Strontium and neodymium isotope study of Bohemian basalts

Summary The Cenozoic alkaline basalts of northern and western Bohemia are part of the Central European Volcanic Province (CEVP) which extends from the Rhineland (Eifel, Germany) to Moravia (Czechoslovakia) and the Lover Silesia (Poland). Seven samlpes from locations within Czechoslovakia have been a...
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Gespeichert in:

Autor*in:	Bendl, J. [verfasserIn] Vokurka, K. Sundvoll, B.

Format:	Artikel
Sprache:	Englisch

Erschienen:	1993

Schlagwörter:	Ocean Island Basalt Alkaline Basalt Cenozoic Basalt Silicate Earth Bulk Silicate

Systematik:	TE 1000

Anmerkung:	© Springer-Verlag 1993

Übergeordnetes Werk:	Enthalten in: Mineralogy and petrology - Springer-Verlag, 1987, 48(1993), 1 vom: März, Seite 35-45
Übergeordnetes Werk:	volume:48 ; year:1993 ; number:1 ; month:03 ; pages:35-45

Links:	Volltext

DOI / URN:	10.1007/BF01164907

Katalog-ID:	OLC2062478437

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allfields	10.1007/BF01164907 doi (DE-627)OLC2062478437 (DE-He213)BF01164907-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn TE 1000 VZ rvk Bendl, J. verfasserin aut Strontium and neodymium isotope study of Bohemian basalts 1993 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1993 Summary The Cenozoic alkaline basalts of northern and western Bohemia are part of the Central European Volcanic Province (CEVP) which extends from the Rhineland (Eifel, Germany) to Moravia (Czechoslovakia) and the Lover Silesia (Poland). Seven samlpes from locations within Czechoslovakia have been analyzed isotopically for the Rb-Sr and the Sm-Nd systems. Present-day, normalised 87Sr/86Sr ratios range from 0.7031 to 0.7036, and the corresponding 143Nd/144Nd ratios range from 0.51279 to 0.51286. An eigth sample from the Silurian basalts of the ‘St. Jan’ type (K-Ar age: 420 Ma) occuring in the Barrandian basin in Central Bohemia is also analysed. Its Present-day, normalised, 87Sr/86Sr ratio is 0.7031, and the corresponding 143Nd/144Nd ratio 0.51288. The Nd ratios of the Cenozoic basalts are similar, but more restricted than those from Germany, but are lower than those from Lower Silesia; a trend which is converse for the Sr ratios. Comparison of the results with the systematics ofZindler andHart (1986), suggests that the mande reservoir source of the Bohemian Cenozoic CEVP basalts is similar to the HIMU (High-μ ocean island basalts), with transition to PUM (primitive upper mantle) or BSE (bulk silicate earth). The reservoir for the Silurian Barrandian basin basalts suggest some affinity to MORB (mid-ocean ridge basalts) or HIMU. Ocean Island Basalt Alkaline Basalt Cenozoic Basalt Silicate Earth Bulk Silicate Vokurka, K. aut Sundvoll, B. aut Enthalten in Mineralogy and petrology Springer-Verlag, 1987 48(1993), 1 vom: März, Seite 35-45 (DE-627)129383856 (DE-600)166036-6 (DE-576)014770881 0930-0708 nnns volume:48 year:1993 number:1 month:03 pages:35-45 https://doi.org/10.1007/BF01164907 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_31 GBV_ILN_40 GBV_ILN_65 GBV_ILN_70 GBV_ILN_2004 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4029 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4306 GBV_ILN_4307 TE 1000 AR 48 1993 1 03 35-45
spelling	10.1007/BF01164907 doi (DE-627)OLC2062478437 (DE-He213)BF01164907-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn TE 1000 VZ rvk Bendl, J. verfasserin aut Strontium and neodymium isotope study of Bohemian basalts 1993 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1993 Summary The Cenozoic alkaline basalts of northern and western Bohemia are part of the Central European Volcanic Province (CEVP) which extends from the Rhineland (Eifel, Germany) to Moravia (Czechoslovakia) and the Lover Silesia (Poland). Seven samlpes from locations within Czechoslovakia have been