Age and origin of the Böllsteiner Odenwald
Summary The granitoid protoliths of the gneisses of the Böllsteiner Odenwald, a part of the Mid German Crystalline Rise, intruded at 405 ± 3 Ma. This age was obtained by single zircon 207Pb/206Pb evaporation measurements. It is supported by an upper discordia intercept age of 410 ± 11 Ma from single...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Reischmann, T. [verfasserIn] |
|---|
| Format: |
Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2001 |
|---|
| Schlagwörter: |
|---|
| Systematik: |
|
|---|
| Anmerkung: |
© Springer-Verlag Wien 2001 |
|---|
| Übergeordnetes Werk: |
Enthalten in: Mineralogy and petrology - Springer-Verlag, 1987, 72(2001), 1 vom: Juni, Seite 29-44 |
|---|---|
| Übergeordnetes Werk: |
volume:72 ; year:2001 ; number:1 ; month:06 ; pages:29-44 |
| Links: |
|---|
| DOI / URN: |
10.1007/s007100170025 |
|---|
| Katalog-ID: |
OLC206248254X |
|---|
| LEADER | 01000caa a22002652 4500 | ||
|---|---|---|---|
| 001 | OLC206248254X | ||
| 003 | DE-627 | ||
| 005 | 20230502144340.0 | ||
| 007 | tu | ||
| 008 | 200820s2001 xx ||||| 00| ||eng c | ||
| 024 | 7 | |a 10.1007/s007100170025 |2 doi | |
| 035 | |a (DE-627)OLC206248254X | ||
| 035 | |a (DE-He213)s007100170025-p | ||
| 040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
| 041 | |a eng | ||
| 082 | 0 | 4 | |a 550 |q VZ |
| 084 | |a 13 |2 ssgn | ||
| 084 | |a TE 1000 |q VZ |2 rvk | ||
| 100 | 1 | |a Reischmann, T. |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a Age and origin of the Böllsteiner Odenwald |
| 264 | 1 | |c 2001 | |
| 336 | |a Text |b txt |2 rdacontent | ||
| 337 | |a ohne Hilfsmittel zu benutzen |b n |2 rdamedia | ||
| 338 | |a Band |b nc |2 rdacarrier | ||
| 500 | |a © Springer-Verlag Wien 2001 | ||
| 520 | |a Summary The granitoid protoliths of the gneisses of the Böllsteiner Odenwald, a part of the Mid German Crystalline Rise, intruded at 405 ± 3 Ma. This age was obtained by single zircon 207Pb/206Pb evaporation measurements. It is supported by an upper discordia intercept age of 410 ± 11 Ma from single zircon U/Pb data. These granitoids were derived from hybrid magmas according to their geochemical characteristics. Inherited zircon grains with apparent ages of 882 and 1138 Ma further constrain the source heterogeneity. The isotope data with Nd model ages for the granitoid gneisses between 1.3 and 1.7 Ga also underline the involvement of Proterozoic material into the magma sources. Since the geochemical data indicate a subduction zone environment we suggest that the Böllsteiner Odenwald was formed as part of a Silurian/Early Devonian magmatic arc in an active continental margin. The age data imply that the Böllsteiner Odenwald is closely related to the Spessart and Ruhla Crystalline Complexes but not to the Bergsträsser Odenwald. Therefore the Otzberg zone is considered to be a Variscan suture zone. | ||
| 650 | 4 | |a Subduction | |
| 650 | 4 | |a Devonian | |
| 650 | 4 | |a Continental Margin | |
| 650 | 4 | |a Subduction Zone | |
| 650 | 4 | |a Active Continental Margin | |
| 700 | 1 | |a Anthes, G. |4 aut | |
| 700 | 1 | |a Jaeckel, P. |4 aut | |
| 700 | 1 | |a Altenberger, U. |4 aut | |
| 773 | 0 | 8 | |i Enthalten in |t Mineralogy and petrology |d Springer-Verlag, 1987 |g 72(2001), 1 vom: Juni, Seite 29-44 |w (DE-627)129383856 |w (DE-600)166036-6 |w (DE-576)014770881 |x 0930-0708 |7 nnns |
| 773 | 1 | 8 | |g volume:72 |g year:2001 |g number:1 |g month:06 |g pages:29-44 |
| 856 | 4 | 1 | |u https://doi.org/10.1007/s007100170025 |z lizenzpflichtig |3 Volltext |
| 912 | |a GBV_USEFLAG_A | ||
| 912 | |a SYSFLAG_A | ||
| 912 | |a GBV_OLC | ||
| 912 | |a SSG-OLC-GEO | ||
| 912 | |a SSG-OPC-GGO | ||
| 912 | |a GBV_ILN_11 | ||
| 912 | |a GBV_ILN_22 | ||
| 912 | |a GBV_ILN_31 | ||
| 912 | |a GBV_ILN_40 | ||
| 912 | |a GBV_ILN_65 | ||
| 912 | |a GBV_ILN_70 | ||
| 912 | |a GBV_ILN_2004 | ||
| 912 | |a GBV_ILN_2010 | ||
| 912 | |a GBV_ILN_2015 | ||
| 912 | |a GBV_ILN_2027 | ||
| 912 | |a GBV_ILN_2399 | ||
| 912 | |a GBV_ILN_4112 | ||
| 912 | |a GBV_ILN_4125 | ||
| 912 | |a GBV_ILN_4306 | ||
| 936 | r | v | |a TE 1000 |
| 951 | |a AR | ||
| 952 | |d 72 |j 2001 |e 1 |c 06 |h 29-44 | ||
| author_variant |
t r tr g a ga p j pj u a ua |
|---|---|
| matchkey_str |
article:09300708:2001----::gadrgnfhblti |
| hierarchy_sort_str |
2001 |
| publishDate |
