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Title: Rock magnetism of the Early Pliocene Trubi Formation at Eraclea Minoa (Sicily)

Journal Article · · Geophysical Research Letters (American Geophysical Union); (USA)

The most important magnetic mineral in the fine-grained marls of the Early Pliocene Trubi formation near Eraclea Minoa is magnetite. Some geothite is also present. The magnetite is of high purity and of primary origin. Hysteresis and low-temperature measurements show that most magnetite grains are single-domain. The presence of superparamagnetic grains is suspected. Multi-domain grains are rare. It is shown that AF demagnetization does not yield correct NRM directions.

OSTI ID:
5981266
Journal Information:
Geophysical Research Letters (American Geophysical Union); (USA), Vol. 17:6; ISSN 0094-8276
Country of Publication:
United States
Language:
English