Eruptive history and age of magmatic processes in the Cǎlimani volcanic structure (Romania)

Ioan Seghedi, Alexandru Szakács, Z. Pécskay, Paul R D Mason

Research output: Contribution to journalArticle

23 Citations (Scopus)

Abstract

The Cǎlimani Mountains represent the largest and most complex volcanic structure at the northern part of the Cǎlimani-Gurghiu-Harghita range in Romania. Sixty-eight K-Ar ages (thirty-three new) provide constraints on the eruptive history of the Cǎlimani volcanic structure between 11.3 and 6.7 Ma. The oldest rocks are from shallow exhumed intrusions, which pierced the basement between 11.3-9.4 Ma. The oldest stratovolcano was centered on the presently recognizable main volcanoes, Rusca-Tihu and the Cǎlimani Caldera and grew very large (ca. 300 km3), generating a large-volume (26 km3) debris avalanche. Debris avalanche blocks dated between 10.2-7.8 Ma, suggest an edifice failure event at 8.0±0.5 Ma. The Drǎgoiasa Formation (9.3-8.4 Ma), Budacu Formation (9.0-8.5 Ma), Lomaş Formation (8.6 Ma), a munber of Peripheral Domes (8.7-7.1 Ma) and Sǎrmaş basalts (8.5-8.3 Ma) were also active before the debris avalanche event. Volcanic activity continued from the Rusca-Tihu Volcano between 8.0-6.9 Ma, generating the "Rusca-Tihu Volcaniclastic Formation". The Cǎlimani Caldera. structure including pre-caldera and post-caldera stages was generated between 7.5-6.7 Ma, with an inferred collapse event at 7.1±0.5 Ma. Monzodioritic-dioritic bodies in the central part of the caldera show ages between 8.8-7.3 Ma, implying several episodes of intrusions. Fractional crystallization was important in the generation of different magma series at lower crustal to shallow crustal depths, where plagioclase was the main crystallizing phase. Crustal assimilation affected most of the analysed samples to some degree through assimilation-fractional-crystallization (AFC) processes. Isotopic enrichment of the most basic rocks suggests that contamination processes affected the source of most parental magmas, except those of the Lomaş Formation. The initial stages of volcanism were most complex from the petrological point of view. The Drǎgoiasa Formation (represented only by felsic rocks), for instance, suggests either fractionation from a basic parental magma and mixing with partial melts of (lower) crustal origin, or represents direct melting of the garnet bearing lower crust. The Lomaş Formation represents the most primitive magma, which reached the surface recording minimal interaction with crustal material and most closely characterizes the isotopic composition of the mantle source beneath the Cǎlimani Volcano. The youngest volcanic rocks represented by the Cǎlimani Caldera structure were derived from magmas that show a lower degree of partial melting and were largely affected by assimilation processes.

Original languageEnglish
Pages (from-to)67-75
Number of pages9
JournalGeologica Carpathica
Volume56
Issue number1
Publication statusPublished - Feb 2005

Fingerprint

caldera
debris avalanche
history
volcano
magma
fractional crystallization
stratovolcano
felsic rock
mantle source
rock
lower crust
dome
partial melting
volcanism
plagioclase
garnet
volcanic rock
isotopic composition
fractionation
melting

Keywords

  • Cǎlimani Mountains
  • Eastern Carpathians
  • K-Ar data
  • Petrology
  • Volcanology

ASJC Scopus subject areas

  • Earth and Planetary Sciences (miscellaneous)

Cite this

Eruptive history and age of magmatic processes in the Cǎlimani volcanic structure (Romania). / Seghedi, Ioan; Szakács, Alexandru; Pécskay, Z.; Mason, Paul R D.

In: Geologica Carpathica, Vol. 56, No. 1, 02.2005, p. 67-75.

