Intra-Grain Sr Isotope Evidence for Crystal Recycling and Multiple Magma Reservoirs in the Recent Activity of Stromboli Volcano, Southern Italy

L. Francalanci; G.R. Davies; W. Lustenhouwer; S. Tommasini; P.R.D. Mason; S. Conticelli

doi:10.1093/petrology/egi045

Intra-Grain Sr Isotope Evidence for Crystal Recycling and Multiple Magma Reservoirs in the Recent Activity of Stromboli Volcano, Southern Italy

L. Francalanci, G.R. Davies, W. Lustenhouwer, S. Tommasini, P.R.D. Mason, S. Conticelli

Research output: Contribution to Journal › Article › Academic › peer-review

188 Downloads (Pure)

Abstract

Over the last several hundred years, Stromboli has been characterized by steady-state Strombolian activity. The volcanic products are dominated by degassed and highly porphyritic (HP-magma) black scoria bombs, lapilli and lava flows of basaltic shoshonitic composition. Periodically (about one to three events per year), more energetic explosive eruptions also eject light coloured volatile-rich pumices with low phenocryst content (LP-magma) that have more mafic compositions than the HP-magma. An in situ major and trace element and Sr isotope microanalysis study is presented on four samples chosen to characterize the different modes of activity at Stromboli: a lava flow (1985-1986 effusive event), a scoria bomb from the 'normal' present-day activity of Stromboli (April 1984), and a scoria and coeval pumice sample from a recent more explosive eruption (September 1996). Plagioclase (An

Original language	English
Pages (from-to)	1997-2021
Journal	Journal of Petrology
Volume	46
DOIs	https://doi.org/10.1093/petrology/egi045
Publication status	Published - 2005

Access to Document

10.1093/petrology/egi045

180397Final published version, 1.45 MB

Persistent URL (handle)

Copy link address

Cite this

@article{21e0bd2fc4384b339eb6040b8cf1d054,

title = "Intra-Grain Sr Isotope Evidence for Crystal Recycling and Multiple Magma Reservoirs in the Recent Activity of Stromboli Volcano, Southern Italy",

abstract = "Over the last several hundred years, Stromboli has been characterized by steady-state Strombolian activity. The volcanic products are dominated by degassed and highly porphyritic (HP-magma) black scoria bombs, lapilli and lava flows of basaltic shoshonitic composition. Periodically (about one to three events per year), more energetic explosive eruptions also eject light coloured volatile-rich pumices with low phenocryst content (LP-magma) that have more mafic compositions than the HP-magma. An in situ major and trace element and Sr isotope microanalysis study is presented on four samples chosen to characterize the different modes of activity at Stromboli: a lava flow (1985-1986 effusive event), a scoria bomb from the 'normal' present-day activity of Stromboli (April 1984), and a scoria and coeval pumice sample from a recent more explosive eruption (September 1996). Plagioclase (An",

author = "L. Francalanci and G.R. Davies and W. Lustenhouwer and S. Tommasini and P.R.D. Mason and S. Conticelli",

year = "2005",

doi = "10.1093/petrology/egi045",

language = "English",

volume = "46",

pages = "1997--2021",

journal = "Journal of Petrology",

issn = "0022-3530",

publisher = "Oxford University Press",

}

TY - JOUR

T1 - Intra-Grain Sr Isotope Evidence for Crystal Recycling and Multiple Magma Reservoirs in the Recent Activity of Stromboli Volcano, Southern Italy

AU - Francalanci, L.

AU - Davies, G.R.

AU - Lustenhouwer, W.

AU - Tommasini, S.

AU - Mason, P.R.D.

AU - Conticelli, S.

PY - 2005

Y1 - 2005

N2 - Over the last several hundred years, Stromboli has been characterized by steady-state Strombolian activity. The volcanic products are dominated by degassed and highly porphyritic (HP-magma) black scoria bombs, lapilli and lava flows of basaltic shoshonitic composition. Periodically (about one to three events per year), more energetic explosive eruptions also eject light coloured volatile-rich pumices with low phenocryst content (LP-magma) that have more mafic compositions than the HP-magma. An in situ major and trace element and Sr isotope microanalysis study is presented on four samples chosen to characterize the different modes of activity at Stromboli: a lava flow (1985-1986 effusive event), a scoria bomb from the 'normal' present-day activity of Stromboli (April 1984), and a scoria and coeval pumice sample from a recent more explosive eruption (September 1996). Plagioclase (An

AB - Over the last several hundred years, Stromboli has been characterized by steady-state Strombolian activity. The volcanic products are dominated by degassed and highly porphyritic (HP-magma) black scoria bombs, lapilli and lava flows of basaltic shoshonitic composition. Periodically (about one to three events per year), more energetic explosive eruptions also eject light coloured volatile-rich pumices with low phenocryst content (LP-magma) that have more mafic compositions than the HP-magma. An in situ major and trace element and Sr isotope microanalysis study is presented on four samples chosen to characterize the different modes of activity at Stromboli: a lava flow (1985-1986 effusive event), a scoria bomb from the 'normal' present-day activity of Stromboli (April 1984), and a scoria and coeval pumice sample from a recent more explosive eruption (September 1996). Plagioclase (An

U2 - 10.1093/petrology/egi045

DO - 10.1093/petrology/egi045

M3 - Article

SN - 0022-3530

VL - 46

SP - 1997

EP - 2021

JO - Journal of Petrology

JF - Journal of Petrology

ER -

Intra-Grain Sr Isotope Evidence for Crystal Recycling and Multiple Magma Reservoirs in the Recent Activity of Stromboli Volcano, Southern Italy

Abstract

Access to Document

Persistent URL (handle)

Fingerprint

Cite this