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Earth, Planets and Space
Fig. 3 | Earth, Planets and Space

Fig. 3

From: A brief review of single silicate crystal paleointensity: rock-magnetic characteristics, mineralogical backgrounds, methods and applications

Fig. 3

Rock-magnetic measurements of a plagioclase sample from a layered gabbro from the southern part of the Oman ophiolite (Sumail massif; 23.47◦N, 58.19◦E). a Low-temperature measurements. Red circles, blue squares, and green diamonds show thermal demagnetization during zero-field warming (ZFW) for an isothermal remanent magnetization (IRM) imparted in a field of 2.5 T at 10 K after zero-field cooling from 300 K (ZFC remanence), thermal demagnetization during ZFW for a remanence given by field cooling from 300 to 10Kin a field of 2.5 T (FC remanence), and low-temperature demagnetization (LTD) cycle for saturation IRM (SIRM) imparted in a field of 2.5 T at 300 K (RT-SIRM), respectively. b The FORC diagram calculated using a smoothing factor of 3. From Fig. 1 in Sato et al. (2015b)

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