Research output: Contribution to journalArticle

Seghedi, Ioan ; Szakács, Alexandru ; Pécskay, Z. ; Mason, Paul R D. / Eruptive history and age of magmatic processes in the Cǎlimani volcanic structure (Romania). In: Geologica Carpathica. 2005 ; Vol. 56, No. 1. pp. 67-75.
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N2 - The Cǎlimani Mountains represent the largest and most complex volcanic structure at the northern part of the Cǎlimani-Gurghiu-Harghita range in Romania. Sixty-eight K-Ar ages (thirty-three new) provide constraints on the eruptive history of the Cǎlimani volcanic structure between 11.3 and 6.7 Ma. The oldest rocks are from shallow exhumed intrusions, which pierced the basement between 11.3-9.4 Ma. The oldest stratovolcano was centered on the presently recognizable main volcanoes, Rusca-Tihu and the Cǎlimani Caldera and grew very large (ca. 300 km3), generating a large-volume (26 km3) debris avalanche. Debris avalanche blocks dated between 10.2-7.8 Ma, suggest an edifice failure event at 8.0±0.5 Ma. The Drǎgoiasa Formation (9.3-8.4 Ma), Budacu Formation (9.0-8.5 Ma), Lomaş Formation (8.6 Ma), a munber of Peripheral Domes (8.7-7.1 Ma) and Sǎrmaş basalts (8.5-8.3 Ma) were also active before the debris avalanche event. Volcanic activity continued from the Rusca-Tihu Volcano between 8.0-6.9 Ma, generating the "Rusca-Tihu Volcaniclastic Formation". The Cǎlimani Caldera. structure including pre-caldera and post-caldera stages was generated between 7.5-6.7 Ma, with an inferred collapse event at 7.1±0.5 Ma. Monzodioritic-dioritic bodies in the central part of the caldera show ages between 8.8-7.3 Ma, implying several episodes of intrusions. Fractional crystallization was important in the generation of different magma series at lower crustal to shallow crustal depths, where plagioclase was the main crystallizing phase. Crustal assimilation affected most of the analysed samples to some degree through assimilation-fractional-crystallization (AFC) processes. Isotopic enrichment of the most basic rocks suggests that contamination processes affected the source of most parental magmas, except those of the Lomaş Formation. The initial stages of volcanism were most complex from the petrological point of view. The Drǎgoiasa Formation (represented only by felsic rocks), for instance, suggests either fractionation from a basic parental magma and mixing with partial melts of (lower) crustal origin, or represents direct melting of the garnet bearing lower crust. The Lomaş Formation represents the most primitive magma, which reached the surface recording minimal interaction with crustal material and most closely characterizes the isotopic composition of the mantle source beneath the Cǎlimani Volcano. The youngest volcanic rocks represented by the Cǎlimani Caldera structure were derived from magmas that show a lower degree of partial melting and were largely affected by assimilation processes.

AB - The Cǎlimani Mountains represent the largest and most complex volcanic structure at the northern part of the Cǎlimani-Gurghiu-Harghita range in Romania. Sixty-eight K-Ar ages (thirty-three new) provide constraints on the eruptive history of the Cǎlimani volcanic structure between 11.3 and 6.7 Ma. The oldest rocks are from shallow exhumed intrusions, which pierced the basement between 11.3-9.4 Ma. The oldest stratovolcano was centered on the presently recognizable main volcanoes, Rusca-Tihu and the Cǎlimani Caldera and grew very large (ca. 300 km3), generating a large-volume (26 km3) debris avalanche. Debris avalanche blocks dated between 10.2-7.8 Ma, suggest an edifice failure event at 8.0±0.5 Ma. The Drǎgoiasa Formation (9.3-8.4 Ma), Budacu Formation (9.0-8.5 Ma), Lomaş Formation (8.6 Ma), a munber of Peripheral Domes (8.7-7.1 Ma) and Sǎrmaş basalts (8.5-8.3 Ma) were also active before the debris avalanche event. Volcanic activity continued from the Rusca-Tihu Volcano between 8.0-6.9 Ma, generating the "Rusca-Tihu Volcaniclastic Formation". The Cǎlimani Caldera. structure including pre-caldera and post-caldera stages was generated between 7.5-6.7 Ma, with an inferred collapse event at 7.1±0.5 Ma. Monzodioritic-dioritic bodies in the central part of the caldera show ages between 8.8-7.3 Ma, implying several episodes of intrusions. Fractional crystallization was important in the generation of different magma series at lower crustal to shallow crustal depths, where plagioclase was the main crystallizing phase. Crustal assimilation affected most of the analysed samples to some degree through assimilation-fractional-crystallization (AFC) processes. Isotopic enrichment of the most basic rocks suggests that contamination processes affected the source of most parental magmas, except those of the Lomaş Formation. The initial stages of volcanism were most complex from the petrological point of view. The Drǎgoiasa Formation (represented only by felsic rocks), for instance, suggests either fractionation from a basic parental magma and mixing with partial melts of (lower) crustal origin, or represents direct melting of the garnet bearing lower crust. The Lomaş Formation represents the most primitive magma, which reached the surface recording minimal interaction with crustal material and most closely characterizes the isotopic composition of the mantle source beneath the Cǎlimani Volcano. The youngest volcanic rocks represented by the Cǎlimani Caldera structure were derived from magmas that show a lower degree of partial melting and were largely affected by assimilation processes.

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