2001 |
| allfields |
10.1007/s007100170025 doi (DE-627)OLC206248254X (DE-He213)s007100170025-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn TE 1000 VZ rvk Reischmann, T. verfasserin aut Age and origin of the Böllsteiner Odenwald 2001 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag Wien 2001 Summary The granitoid protoliths of the gneisses of the Böllsteiner Odenwald, a part of the Mid German Crystalline Rise, intruded at 405 ± 3 Ma. This age was obtained by single zircon 207Pb/206Pb evaporation measurements. It is supported by an upper discordia intercept age of 410 ± 11 Ma from single zircon U/Pb data. These granitoids were derived from hybrid magmas according to their geochemical characteristics. Inherited zircon grains with apparent ages of 882 and 1138 Ma further constrain the source heterogeneity. The isotope data with Nd model ages for the granitoid gneisses between 1.3 and 1.7 Ga also underline the involvement of Proterozoic material into the magma sources. Since the geochemical data indicate a subduction zone environment we suggest that the Böllsteiner Odenwald was formed as part of a Silurian/Early Devonian magmatic arc in an active continental margin. The age data imply that the Böllsteiner Odenwald is closely related to the Spessart and Ruhla Crystalline Complexes but not to the Bergsträsser Odenwald. Therefore the Otzberg zone is considered to be a Variscan suture zone. Subduction Devonian Continental Margin Subduction Zone Active Continental Margin Anthes, G. aut Jaeckel, P. aut Altenberger, U. aut Enthalten in Mineralogy and petrology Springer-Verlag, 1987 72(2001), 1 vom: Juni, Seite 29-44 (DE-627)129383856 (DE-600)166036-6 (DE-576)014770881 0930-0708 nnns volume:72 year:2001 number:1 month:06 pages:29-44 https://doi.org/10.1007/s007100170025 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_2010 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_2399 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4306 TE 1000 AR 72 2001 1 06 29-44 |
| spelling |
10.1007/s007100170025 doi (DE-627)OLC206248254X (DE-He213)s007100170025-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn TE 1000 VZ rvk Reischmann, T. verfasserin aut Age and origin of the Böllsteiner Odenwald 2001 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag Wien 2001 Summary The granitoid protoliths of the gneisses of the Böllsteiner Odenwald, a part of the Mid German Crystalline Rise, intruded at 405 ± 3 Ma. This age was obtained by single zircon 207Pb/206Pb evaporation measurements. It is supported by an upper discordia intercept age of 410 ± 11 Ma from single zircon U/Pb data. These granitoids were derived from hybrid magmas according to their geochemical characteristics. Inherited zircon grains with apparent ages of 882 and 1138 Ma further constrain the source heterogeneity. The isotope data with Nd model ages for the granitoid gneisses between 1.3 and 1.7 Ga also underline the involvement of Proterozoic material into the magma sources. Since the geochemical data indicate a subduction zone environment we suggest that the Böllsteiner Odenwald was formed as part of a Silurian/Early Devonian magmatic arc in an active continental margin. The age data imply that the Böllsteiner Odenwald is closely related to the Spessart and Ruhla Crystalline Complexes but not to the Bergsträsser Odenwald. Therefore the Otzberg zone is considered to be a Variscan suture zone. Subduction Devonian Continental Margin Subduction Zone Active Continental Margin Anthes, G. aut Jaeckel, P. aut Altenberger, U. aut Enthalten in Mineralogy and petrology Springer-Verlag, 1987 72(2001), 1 vom: Juni, Seite 29-44 (DE-627)129383856 (DE-600)166036-6 (DE-576)014770881 0930-0708 nnns volume:72 year:2001 number:1 month:06 pages:29-44 https://doi.org/10.1007/s007100170025 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_2010 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_2399 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4306 TE 1000 AR 72 2001 1 06 29-44 |
| allfields_unstemmed |
