios are noticed between these two types of basalt. They seem to have been derived from varying-degree partial melting of mantle rocks.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Partial Melting</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Alkali Basalt</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Mantle Rock</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Olivine Basalt</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Cenozoic Basalt</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Delin, Liu</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Zhenjiang, Zhang</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Jianen, Xu</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Chinese journal of geochemistry</subfield><subfield code="d">Science in China Press, 1985</subfield><subfield code="g">7(1988), 3 vom: Juli, Seite 243-251</subfield><subfield code="w">(DE-627)130963208</subfield><subfield code="w">(DE-600)1066729-5</subfield><subfield code="w">(DE-576)077051459</subfield><subfield code="x">1000-9426</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:7</subfield><subfield code="g">year:1988</subfield><subfield code="g">number:3</subfield><subfield code="g">month:07</subfield><subfield code="g">pages:243-251</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1007/BF02840966</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_22</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4012</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">7</subfield><subfield code="j">1988</subfield><subfield code="e">3</subfield><subfield code="c">07</subfield><subfield code="h">243-251</subfield></datafield></record></collection>
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