Recurrent Cenozoic volcanic activity in the Bohemian Massif
(Czech Republic)

J 2011

Recurrent Cenozoic volcanic activity in the Bohemian Massif (Czech Republic)

ULRYCH, Jaromír, Jaroslav DOSTAL, Jiří ADAMOVIČ, Emil JELÍNEK, Petr ŠPAČEK et. al.

Basic information

Original name

Recurrent Cenozoic volcanic activity in the Bohemian Massif (Czech Republic)

Authors

ULRYCH, Jaromír (203 Czech Republic), Jaroslav DOSTAL (124 Canada), Jiří ADAMOVIČ (203 Czech Republic), Emil JELÍNEK (203 Czech Republic), Petr ŠPAČEK (203 Czech Republic, guarantor, belonging to the institution), Ernst HEGNER (276 Germany) and Kadosa BALOGH (348 Hungary)

Edition

Lithos, 2011, 0024-4937

Other information

Language

English

Type of outcome

Článek v odborném periodiku

Field of Study

10500 1.5. Earth and related environmental sciences

Country of publisher

Netherlands

Confidentiality degree

není předmětem státního či obchodního tajemství

Impact factor

Impact factor: 3.246

RIV identification code

RIV/00216224:14310/11:00056501

Organization unit

Faculty of Science

DOI

http://dx.doi.org/10.1016/j.lithos.2010.12.008

UT WoS

000289335800010

Keywords in English

Bohemian Massif; Cenozoic; Alkaline volcanism; Paleostress fields; Rift Mantle

Abstract

V originále

Cenozoic anorogenic volcanism of the Bohemian Massif is an integral part of the Central European Volcanic Province. The temporal and spatial distribution of volcanic rocks in the Bohemian Massif, their geochemistry and mineralogy as well as their tectonic setting and paleostress data are used to characterize and classify this volcanic activity. Three main volcanic periods can be distinguished based on K–Ar data and known paleostress fields: (i) pre-rift (79–49 Ma), (ii) syn-rift (42–16 Ma) and (iii) late-rift (16–0.3 Ma), with the youngest period further subdivided into three episodes. The dominant mafic rock types (N7 wt.% MgO) of all periods are of nephelinite–basanite/tephrite composition. The exceptions are suites of melilitic ultramafic rocks of the pre-rift period in northern Bohemia and of the final episode of the late-rift period in western Bohemia. The most voluminous are volcanic rocks of the syn-rift period occurring in the Ohře Rift Graben. The initial 87Sr/86Sr (0.7032 to 0.7050) and 143Nd/144Nd (0.51264 to 0.51301) ratios of the mafic volcanic rocks of the Bohemian Massif are characteristic of magmas derived from a sub-lithospheric mantle source. The isotopic ratios resemble those of the HIMU mantle source (206Pb/204Pb ca. 19 to 20). These rocks have themost isotopically depleted compositions among the Central European Volcanic Province volcanics.

Citovat

ULRYCH, Jaromír, Jaroslav DOSTAL, Jiří ADAMOVIČ, Emil JELÍNEK, Petr ŠPAČEK, Ernst HEGNER and Kadosa BALOGH. Recurrent Cenozoic volcanic activity in the Bohemian Massif (Czech Republic). Lithos. 2011, vol. 123, 1-4, p. 133-144. ISSN 0024-4937. Available from: https://dx.doi.org/10.1016/j.lithos.2010.12.008.

@article{977052,
   author = {Ulrych, Jaromír and Dostal, Jaroslav and Adamovič, Jiří and Jelínek, Emil and Špaček, Petr and Hegner, Ernst and Balogh, Kadosa},
   article_number = {1-4},
   doi = {http://dx.doi.org/10.1016/j.lithos.2010.12.008},
   keywords = {Bohemian Massif; Cenozoic; Alkaline volcanism; Paleostress fields; Rift Mantle},
   language = {eng},
   issn = {0024-4937},
   journal = {Lithos},
   title = {Recurrent Cenozoic volcanic activity in the Bohemian Massif (Czech Republic)},
   volume = {123},
   year = {2011}
}

TY  - JOUR
ID  - 977052
AU  - Ulrych, Jaromír - Dostal, Jaroslav - Adamovič, Jiří - Jelínek, Emil - Špaček, Petr - Hegner, Ernst - Balogh, Kadosa
PY  - 2011
TI  - Recurrent Cenozoic volcanic activity in the Bohemian Massif (Czech Republic)
JF  - Lithos
VL  - 123
IS  - 1-4
SP  - 133-144
EP  - 133-144
SN  - 00244937
KW  - Bohemian Massif
KW  - Cenozoic
KW  - Alkaline volcanism
KW  - Paleostress fields
KW  - Rift Mantle
N2  - Cenozoic anorogenic volcanism of the Bohemian Massif is an integral part of the Central European Volcanic Province. The temporal and spatial distribution of volcanic rocks in the Bohemian Massif, their geochemistry and mineralogy as well as their tectonic setting and paleostress data are used to characterize and classify this volcanic activity. Three main volcanic periods can be distinguished based on K–Ar data and known paleostress fields: (i) pre-rift (79–49 Ma), (ii) syn-rift (42–16 Ma) and (iii) late-rift (16–0.3 Ma), with the youngest period further subdivided into three episodes. The dominant mafic rock types (N7 wt.% MgO) of all periods are of nephelinite–basanite/tephrite composition. The exceptions are suites of melilitic ultramafic rocks of the pre-rift period in northern Bohemia and of the final episode of the late-rift period in western Bohemia. The most voluminous are volcanic rocks of the syn-rift period occurring in the Ohře Rift Graben. The initial 87Sr/86Sr (0.7032 to 0.7050) and 143Nd/144Nd (0.51264 to 0.51301) ratios of the mafic volcanic rocks of the Bohemian Massif are characteristic of magmas derived from a sub-lithospheric mantle source. The isotopic ratios resemble those of the HIMU mantle source (206Pb/204Pb ca. 19 to 20). These rocks have themost isotopically depleted compositions among the Central European Volcanic Province volcanics.
ER  -

ULRYCH, Jaromír, Jaroslav DOSTAL, Jiří ADAMOVIČ, Emil JELÍNEK, Petr ŠPAČEK, Ernst HEGNER and Kadosa BALOGH. Recurrent Cenozoic volcanic activity in the Bohemian Massif (Czech Republic). \textit{Lithos}. 2011, vol.~123, 1-4, p.~133-144. ISSN~0024-4937. Available from: https://dx.doi.org/10.1016/j.lithos.2010.12.008.

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