The transition from subduction arc to slab tearing: Evidence from Capraia Island, northern Tyrrhenian Sea

M. Gasparon; G. Rosenbaum; J.R. Wijbrans; P. Manetti

doi:10.1016/j.jog.2008.06.004

The transition from subduction arc to slab tearing: Evidence from Capraia Island, northern Tyrrhenian Sea

M. Gasparon, G. Rosenbaum, J.R. Wijbrans, P. Manetti

Geology and Geochemistry

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

Abstract

The magmatic island of Capraia in the northern Tyrrhenian Sea records late stages in the evolution of a retreating subduction zone following continental accretion. Subduction rollback in the northern Tyrrhenian Sea was accompanied by an eastward migrating magmatic arc that coincided with Capraia at ∼7.7 Ma. This was followed by segmentation of the subducting slab through eastward propagating tear faults. We present high-precision, step-heating

Original language	English
Pages (from-to)	30-38
Journal	Journal of Geodynamics
Issue number	47
DOIs	https://doi.org/10.1016/j.jog.2008.06.004
Publication status	Published - 2009

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title = "The transition from subduction arc to slab tearing: Evidence from Capraia Island, northern Tyrrhenian Sea",

abstract = "The magmatic island of Capraia in the northern Tyrrhenian Sea records late stages in the evolution of a retreating subduction zone following continental accretion. Subduction rollback in the northern Tyrrhenian Sea was accompanied by an eastward migrating magmatic arc that coincided with Capraia at ∼7.7 Ma. This was followed by segmentation of the subducting slab through eastward propagating tear faults. We present high-precision, step-heating",

author = "M. Gasparon and G. Rosenbaum and J.R. Wijbrans and P. Manetti",

year = "2009",

doi = "10.1016/j.jog.2008.06.004",

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journal = "Journal of Geodynamics",

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AU - Gasparon, M.

AU - Rosenbaum, G.

AU - Wijbrans, J.R.

AU - Manetti, P.

PY - 2009

Y1 - 2009

N2 - The magmatic island of Capraia in the northern Tyrrhenian Sea records late stages in the evolution of a retreating subduction zone following continental accretion. Subduction rollback in the northern Tyrrhenian Sea was accompanied by an eastward migrating magmatic arc that coincided with Capraia at ∼7.7 Ma. This was followed by segmentation of the subducting slab through eastward propagating tear faults. We present high-precision, step-heating

AB - The magmatic island of Capraia in the northern Tyrrhenian Sea records late stages in the evolution of a retreating subduction zone following continental accretion. Subduction rollback in the northern Tyrrhenian Sea was accompanied by an eastward migrating magmatic arc that coincided with Capraia at ∼7.7 Ma. This was followed by segmentation of the subducting slab through eastward propagating tear faults. We present high-precision, step-heating

U2 - 10.1016/j.jog.2008.06.004

DO - 10.1016/j.jog.2008.06.004

M3 - Article

SN - 0264-3707

SP - 30

EP - 38

JO - Journal of Geodynamics

JF - Journal of Geodynamics

IS - 47

ER -

The transition from subduction arc to slab tearing: Evidence from Capraia Island, northern Tyrrhenian Sea

Abstract

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