10.1007/s007100170025 doi (DE-627)OLC206248254X (DE-He213)s007100170025-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn TE 1000 VZ rvk Reischmann, T. verfasserin aut Age and origin of the Böllsteiner Odenwald 2001 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag Wien 2001 Summary The granitoid protoliths of the gneisses of the Böllsteiner Odenwald, a part of the Mid German Crystalline Rise, intruded at 405 ± 3 Ma. This age was obtained by single zircon 207Pb/206Pb evaporation measurements. It is supported by an upper discordia intercept age of 410 ± 11 Ma from single zircon U/Pb data. These granitoids were derived from hybrid magmas according to their geochemical characteristics. Inherited zircon grains with apparent ages of 882 and 1138 Ma further constrain the source heterogeneity. The isotope data with Nd model ages for the granitoid gneisses between 1.3 and 1.7 Ga also underline the involvement of Proterozoic material into the magma sources. Since the geochemical data indicate a subduction zone environment we suggest that the Böllsteiner Odenwald was formed as part of a Silurian/Early Devonian magmatic arc in an active continental margin. The age data imply that the Böllsteiner Odenwald is closely related to the Spessart and Ruhla Crystalline Complexes but not to the Bergsträsser Odenwald. Therefore the Otzberg zone is considered to be a Variscan suture zone. Subduction Devonian Continental Margin Subduction Zone Active Continental Margin Anthes, G. aut Jaeckel, P. aut Altenberger, U. aut Enthalten in Mineralogy and petrology Springer-Verlag, 1987 72(2001), 1 vom: Juni, Seite 29-44 (DE-627)129383856 (DE-600)166036-6 (DE-576)014770881 0930-0708 nnns volume:72 year:2001 number:1 month:06 pages:29-44 https://doi.org/10.1007/s007100170025 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_2010 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_2399 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4306 TE 1000 AR 72 2001 1 06 29-44 |
| allfieldsGer |
10.1007/s007100170025 doi (DE-627)OLC206248254X (DE-He213)s007100170025-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn TE 1000 VZ rvk Reischmann, T. verfasserin aut Age and origin of the Böllsteiner Odenwald 2001 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag Wien 2001 Summary The granitoid protoliths of the gneisses of the Böllsteiner Odenwald, a part of the Mid German Crystalline Rise, intruded at 405 ± 3 Ma. This age was obtained by single zircon 207Pb/206Pb evaporation measurements. It is supported by an upper discordia intercept age of 410 ± 11 Ma from single zircon U/Pb data. These granitoids were derived from hybrid magmas according to their geochemical characteristics. Inherited zircon grains with apparent ages of 882 and 1138 Ma further constrain the source heterogeneity. The isotope data with Nd model ages for the granitoid gneisses between 1.3 and 1.7 Ga also underline the involvement of Proterozoic material into the magma sources. Since the geochemical data indicate a subduction zone environment we suggest that the Böllsteiner Odenwald was formed as part of a Silurian/Early Devonian magmatic arc in an active continental margin. The age data imply that the Böllsteiner Odenwald is closely related to the Spessart and Ruhla Crystalline Complexes but not to the Bergsträsser Odenwald. Therefore the Otzberg zone is considered to be a Variscan suture zone. Subduction Devonian Continental Margin Subduction Zone Active Continental Margin Anthes, G. aut Jaeckel, P. aut Altenberger, U. aut Enthalten in Mineralogy and petrology Springer-Verlag, 1987 72(2001), 1 vom: Juni, Seite 29-44 (DE-627)129383856 (DE-600)166036-6 (DE-576)014770881 0930-0708 nnns volume:72 year:2001 number:1 month:06 pages:29-44 https://doi.org/10.1007/s007100170025 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_2010 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_2399 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4306 TE 1000 AR 72 2001 1 06 29-44 |
| allfieldsSound |
10.1007/s007100170025 doi (DE-627)OLC206248254X (DE-He213)s007100170025-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn TE 1000 VZ rvk Reischmann, T. verfasserin aut Age and origin of the Böllsteiner Odenwald 2001 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag Wien 2001 Summary The granitoid protoliths of the gneisses of the Böllsteiner Odenwald, a part of the Mid German Crystalline Rise, intruded at 405 ± 3 Ma. This age was obtained by single zircon 207Pb/206Pb evaporation measurements. It is supported by an upper discordia intercept age of 410 ± 11 Ma from single zircon U/Pb data. These granitoids were derived from hybrid magmas according to their