analyzed isotopically for the Rb-Sr and the Sm-Nd systems. Present-day, normalised 87Sr/86Sr ratios range from 0.7031 to 0.7036, and the corresponding 143Nd/144Nd ratios range from 0.51279 to 0.51286. An eigth sample from the Silurian basalts of the ‘St. Jan’ type (K-Ar age: 420 Ma) occuring in the Barrandian basin in Central Bohemia is also analysed. Its Present-day, normalised, 87Sr/86Sr ratio is 0.7031, and the corresponding 143Nd/144Nd ratio 0.51288. The Nd ratios of the Cenozoic basalts are similar, but more restricted than those from Germany, but are lower than those from Lower Silesia; a trend which is converse for the Sr ratios. Comparison of the results with the systematics ofZindler andHart (1986), suggests that the mande reservoir source of the Bohemian Cenozoic CEVP basalts is similar to the HIMU (High-μ ocean island basalts), with transition to PUM (primitive upper mantle) or BSE (bulk silicate earth). The reservoir for the Silurian Barrandian basin basalts suggest some affinity to MORB (mid-ocean ridge basalts) or HIMU. Ocean Island Basalt Alkaline Basalt Cenozoic Basalt Silicate Earth Bulk Silicate Vokurka, K. aut Sundvoll, B. aut Enthalten in Mineralogy and petrology Springer-Verlag, 1987 48(1993), 1 vom: März, Seite 35-45 (DE-627)129383856 (DE-600)166036-6 (DE-576)014770881 0930-0708 nnns volume:48 year:1993 number:1 month:03 pages:35-45 https://doi.org/10.1007/BF01164907 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_31 GBV_ILN_40 GBV_ILN_65 GBV_ILN_70 GBV_ILN_2004 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4029 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4306 GBV_ILN_4307 TE 1000 AR 48 1993 1 03 35-45
allfields_unstemmed	10.1007/BF01164907 doi (DE-627)OLC2062478437 (DE-He213)BF01164907-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn TE 1000 VZ rvk Bendl, J. verfasserin aut Strontium and neodymium isotope study of Bohemian basalts 1993 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1993 Summary The Cenozoic alkaline basalts of northern and western Bohemia are part of the Central European Volcanic Province (CEVP) which extends from the Rhineland (Eifel, Germany) to Moravia (Czechoslovakia) and the Lover Silesia (Poland). Seven samlpes from locations within Czechoslovakia have been analyzed isotopically for the Rb-Sr and the Sm-Nd systems. Present-day, normalised 87Sr/86Sr ratios range from 0.7031 to 0.7036, and the corresponding 143Nd/144Nd ratios range from 0.51279 to 0.51286. An eigth sample from the Silurian basalts of the ‘St. Jan’ type (K-Ar age: 420 Ma) occuring in the Barrandian basin in Central Bohemia is also analysed. Its Present-day, normalised, 87Sr/86Sr ratio is 0.7031, and the corresponding 143Nd/144Nd ratio 0.51288. The Nd ratios of the Cenozoic basalts are similar, but more restricted than those from Germany, but are lower than those from Lower Silesia; a trend which is converse for the Sr ratios. Comparison of the results with the systematics ofZindler andHart (1986), suggests that the mande reservoir source of the Bohemian Cenozoic CEVP basalts is similar to the HIMU (High-μ ocean island basalts), with transition to PUM (primitive upper mantle) or BSE (bulk silicate earth). The reservoir for the Silurian Barrandian basin basalts suggest some affinity to MORB (mid-ocean ridge basalts) or HIMU. Ocean Island Basalt Alkaline Basalt Cenozoic Basalt Silicate Earth Bulk Silicate Vokurka, K. aut Sundvoll, B. aut Enthalten in Mineralogy and petrology Springer-Verlag, 1987 48(1993), 1 vom: März, Seite 35-45 (DE-627)129383856 (DE-600)166036-6 (DE-576)014770881 0930-0708 nnns volume:48 year:1993 number:1 month:03 pages:35-45 https://doi.org/10.1007/BF01164907 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_31 GBV_ILN_40 GBV_ILN_65 GBV_ILN_70 GBV_ILN_2004 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4029 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4306 GBV_ILN_4307 TE 1000 AR 48 1993 1 03 35-45
