Identification of latent faults using a radon test
This paper discusses the use of 222Rn concentrations in water of natural springs as a geomorphological method to identify latent faults in low-mid term activity areas. The identification of this type of active fault may be crucial in hazard analysis, structural geomorphology and in landscape evoluti...
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| Published in | Geomorphology (Amsterdam) Vol. 110; no. 1; pp. 11 - 19 |
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| Main Authors | , , , , , , , , , |
| Format | Journal Article Conference Proceeding |
| Language | English |
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Amsterdam
Elsevier B.V
01.09.2009
Elsevier |
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| Abstract | This paper discusses the use of
222Rn concentrations in water of natural springs as a geomorphological method to identify latent faults in low-mid term activity areas. The identification of this type of active fault may be crucial in hazard analysis, structural geomorphology and in landscape evolution analysis. The test used to identify these faults is based on the measuring of
222Rn concentrations in water of springs linked to faults, and comparison with those obtained from springs which, although exactly the same lithological context, are not linked with faults (reference values). If the difference between the measured value and the reference value is positive then an anomaly is identified and that measurement indicates a spring linked to a latent fault. The test was applied and validated in springs linked to faults with a latent behaviour in Cantabria, Northern Spain. These faults have shown an intermittent movement over the last 50,000 years, and have contributed towards landslide processes playing a significant role in landscape evolution of the area. |
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| AbstractList | This paper discusses the use of (2(2(2)Rn concentrations in water of natural springs as a geomorphological method to identify latent faults in low-mid term activity areas. The identification of this type of active fault may be crucial in hazard analysis, structural geomorphology and in landscape evolution analysis. The test used to identify these faults is based on the measuring of (2(2(2)Rn concentrations in water of springs linked to faults, and comparison with those obtained from springs which, although exactly the same lithological context, are not linked with faults (reference values). If the difference between the measured value and the reference value is positive then an anomaly is identified and that measurement indicates a spring linked to a latent fault. The test was applied and validated in springs linked to faults with a latent behaviour in Cantabria, Northern Spain. These faults have shown an intermittent movement over the last 50,000 years, and have contributed towards landslide processes playing a significant role in landscape evolution of the area. This paper discusses the use of super(2) super(2) super(2)Rn concentrations in water of natural springs as a geomorphological method to identify latent faults in low-mid term activity areas. The identification of this type of active fault may be crucial in hazard analysis, structural geomorphology and in landscape evolution analysis. The test used to identify these faults is based on the measuring of super(2) super(2) super(2)Rn concentrations in water of springs linked to faults, and comparison with those obtained from springs which, although exactly the same lithological context, are not linked with faults (reference values). If the difference between the measured value and the reference value is positive then an anomaly is identified and that measurement indicates a spring linked to a latent fault. The test was applied and validated in springs linked to faults with a latent behaviour in Cantabria, Northern Spain. These faults have shown an intermittent movement over the last 50,000 years, and have contributed towards landslide processes playing a significant role in landscape evolution of the area. This paper discusses the use of 222Rn concentrations in water of natural springs as a geomorphological method to identify latent faults in low-mid term activity areas. The identification of this type of active fault may be crucial in hazard analysis, structural geomorphology and in landscape evolution analysis. The test used to identify these faults is based on the measuring of 222Rn concentrations in water of springs linked to faults, and comparison with those obtained from springs which, although exactly the same lithological context, are not linked with faults (reference values). If the difference between the measured value and the reference value is positive then an anomaly is identified and that measurement indicates a spring linked to a latent fault. The test was applied and validated in springs linked to faults with a latent behaviour in Cantabria, Northern Spain. These faults have shown an intermittent movement over the last 50,000 years, and have contributed towards landslide processes playing a significant role in landscape evolution of the area. |
| Author | González-Díez, A. Gómez-Arozamena, J. Díaz de Terán, J.R. Soto, J. Cuesta, J.A. Fernández Maroto, G. Olague, I. Bonachea, J. Martínez-Díaz, J.J. Remondo, J. |
| Author_xml | – sequence: 1 givenname: A. surname: González-Díez fullname: González-Díez, A. email: gonzalea@unican.es organization: DCITIMAC, Facultad de Ciencias, Universidad de Cantabria, Spain – sequence: 2 givenname: J. surname: Soto fullname: Soto, J. organization: Dept. Ciencias Medicas y Quirúrgicas, Física Médica, Facultad de Medicina, Universidad de Cantabria, Spain – sequence: 3 givenname: J. surname: Gómez-Arozamena fullname: Gómez-Arozamena, J. organization: Dept. Ciencias Medicas y Quirúrgicas, Física Médica, Facultad de Medicina, Universidad de Cantabria, Spain – sequence: 4 givenname: J. surname: Bonachea fullname: Bonachea, J. organization: DCITIMAC, Facultad de Ciencias, Universidad de Cantabria, Spain – sequence: 5 givenname: J.J. surname: Martínez-Díaz fullname: Martínez-Díaz, J.J. organization: Dept. de Geodinámica, Facultad de Ciencias Geológicas, Universidad Complutense de Madrid, Spain – sequence: 6 givenname: J.A. surname: Cuesta fullname: Cuesta, J.A. organization: Dept. Matemáticas, Estadística y Computación, Facultad de Ciencias, Universidad de Cantabria, Spain – sequence: 7 givenname: I. surname: Olague fullname: Olague, I. organization: DCITIMAC, Facultad de Ciencias, Universidad de Cantabria, Spain – sequence: 8 givenname: J. surname: Remondo fullname: Remondo, J. organization: DCITIMAC, Facultad de Ciencias, Universidad de Cantabria, Spain – sequence: 9 givenname: G. surname: Fernández Maroto fullname: Fernández Maroto, G. organization: DCITIMAC, Facultad de Ciencias, Universidad de Cantabria, Spain – sequence: 10 givenname: J.R. surname: Díaz de Terán fullname: Díaz de Terán, J.R. organization: DCITIMAC, Facultad de Ciencias, Universidad de Cantabria, Spain |
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| Keywords | Structural geomorphology Radon test Latent faults Methods in Geomorphology Hazard analysis radon springs upper Quaternary epicenters earthquakes spatial distribution Rn-222 hydrochemistry Cenozoic landscapes Quaternary concentration upper Pleistocene active faults landslides Phanerozoic Holocene landform evolution theory Pleistocene |
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222Rn concentrations in water of natural springs as a geomorphological method to identify latent faults in low-mid term... This paper discusses the use of super(2) super(2) super(2)Rn concentrations in water of natural springs as a geomorphological method to identify latent faults... This paper discusses the use of (2(2(2)Rn concentrations in water of natural springs as a geomorphological method to identify latent faults in low-mid term... |
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| SubjectTerms | Earth sciences Earth, ocean, space Exact sciences and technology Geochemistry Hazard analysis Isotope geochemistry Isotope geochemistry. Geochronology Latent faults Marine and continental quaternary Methods in Geomorphology Mineralogy Radon test Silicates Structural geomorphology Surficial geology Water geochemistry |
| Title | Identification of latent faults using a radon test |
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