geochemical characteristics. Inherited zircon grains with apparent ages of 882 and 1138 Ma further constrain the source heterogeneity. The isotope data with Nd model ages for the granitoid gneisses between 1.3 and 1.7 Ga also underline the involvement of Proterozoic material into the magma sources. Since the geochemical data indicate a subduction zone environment we suggest that the Böllsteiner Odenwald was formed as part of a Silurian/Early Devonian magmatic arc in an active continental margin. The age data imply that the Böllsteiner Odenwald is closely related to the Spessart and Ruhla Crystalline Complexes but not to the Bergsträsser Odenwald. Therefore the Otzberg zone is considered to be a Variscan suture zone. Subduction Devonian Continental Margin Subduction Zone Active Continental Margin Anthes, G. aut Jaeckel, P. aut Altenberger, U. aut Enthalten in Mineralogy and petrology Springer-Verlag, 1987 72(2001), 1 vom: Juni, Seite 29-44 (DE-627)129383856 (DE-600)166036-6 (DE-576)014770881 0930-0708 nnns volume:72 year:2001 number:1 month:06 pages:29-44 https://doi.org/10.1007/s007100170025 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_2010 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_2399 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4306 TE 1000 AR 72 2001 1 06 29-44 |
| language |
English |
| source |
Enthalten in Mineralogy and petrology 72(2001), 1 vom: Juni, Seite 29-44 volume:72 year:2001 number:1 month:06 pages:29-44 |
| sourceStr |
Enthalten in Mineralogy and petrology 72(2001), 1 vom: Juni, Seite 29-44 volume:72 year:2001 number:1 month:06 pages:29-44 |
| format_phy_str_mv |
Article |
| institution |
findex.gbv.de |
| topic_facet |
Subduction Devonian Continental Margin Subduction Zone Active Continental Margin |
| dewey-raw |
550 |
| isfreeaccess_bool |
false |
| container_title |
Mineralogy and petrology |
| authorswithroles_txt_mv |
Reischmann, T. @@aut@@ Anthes, G. @@aut@@ Jaeckel, P. @@aut@@ Altenberger, U. @@aut@@ |
| publishDateDaySort_date |
2001-06-01T00:00:00Z |
| hierarchy_top_id |
129383856 |
| dewey-sort |
3550 |
| id |
OLC206248254X |
| language_de |
englisch |
| fullrecord |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">OLC206248254X</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230502144340.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">200820s2001 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s007100170025</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC206248254X</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)s007100170025-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="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">13</subfield><subfield code="2">ssgn</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">TE 1000</subfield><subfield code="q">VZ</subfield><subfield code="2">rvk</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Reischmann, T.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Age and origin of the Böllsteiner Odenwald</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2001</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">© Springer-Verlag Wien 2001</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Summary The granitoid protoliths of the gneisses of the Böllsteiner Odenwald, a part of the Mid German Crystalline Rise, intruded at 405 ± 3 Ma. This age was obtained by single zircon 207Pb/206Pb evaporation measurements. It is supported by an upper discordia intercept age of 410 ± 11 Ma from single zircon U/Pb data. These granitoids were derived from hybrid magmas according to their geochemical characteristics. Inherited zircon grains with apparent ages of 882 and 1138 Ma further constrain the source heterogeneity. The isotope data with Nd model ages for the granitoid gneisses between 1.3 and 1.7 Ga also underline the involvement of Proterozoic material into the magma sources. Since the geochemical data indicate a subduction zone environment we suggest that the Böllsteiner Odenwald was formed as part of a Silurian/Early Devonian magmatic arc in an active continental margin. The age data imply that the Böllsteiner Odenwald is closely related to the Spessart and Ruhla Crystalline Complexes but not to the Bergsträsser Odenwald. Therefore the Otzberg zone is considered to be a Variscan suture zone.