allfieldsGer	10.1007/BF01164907 doi (DE-627)OLC2062478437 (DE-He213)BF01164907-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn TE 1000 VZ rvk Bendl, J. verfasserin aut Strontium and neodymium isotope study of Bohemian basalts 1993 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1993 Summary The Cenozoic alkaline basalts of northern and western Bohemia are part of the Central European Volcanic Province (CEVP) which extends from the Rhineland (Eifel, Germany) to Moravia (Czechoslovakia) and the Lover Silesia (Poland). Seven samlpes from locations within Czechoslovakia have been analyzed isotopically for the Rb-Sr and the Sm-Nd systems. Present-day, normalised 87Sr/86Sr ratios range from 0.7031 to 0.7036, and the corresponding 143Nd/144Nd ratios range from 0.51279 to 0.51286. An eigth sample from the Silurian basalts of the ‘St. Jan’ type (K-Ar age: 420 Ma) occuring in the Barrandian basin in Central Bohemia is also analysed. Its Present-day, normalised, 87Sr/86Sr ratio is 0.7031, and the corresponding 143Nd/144Nd ratio 0.51288. The Nd ratios of the Cenozoic basalts are similar, but more restricted than those from Germany, but are lower than those from Lower Silesia; a trend which is converse for the Sr ratios. Comparison of the results with the systematics ofZindler andHart (1986), suggests that the mande reservoir source of the Bohemian Cenozoic CEVP basalts is similar to the HIMU (High-μ ocean island basalts), with transition to PUM (primitive upper mantle) or BSE (bulk silicate earth). The reservoir for the Silurian Barrandian basin basalts suggest some affinity to MORB (mid-ocean ridge basalts) or HIMU. Ocean Island Basalt Alkaline Basalt Cenozoic Basalt Silicate Earth Bulk Silicate Vokurka, K. aut Sundvoll, B. aut Enthalten in Mineralogy and petrology Springer-Verlag, 1987 48(1993), 1 vom: März, Seite 35-45 (DE-627)129383856 (DE-600)166036-6 (DE-576)014770881 0930-0708 nnns volume:48 year:1993 number:1 month:03 pages:35-45 https://doi.org/10.1007/BF01164907 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_31 GBV_ILN_40 GBV_ILN_65 GBV_ILN_70 GBV_ILN_2004 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4029 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4306 GBV_ILN_4307 TE 1000 AR 48 1993 1 03 35-45
allfieldsSound	10.1007/BF01164907 doi (DE-627)OLC2062478437 (DE-He213)BF01164907-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn TE 1000 VZ rvk Bendl, J. verfasserin aut Strontium and neodymium isotope study of Bohemian basalts 1993 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1993 Summary The Cenozoic alkaline basalts of northern and western Bohemia are part of the Central European Volcanic Province (CEVP) which extends from the Rhineland (Eifel, Germany) to Moravia (Czechoslovakia) and the Lover Silesia (Poland). Seven samlpes from locations within Czechoslovakia have been analyzed isotopically for the Rb-Sr and the Sm-Nd systems. Present-day, normalised 87Sr/86Sr ratios range from 0.7031 to 0.7036, and the corresponding 143Nd/144Nd ratios range from 0.51279 to 0.51286. An eigth sample from the Silurian basalts of the ‘St. Jan’ type (K-Ar age: 420 Ma) occuring in the Barrandian basin in Central Bohemia is also analysed. Its Present-day, normalised, 87Sr/86Sr ratio is 0.7031, and the corresponding 143Nd/144Nd ratio 0.51288. The Nd ratios of the Cenozoic basalts are similar, but more restricted than those from Germany, but are lower than those from Lower Silesia; a trend which is converse for the Sr ratios. Comparison of the results with the systematics ofZindler andHart (1986), suggests that the mande reservoir source of the Bohemian Cenozoic CEVP basalts is similar to the HIMU (High-μ ocean island basalts), with transition to PUM (primitive upper mantle) or BSE (bulk silicate earth). The reservoir for the Silurian