Abstract
The δD values of molecular hydrogen in soil gases obtained from sites along the Yamasaki fault, one of active faults in Southwest Japan were measured. The SD values were in the range between −770 and −470‰, which suggests that molecular hydrogen is formed by chemical reactions between groundwater and the fresh surface of basement rocks formed by the fault movement. © 1980, GEOCHEMICAL SOCIETY OF JAPAN. All rights reserved.
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CITATION STYLE
APA
Kita, I., Matsuo, S., Wakita, H., & Nakamura, Y. (1980). D/H ratios of H2 in soil gases as an indicator of fault movements. GEOCHEMICAL JOURNAL, 14(6), 317–320. https://doi.org/10.2343/geochemj.14.317
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