Titlebook: Spectroscopy, Luminescence and Radiation Centers in Minerals; Arnold S. Marfunin Book 1979 Springer-Verlag Berlin Heidelberg 1979 Gitterfe

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书目名称Spectroscopy, Luminescence and Radiation Centers in Minerals影响因子(影响力)




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Nuclear Magnetic Resonance (NMR) and Nuclear Quadrupole Resonance (NQR), 61). resulting in the appearance of the NMR signal, are nuclear levels, as in Mössbauer spectroscopy (NGR), but in NMR the transitions take place between sublevels of the ground state arising in the applied magnetic field, whereas in NGR, transitions occur between the ground and excited levels of the nucleus (see Fig. 7).

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Thermoluminescence,ting due to electrons escaping from traps. It was, however, not until after development of the theory of the phenomenon (since 1945) that thermoluminescence has found wide application [591, 664, 713, 732].

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e progress of research methods. Over a space of more than two and half centuries, from the goniometry of the mineral crystals to microscopic petrography and optical mineralogy, to crystal structure determinations, electron micros­ copy and electron diffraction and finally investigations into their e

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Electron Paramagnetic Resonance,ron, i.e., an electron tube, operating within the range of a superhigh-frequency band, and yielding a strictly monochromatic emission with a wavelength in commercially constructed spectrometers equal to 3.2, 1.2, or 0.8 cm. Therefore no monochromator is required here, but a waveguide and resonator,

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