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Magnetic fabric of weakly deformed clay-rich sediments in the Italian peninsula: Relationship with compressional and extensional tectonics

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Magnetic fabric of weakly deformed clay-rich sediments in the Italian peninsula: Relationship with compressional and extensional tectonics (English)

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L. Sagnotti

2

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author name string

M. Mattei

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1

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C. Faccenna

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3

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R. Funiciello

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4

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publication date

March 1997

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published in

Tectonophysics

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volume

271

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issue

1-2

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page(s)

107-122

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cites work

Magnetic susceptibility, petrofabrics and strain

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7 January 2021

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Correlation between magnetic anisotropy and fabric for Devonian shales on the Appalachian Plateau

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Anisotropy of magnetic susceptibility in the Scaglia Rossa pelagic limestone

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Extension in the Tyrrhenian Sea and shortening in the Apennines as result of arc migration driven by sinking of the lithosphere

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Slaty cleavage: incipient occurrences in the deep sea

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Primary and tectonic fabric intensities in mudrocks

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The magnetic fabrics of experimentally deformed artificial clay-water dispersions

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Magnetic fabric analysis of the Plio-Pleistocene clayey units of the Sant'Arcangelo basin, southern Italy

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Magnetic fabric and structural setting of Plio-Pleistocene clayey units in an extensional regime: the Tyrrhenian margin of central Italy

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Dip analysis as a tool for estimating regional kinematics in extensional terranes

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Shallow intrusive directions of sheeted dikes in the Troodos ophiolite: Anisotropy of magnetic susceptibility and structural data

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Identifiers

DOI

10.1016/S0040-1951(96)00244-2

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ADS bibcode

1997Tectp.271..107M

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(Q63646128)

Magnetic fabric of weakly deformed clay-rich sediments in the Italian peninsula: Relationship with compressional and extensional tectonics

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