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Origin of the absarokite–banakite association of the Damavand volcano (Iran): trace elements and Sr,...

Origin of the absarokite–banakite association of the Damavand volcano (Iran): trace elements and Sr,...

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_hal_primary_oai_HAL_hal_00411553v1

Origin of the absarokite–banakite association of the Damavand volcano (Iran): trace elements and Sr, Nd, Pb isotope constraints

About this item

Full title

Origin of the absarokite–banakite association of the Damavand volcano (Iran): trace elements and Sr, Nd, Pb isotope constraints

Publisher

Berlin/Heidelberg: Springer-Verlag

Journal title

International journal of earth sciences : Geologische Rundschau, 2008-02, Vol.97 (1), p.89-102

Language

English

Formats

Publication information

Publisher

Berlin/Heidelberg: Springer-Verlag

More information

Scope and Contents

Contents

The activity of the Damavand volcano (Central Alborz, northern Iran) began 1.8 Ma ago and continued up to 7 ka BP. Although the volcanic suite is clearly of shoshonitic affinity, only two petrographic types can be distinguished in the studied lavas: (1) weakly differentiated absarokites (49 < %SiO
2
 < 51), scattered around the volcano but wi...

Alternative Titles

Full title

Origin of the absarokite–banakite association of the Damavand volcano (Iran): trace elements and Sr, Nd, Pb isotope constraints

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_hal_primary_oai_HAL_hal_00411553v1

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_hal_primary_oai_HAL_hal_00411553v1

Other Identifiers

ISSN

1437-3254

E-ISSN

1437-3262

DOI

10.1007/s00531-006-0159-6

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