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Subduction</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Devonian</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Continental Margin</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Subduction Zone</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Active Continental Margin</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Anthes, G.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Jaeckel, P.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Altenberger, U.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Mineralogy and petrology</subfield><subfield code="d">Springer-Verlag, 1987</subfield><subfield code="g">72(2001), 1 vom: Juni, Seite 29-44</subfield><subfield code="w">(DE-627)129383856</subfield><subfield code="w">(DE-600)166036-6</subfield><subfield code="w">(DE-576)014770881</subfield><subfield code="x">0930-0708</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:72</subfield><subfield code="g">year:2001</subfield><subfield code="g">number:1</subfield><subfield code="g">month:06</subfield><subfield code="g">pages:29-44</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1007/s007100170025</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_11</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_31</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_65</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_2004</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2010</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2015</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2027</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2399</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4112</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4125</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4306</subfield></datafield><datafield tag="936" ind1="r" ind2="v"><subfield code="a">TE 1000</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">72</subfield><subfield code="j">2001</subfield><subfield code="e">1</subfield><subfield code="c">06</subfield><subfield code="h">29-44</subfield></datafield></record></collection>
|
| author |
Reischmann, T. |
| spellingShingle |
Reischmann, T. ddc 550 ssgn 13 rvk TE 1000 misc Subduction misc Devonian misc Continental Margin misc Subduction Zone misc Active Continental Margin Age and origin of the Böllsteiner Odenwald |
| authorStr |
Reischmann, T. |
| ppnlink_with_tag_str_mv |
@@773@@(DE-627)129383856 |
| format |
Article |
| dewey-ones |
550 - Earth sciences |
| delete_txt_mv |
keep |
| author_role |
aut aut aut aut |
| collection |
OLC |
| remote_str |
false |
| illustrated |
Not Illustrated |
| issn |
0930-0708 |
| topic_title |
550 VZ 13 ssgn TE 1000 VZ rvk Age and origin of the Böllsteiner Odenwald Subduction Devonian Continental Margin Subduction Zone Active Continental Margin |
| topic |
ddc 550 ssgn 13 rvk TE 1000 misc Subduction misc Devonian misc Continental Margin misc Subduction Zone misc Active Continental Margin |
| topic_unstemmed |
ddc 550 ssgn 13 rvk TE 1000 misc Subduction misc Devonian misc Continental Margin misc Subduction Zone misc Active Continental Margin |
| topic_browse |
ddc 550 ssgn 13 rvk TE 1000 misc Subduction misc Devonian misc Continental Margin misc Subduction Zone misc Active Continental Margin |
| format_facet |
Aufsätze Gedruckte Aufsätze |
| format_main_str_mv |
Text Zeitschrift/Artikel |
| carriertype_str_mv |
nc |
| hierarchy_parent_title |
Mineralogy and petrology |
| hierarchy_parent_id |
129383856 |
| dewey-tens |
550 - Earth sciences & geology |
| hierarchy_top_title |
Mineralogy and petrology |
| isfreeaccess_txt |
false |
| familylinks_str_mv |
(DE-627)129383856 (DE-600)166036-6 (DE-576)014770881 |
| title |
Age and origin of the Böllsteiner Odenwald |
| ctrlnum |
(DE-627)OLC206248254X (DE-He213)s007100170025-p |
| title_full |
Age and origin of the Böllsteiner Odenwald |
| author_sort |
Reischmann, T. |
| journal |
Mineralogy and petrology |
| journalStr |
Mineralogy and petrology |
| lang_code |
eng |
| isOA_bool |
false |
| dewey-hundreds |
500 - Science |
| recordtype |
marc |
| publishDateSort |
2001 |
| contenttype_str_mv |
txt |
| container_start_page |
29 |
| author_browse |
Reischmann, T. Anthes, G. Jaeckel, P. Altenberger, U. |
| container_volume |
72 |
| class |
550 VZ 13 ssgn TE 1000 VZ rvk |
| format_se |
Aufsätze |
| author-letter |
