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Remanent magnetism of soil layer is taken as a reference frame for locating hydrocarbon seepage zone.
本文利用土壤剩余磁性作为确定烃类渗漏带的参考系.
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Anisotropy of isothermal remanent magnetism is a recently developed technique for rock fabric study.
等温剩磁各向异性是一种新的磁组构研究方法.
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