Barrandian basin basalts suggest some affinity to MORB (mid-ocean ridge basalts) or HIMU. Ocean Island Basalt Alkaline Basalt Cenozoic Basalt Silicate Earth Bulk Silicate Vokurka, K. aut Sundvoll, B. aut Enthalten in Mineralogy and petrology Springer-Verlag, 1987 48(1993), 1 vom: März, Seite 35-45 (DE-627)129383856 (DE-600)166036-6 (DE-576)014770881 0930-0708 nnns volume:48 year:1993 number:1 month:03 pages:35-45 https://doi.org/10.1007/BF01164907 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_31 GBV_ILN_40 GBV_ILN_65 GBV_ILN_70 GBV_ILN_2004 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4029 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4306 GBV_ILN_4307 TE 1000 AR 48 1993 1 03 35-45
language	English
source	Enthalten in Mineralogy and petrology 48(1993), 1 vom: März, Seite 35-45 volume:48 year:1993 number:1 month:03 pages:35-45
sourceStr	Enthalten in Mineralogy and petrology 48(1993), 1 vom: März, Seite 35-45 volume:48 year:1993 number:1 month:03 pages:35-45
format_phy_str_mv	Article
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topic_facet	Ocean Island Basalt Alkaline Basalt Cenozoic Basalt Silicate Earth Bulk Silicate
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container_title	Mineralogy and petrology
authorswithroles_txt_mv	Bendl, J. @@aut@@ Vokurka, K. @@aut@@ Sundvoll, B. @@aut@@
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Seven samlpes from locations within Czechoslovakia have been analyzed isotopically for the Rb-Sr and the Sm-Nd systems. Present-day, normalised 87Sr/86Sr ratios range from 0.7031 to 0.7036, and the corresponding 143Nd/144Nd ratios range from 0.51279 to 0.51286. An eigth sample from the Silurian basalts of the ‘St. Jan’ type (K-Ar age: 420 Ma) occuring in the Barrandian basin in Central Bohemia is also analysed. Its Present-day, normalised, 87Sr/86Sr ratio is 0.7031, and the corresponding 143Nd/144Nd ratio 0.51288. The Nd ratios of the Cenozoic basalts are similar, but more restricted than those from Germany, but are lower than those from Lower Silesia; a trend which is converse for the Sr ratios. Comparison of the results with the systematics ofZindler andHart (1986), suggests that the mande reservoir source of the Bohemian Cenozoic CEVP basalts is similar to the HIMU (High-μ ocean island basalts), with transition to PUM (primitive upper mantle) or BSE (bulk silicate earth). 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author	Bendl, J.
spellingShingle	Bendl, J. ddc 550 ssgn 13 rvk TE 1000 misc Ocean Island Basalt misc Alkaline Basalt misc Cenozoic Basalt misc Silicate Earth misc Bulk Silicate Strontium and neodymium isotope study of Bohemian basalts
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topic_title	550 VZ 13 ssgn TE 1000 VZ rvk Strontium and neodymium isotope study of Bohemian basalts Ocean Island Basalt Alkaline Basalt Cenozoic Basalt Silicate Earth Bulk Silicate
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title	Strontium and neodymium isotope study of Bohemian basalts
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title_full	Strontium and neodymium isotope study of Bohemian basalts
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author_browse	Bendl, J. Vokurka, K. Sundvoll, B.
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title_sort	strontium and neodymium isotope study of bohemian basalts
title_auth	Strontium and neodymium isotope study of Bohemian basalts
