Dual polarity directions in basaltic-andesitic dykes-reversal record or self-reversed magnetization?
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چکیده
منابع مشابه
Origin of self-reversed thermoremanent magnetization.
The ability of certain magnetic minerals to acquire a remanent magnetization that opposes the direction of the Earth's magnetic field has fascinated rock magnetists since its discovery in 1951. Here, we determine the origin of this phenomenon, which is termed self-reversed thermoremanent magnetization (SR-TRM). We present direct transmission electron microscopy observations of negative exchange...
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ژورنال
عنوان ژورنال: Geophysical Journal International
سال: 2012
ISSN: 0956-540X
DOI: 10.1111/j.1365-246x.2012.05543.x