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ESR studies of E ' centres in geological flint

机译:E'地质fl石中心的ESR研究

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Properties of E' centres of high geological age in flint from different locations have been studied. ESR spectra of gamma -irradiated samples of heated and unheated Silurian and Eocene flint show thermally unstable components. The spectrum of one species could be simulated using the g values: 2.00164, 2.00059, and 2.00046, Two others deliver ESR-signals at g = 2.0015 and 2.0012, respectively. These unstable components cannot be identified with any known E' centres. About 50% of the ESR intensity of the E' centres in unheated flint induced by artificial gamma -rays is thermally stable. This effect is probably due to a steady state and might be useful for dating of unburned flint tools ("skinflint dating"). (C) 2001 Elsevier Science Ltd. All rights reserved. [References: 17]
机译:已经研究了来自不同地点的火石中E'高地质年龄中心的特性。加热和未加热志留纪和始新世火石的伽马射线辐照样品的ESR光谱显示出热不稳定成分。可以使用g值2.00164、2.00059和2.00046来模拟一种物种的光谱,另外两种在g = 2.0015和2.0012处传递ESR信号。这些不稳定的成分无法通过任何已知的E'中心进行识别。在人造伽马射线诱发的未加热的火石中,E'中心的ESR强度的大约50%是热稳定的。此效果可能是由于处于稳定状态,并且可能对未燃烧的火石工具的约会(“ skinflint约会”)有用。 (C)2001 Elsevier ScienceLtd。保留所有权利。 [参考:17]

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