abstract	Summary The Cenozoic alkaline basalts of northern and western Bohemia are part of the Central European Volcanic Province (CEVP) which extends from the Rhineland (Eifel, Germany) to Moravia (Czechoslovakia) and the Lover Silesia (Poland). Seven samlpes from locations within Czechoslovakia have been analyzed isotopically for the Rb-Sr and the Sm-Nd systems. Present-day, normalised 87Sr/86Sr ratios range from 0.7031 to 0.7036, and the corresponding 143Nd/144Nd ratios range from 0.51279 to 0.51286. An eigth sample from the Silurian basalts of the ‘St. Jan’ type (K-Ar age: 420 Ma) occuring in the Barrandian basin in Central Bohemia is also analysed. Its Present-day, normalised, 87Sr/86Sr ratio is 0.7031, and the corresponding 143Nd/144Nd ratio 0.51288. The Nd ratios of the Cenozoic basalts are similar, but more restricted than those from Germany, but are lower than those from Lower Silesia; a trend which is converse for the Sr ratios. Comparison of the results with the systematics ofZindler andHart (1986), suggests that the mande reservoir source of the Bohemian Cenozoic CEVP basalts is similar to the HIMU (High-μ ocean island basalts), with transition to PUM (primitive upper mantle) or BSE (bulk silicate earth). The reservoir for the Silurian Barrandian basin basalts suggest some affinity to MORB (mid-ocean ridge basalts) or HIMU. © Springer-Verlag 1993
abstractGer	Summary The Cenozoic alkaline basalts of northern and western Bohemia are part of the Central European Volcanic Province (CEVP) which extends from the Rhineland (Eifel, Germany) to Moravia (Czechoslovakia) and the Lover Silesia (Poland). Seven samlpes from locations within Czechoslovakia have been analyzed isotopically for the Rb-Sr and the Sm-Nd systems. Present-day, normalised 87Sr/86Sr ratios range from 0.7031 to 0.7036, and the corresponding 143Nd/144Nd ratios range from 0.51279 to 0.51286. An eigth sample from the Silurian basalts of the ‘St. Jan’ type (K-Ar age: 420 Ma) occuring in the Barrandian basin in Central Bohemia is also analysed. Its Present-day, normalised, 87Sr/86Sr ratio is 0.7031, and the corresponding 143Nd/144Nd ratio 0.51288. The Nd ratios of the Cenozoic basalts are similar, but more restricted than those from Germany, but are lower than those from Lower Silesia; a trend which is converse for the Sr ratios. Comparison of the results with the systematics ofZindler andHart (1986), suggests that the mande reservoir source of the Bohemian Cenozoic CEVP basalts is similar to the HIMU (High-μ ocean island basalts), with transition to PUM (primitive upper mantle) or BSE (bulk silicate earth). The reservoir for the Silurian Barrandian basin basalts suggest some affinity to MORB (mid-ocean ridge basalts) or HIMU. © Springer-Verlag 1993
abstract_unstemmed	Summary The Cenozoic alkaline basalts of northern and western Bohemia are part of the Central European Volcanic Province (CEVP) which extends from the Rhineland (Eifel, Germany) to Moravia (Czechoslovakia) and the Lover Silesia (Poland). Seven samlpes from locations within Czechoslovakia have been analyzed isotopically for the Rb-Sr and the Sm-Nd systems. Present-day, normalised 87Sr/86Sr ratios range from 0.7031 to 0.7036, and the corresponding 143Nd/144Nd ratios range from 0.51279 to 0.51286. An eigth sample from the Silurian basalts of the ‘St. Jan’ type (K-Ar age: 420 Ma) occuring in the Barrandian basin in Central Bohemia is also analysed. Its Present-day, normalised, 87Sr/86Sr ratio is 0.7031, and the corresponding 143Nd/144Nd ratio 0.51288. The Nd ratios of the Cenozoic basalts are similar, but more restricted than those from Germany, but are lower than those from Lower Silesia; a trend which is converse for the Sr ratios. Comparison of the results with the systematics ofZindler andHart (1986), suggests that the mande reservoir source of the Bohemian Cenozoic CEVP basalts is similar to the HIMU (High-μ ocean island basalts), with transition to PUM (primitive upper mantle) or BSE (bulk silicate earth). The reservoir for the Silurian Barrandian basin basalts suggest some affinity to MORB (mid-ocean ridge basalts) or HIMU. © Springer-Verlag 1993
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title_short	Strontium and neodymium isotope study of Bohemian basalts
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