40Ar/39Ar laserprobe direct dating of discrete deformational events: continuous record of Early Alpine tectonics in the Pelagonian Zone, NW Aegean area, Greece.

A.W.L. Lips; J.R. Wijbrans; S.H. White

doi:10.1016/S0040-1951(98)00181-4

40Ar/39Ar laserprobe direct dating of discrete deformational events: continuous record of Early Alpine tectonics in the Pelagonian Zone, NW Aegean area, Greece.

A.W.L. Lips, J.R. Wijbrans, S.H. White

Research output: Contribution to Journal › Article › Academic

Abstract

The Pelagonian Zone of the Hellenides, which occurs in the northwestern Aegean region of the Eastern Mediterranean, contains remnants of a high-pressure metamorphic belt which subsequently underwent localized reworking during low-temperature deformational events. Formation of Alpine deformational structures in the Ossa Massif (northern Pelagonian Zone) occurred at metamorphic temperatures which failed to reset most pre-Alpine

Original language	English
Pages (from-to)	133-153
Journal	Tectonophysics
Volume	298
DOIs	https://doi.org/10.1016/S0040-1951(98)00181-4
Publication status	Published - 1998

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10.1016/S0040-1951(98)00181-4

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title = "40Ar/39Ar laserprobe direct dating of discrete deformational events: continuous record of Early Alpine tectonics in the Pelagonian Zone, NW Aegean area, Greece.",

abstract = "The Pelagonian Zone of the Hellenides, which occurs in the northwestern Aegean region of the Eastern Mediterranean, contains remnants of a high-pressure metamorphic belt which subsequently underwent localized reworking during low-temperature deformational events. Formation of Alpine deformational structures in the Ossa Massif (northern Pelagonian Zone) occurred at metamorphic temperatures which failed to reset most pre-Alpine",

author = "A.W.L. Lips and J.R. Wijbrans and S.H. White",

year = "1998",

doi = "10.1016/S0040-1951(98)00181-4",

language = "English",

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pages = "133--153",

journal = "Tectonophysics",

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AU - Lips, A.W.L.

AU - Wijbrans, J.R.

AU - White, S.H.

PY - 1998

Y1 - 1998

N2 - The Pelagonian Zone of the Hellenides, which occurs in the northwestern Aegean region of the Eastern Mediterranean, contains remnants of a high-pressure metamorphic belt which subsequently underwent localized reworking during low-temperature deformational events. Formation of Alpine deformational structures in the Ossa Massif (northern Pelagonian Zone) occurred at metamorphic temperatures which failed to reset most pre-Alpine

AB - The Pelagonian Zone of the Hellenides, which occurs in the northwestern Aegean region of the Eastern Mediterranean, contains remnants of a high-pressure metamorphic belt which subsequently underwent localized reworking during low-temperature deformational events. Formation of Alpine deformational structures in the Ossa Massif (northern Pelagonian Zone) occurred at metamorphic temperatures which failed to reset most pre-Alpine

U2 - 10.1016/S0040-1951(98)00181-4

DO - 10.1016/S0040-1951(98)00181-4

M3 - Article

SN - 0040-1951

VL - 298

SP - 133

EP - 153

JO - Tectonophysics

JF - Tectonophysics

ER -

40Ar/39Ar laserprobe direct dating of discrete deformational events: continuous record of Early Alpine tectonics in the Pelagonian Zone, NW Aegean area, Greece.

Abstract

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