Reischmann, T. |
| doi_str_mv |
10.1007/s007100170025 |
| dewey-full |
550 |
| title_sort |
age and origin of the böllsteiner odenwald |
| title_auth |
Age and origin of the Böllsteiner Odenwald |
| abstract |
Summary The granitoid protoliths of the gneisses of the Böllsteiner Odenwald, a part of the Mid German Crystalline Rise, intruded at 405 ± 3 Ma. This age was obtained by single zircon 207Pb/206Pb evaporation measurements. It is supported by an upper discordia intercept age of 410 ± 11 Ma from single zircon U/Pb data. These granitoids were derived from hybrid magmas according to their geochemical characteristics. Inherited zircon grains with apparent ages of 882 and 1138 Ma further constrain the source heterogeneity. The isotope data with Nd model ages for the granitoid gneisses between 1.3 and 1.7 Ga also underline the involvement of Proterozoic material into the magma sources. Since the geochemical data indicate a subduction zone environment we suggest that the Böllsteiner Odenwald was formed as part of a Silurian/Early Devonian magmatic arc in an active continental margin. The age data imply that the Böllsteiner Odenwald is closely related to the Spessart and Ruhla Crystalline Complexes but not to the Bergsträsser Odenwald. Therefore the Otzberg zone is considered to be a Variscan suture zone. © Springer-Verlag Wien 2001 |
| abstractGer |
Summary The granitoid protoliths of the gneisses of the Böllsteiner Odenwald, a part of the Mid German Crystalline Rise, intruded at 405 ± 3 Ma. This age was obtained by single zircon 207Pb/206Pb evaporation measurements. It is supported by an upper discordia intercept age of 410 ± 11 Ma from single zircon U/Pb data. These granitoids were derived from hybrid magmas according to their geochemical characteristics. Inherited zircon grains with apparent ages of 882 and 1138 Ma further constrain the source heterogeneity. The isotope data with Nd model ages for the granitoid gneisses between 1.3 and 1.7 Ga also underline the involvement of Proterozoic material into the magma sources. Since the geochemical data indicate a subduction zone environment we suggest that the Böllsteiner Odenwald was formed as part of a Silurian/Early Devonian magmatic arc in an active continental margin. The age data imply that the Böllsteiner Odenwald is closely related to the Spessart and Ruhla Crystalline Complexes but not to the Bergsträsser Odenwald. Therefore the Otzberg zone is considered to be a Variscan suture zone. © Springer-Verlag Wien 2001 |
| abstract_unstemmed |
Summary The granitoid protoliths of the gneisses of the Böllsteiner Odenwald, a part of the Mid German Crystalline Rise, intruded at 405 ± 3 Ma. This age was obtained by single zircon 207Pb/206Pb evaporation measurements. It is supported by an upper discordia intercept age of 410 ± 11 Ma from single zircon U/Pb data. These granitoids were derived from hybrid magmas according to their geochemical characteristics. Inherited zircon grains with apparent ages of 882 and 1138 Ma further constrain the source heterogeneity. The isotope data with Nd model ages for the granitoid gneisses between 1.3 and 1.7 Ga also underline the involvement of Proterozoic material into the magma sources. Since the geochemical data indicate a subduction zone environment we suggest that the Böllsteiner Odenwald was formed as part of a Silurian/Early Devonian magmatic arc in an active continental margin. The age data imply that the Böllsteiner Odenwald is closely related to the Spessart and Ruhla Crystalline Complexes but not to the Bergsträsser Odenwald. Therefore the Otzberg zone is considered to be a Variscan suture zone. © Springer-Verlag Wien 2001 |
| collection_details |
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_2010 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_2399 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4306 |
| container_issue |
1 |
| title_short |
Age and origin of the Böllsteiner Odenwald |
| url |
https://doi.org/10.1007/s007100170025 |
| remote_bool |
false |
| author2 |
Anthes, G. Jaeckel, P. Altenberger, U. |
| author2Str |
Anthes, G. Jaeckel, P. Altenberger, U. |
| ppnlink |
129383856 |
| mediatype_str_mv |
n |
| isOA_txt |
false |
| hochschulschrift_bool |
false |
| doi_str |
10.1007/s007100170025 |
| up_date |
2024-07-03T15:14:06.939Z |
| _version_ |
1803571321311854592 |
