A study of the self-reversal process of rhyodacites from Haruna volcano, Japan and those from the 1991 Pinatubo eruption, Philippines

In: Contributions to Geophysics and Geodesy, vol. 41, no. 1

Oto Orlický

Detaily:

Rok, strany: 2011, 73 - 93

Kľúčové slová:

The Fe-Ti ferrimagnetic-antiferromagnetic phase, the sole carrier of the self-reversed remanent magnetization in the Haruna and Pinatubo rhyodacites

Full text

O článku:

The results of the study of young rhyodacites (erupted in 1400 year) from the Haruna area (Japan) and from the 1991 Pinatubo eruption (Philippines) are presented. The experimental works have proven that the Fe-Ti ferrimagnetic-antiferromagnetic phase is the carrier of the self-reversed remanent magnetization in these rocks. The theoretical solution of this problem has been outlined, but has not yet been accomplished.

Ako citovať:

ISO 690:

Orlický, O. 2011. A study of the self-reversal process of rhyodacites from Haruna volcano, Japan and those from the 1991 Pinatubo eruption, Philippines. In Contributions to Geophysics and Geodesy, vol. 41, no.1, pp. 73-93. 1338-0540.

APA:

Orlický, O. (2011). A study of the self-reversal process of rhyodacites from Haruna volcano, Japan and those from the 1991 Pinatubo eruption, Philippines. Contributions to Geophysics and Geodesy, 41(1), 73-93. 1338-0540.