1992
DOI: 10.1063/1.351256
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The magneto-optical Kerr effect of bilayers Fe/Au-Cu and Fe/Ag-Au

Abstract: Articles you may be interested inSeparation of the first-and second-order contributions in magneto-optic Kerr effect magnetometry of epitaxial FeMn/NiFe bilayers made by vacuum evaporation were studied. The magnetooptical polar Kerr rotation and reflectivity spectra were measured in the region from 400 to 700 nm. In the magneto-optical Kerr rotation spectra of bilayers Fe/Au-Cu and Fe/Ag-Au with the thickness of Fe layer less than the light penetration depth, there is a broad enhancement of the magneto-optical… Show more

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Cited by 5 publications
(2 citation statements)
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“…The shape of the Late Mesozoic magmatic rocks is constrained by a series of NE-trending faults and folds. Numerous polymetallic Cu-Au deposits are products of those intermediate-felsic magmatic and relevant hydrothermal activities (Figure 1b) [49]. Ore-bearing intrusions include the DGS, Tongguanshan, Fenghuangshan, Xinqiao, and Shizishan, which mainly consist of intermediate-felsic magmatic rocks, including pyroxene monzodiorite, quartz monzodiorite, and granodiorite [15,50].…”
Section: Geological Backgroundmentioning
confidence: 99%
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“…The shape of the Late Mesozoic magmatic rocks is constrained by a series of NE-trending faults and folds. Numerous polymetallic Cu-Au deposits are products of those intermediate-felsic magmatic and relevant hydrothermal activities (Figure 1b) [49]. Ore-bearing intrusions include the DGS, Tongguanshan, Fenghuangshan, Xinqiao, and Shizishan, which mainly consist of intermediate-felsic magmatic rocks, including pyroxene monzodiorite, quartz monzodiorite, and granodiorite [15,50].…”
Section: Geological Backgroundmentioning
confidence: 99%
“…The DGS quartz monzodiorites have high SiO 2 and Al 2 O 3 contents varying from 63.2 to 67.9 wt% and 14.9 to 16.2 wt%, respectively. They have high Sr (800-991 ppm), low Y (15.2-17.5 ppm) and Yb (1.37-1.52 ppm) concentrations, and resultant high Sr/Y (46)(47)(48)(49)(50)(51)(52)(53)(54)(55)(56)(57)(58)(59)(60)(61) and (La/Yb) N (14.8-18.5) ratios, which are all typical geochemical features of adakites [78]. In the discrimination diagrams (Figure 9), most of the samples fall in or on the boundary of the adakite field.…”
Section: Petrogenesis Of the Dgs Quartz Monzodioritementioning
confidence: 99%