| fullrecord_marcxml |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">OLC206248254X</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230502144340.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">200820s2001 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s007100170025</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC206248254X</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)s007100170025-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="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">13</subfield><subfield code="2">ssgn</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">TE 1000</subfield><subfield code="q">VZ</subfield><subfield code="2">rvk</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Reischmann, T.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Age and origin of the Böllsteiner Odenwald</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2001</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">© Springer-Verlag Wien 2001</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Summary The granitoid protoliths of the gneisses of the Böllsteiner Odenwald, a part of the Mid German Crystalline Rise, intruded at 405 ± 3 Ma. This age was obtained by single zircon 207Pb/206Pb evaporation measurements. It is supported by an upper discordia intercept age of 410 ± 11 Ma from single zircon U/Pb data. These granitoids were derived from hybrid magmas according to their geochemical characteristics. Inherited zircon grains with apparent ages of 882 and 1138 Ma further constrain the source heterogeneity. The isotope data with Nd model ages for the granitoid gneisses between 1.3 and 1.7 Ga also underline the involvement of Proterozoic material into the magma sources. Since the geochemical data indicate a subduction zone environment we suggest that the Böllsteiner Odenwald was formed as part of a Silurian/Early Devonian magmatic arc in an active continental margin. The age data imply that the Böllsteiner Odenwald is closely related to the Spessart and Ruhla Crystalline Complexes but not to the Bergsträsser Odenwald. Therefore the Otzberg zone is considered to be a Variscan suture zone.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Subduction</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Devonian</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Continental Margin</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Subduction Zone</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Active Continental Margin</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Anthes, G.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Jaeckel, P.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Altenberger, U.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Mineralogy and petrology</subfield><subfield code="d">Springer-Verlag, 1987</subfield><subfield code="g">72(2001), 1 vom: Juni, Seite 29-44</subfield><subfield code="w">(DE-627)129383856</subfield><subfield code="w">(DE-600)166036-6</subfield><subfield code="w">(DE-576)014770881</subfield><subfield code="x">0930-0708</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:72</subfield><subfield code="g">year:2001</subfield><subfield code="g">number:1</subfield><subfield code="g">month:06</subfield><subfield code="g">pages:29-44</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1007/s007100170025</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_11</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_31</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_65</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_2004</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2010</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2015</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2027</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2399</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4112</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4125</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4306</subfield></datafield><datafield tag="936" ind1="r" ind2="v"><subfield code="a">TE 1000</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">72</subfield><subfield code="j">2001</subfield><subfield code="e">1</subfield><subfield code="c">06</subfield><subfield code="h">29-44</subfield></datafield></record></collection>
|
| score |
7.399932 |