Inverse to normal magnetic fabric transition in an Upper Miocene Marly Sequence from Tuscany, Italy

Geophysical Research Letters

Volumn 23, Issue 9, 1996, Pages 909-912

  Winkler, Aldo ^a   Florindo, Fabio ^a   Sagnotti, Leonardo ^a   Sarti, Giovanni ^b  

^a ISTITUTO NAZIONALE DI GEOFISICA E VULCANOLOGIA   (Italy)

^b UNIVERSITY OF PISA   (Italy)

Author keywords

[No Author keywords available]

Indexed keywords

MAGNETIC SUSCEPTIBILITY; CARBONATES; CLAY; FERRIMAGNETIC MATERIALS; GEOGRAPHICAL REGIONS; IRON; MAGNETIC ANISOTROPY; MAGNETIC PERMEABILITY; SEDIMENTARY ROCKS; SEDIMENTOLOGY; STRATIGRAPHY;

INVERSE SUSCEPTIBILITY; MAGNETIC FABRICS; TUSCANY , ITALY; UPPER MIOCENE;

MAGNETISM; GEOPHYSICS;

MAGNETIC FABRIC; MAGNETIC SUSCEPTIBILITY; MARL; MIOCENE;

ITALY, TUSCANY, MORRA CREEK;

ANHYSTERETIC REMANENCE ANISOTROPY; IRON BEARING CARBONATES; MAGNETIC SUSCEPTIBILITY FABRIC; MIOCENE MARLY SEQUENCE; SEDIMENTOLOGICAL VARIATION;

EID: 0029666559     PISSN: 00948276     EISSN: 19448007     Source Type: Journal    
DOI: 10.1029/96GL00745     Document Type: Article

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