In search of earthquake-related hydrologic and chemical changes along Hayward Fault
Reference (13)
- et al.
Effects of the Arvin-Tehachapi earthquake on spring and stream flow
Geology of the San Jose-Mount Hamilton area, California
California Division of Mines Bull.
(1951)- et al.
San Francisco Bay region fault creep rates measured by theodolite
Gas geochemistry applied to earthquake prediction: an overview
J. Geophys. Res.
(1986)- et al.
Anomalous chemical changes in well waters and possible relation to earthquakes
Geophys. Res. Lett.
(1981) - et al.
The Honeydew earthquake, August 17, 1991
California Geol.
(1992)
Cited by (35)
Fault-controlled springs: A review
2022, Earth-Science ReviewsTesting of <sup>222</sup>Rn application for recognizing tectonic events observed on water-tube tiltmeters in underground Geodynamic Laboratory of Space Research Centre at Książ (the Sudetes, SW Poland)
2020, Applied Radiation and IsotopesCitation Excerpt :Another advantage is its radioactivity, which can be easily detected by physico-chemical methods, such as active methods, e.g. using semiconductor detectors, Lucas chamber and AlphaGUARD (Kozłowska and Kozak, 2006; Przylibski et al., 2010) despite its very small concentration (of the order of 10−16 g/kg of rock) in the upper part of the earth's crust (Conen and Robertson, 2002; Oliveira et al., 2003; Hamada and Miyazaki, 2004; Sakashita et al., 2004; Wu et al., 2004; Brunke et al., 2004; Gupta et al., 2004; Zahorowski et al., 2004; Sesana et al., 2006; Podstawczyńska et al., 2009; Richon et al., 2011; Zafrir et al., 2013). There have been attempts to apply variations in 222Rn activity concentration in soil air, groundwaters or other geofluids (e.g. crude oil, natural gas or CO2 stream) to characterize and predict phenomena such as earthquakes (Steinitz et al., 2003; Fleischer, 1981; Hammond et al., 1981; Fong-Liang and Gui-Ru, 1981; Fong-Liang et al., 1981; Ta-Liang et al., 1981; King, 1984/1985, 1986; Igarashi et al., 1993, 1995; King et al., 1993, 1994, 1996; Virk and Singh, 1993, 1994; Heinicke et al., 1995; Ohno and Wakita, 1996; Al-Hilal et al., 1998; Finkelstein et al., 1998; Fytikas et al., 1999; Castro Morales and LaBrecque, 1999; Heinicke and Koch, 2000; Zmazek et al., 2000, 2005; LaBrecque et al., 2001; Biagi et al., 2001; Planinić et al., 2001, 2004; Virk and Walia, 2001; Tsvetkova et al., 2001; Richon et al., 2003; Huang et al., 2004; Hartmann and Levy, 2005; Choubey et al., 2007, 2009; Crockett et al., 2006; Ghosh et al., 2009; Kuo et al., 2006, 2011; İnan and Seyis, 2010; Crockett and Gillmore, 2010; Yalım et al., 2012; Shi et al., 2013; Negarestani et al., 2014; Petraki et al., 2015), volcanic eruptions (Barillon et al., 1993; Martinelli, 1998; Martinelli et al., 1995; Segovia, 1991; Segovia et al., 1995, 1997; 2001; Connor et al., 1996; Segovia and Mena, 1999; Garcìa et al., 2000; Berlo et al., 2004; Immè et al., 2006), landslide formation (Choubey et al., 2005), mining subsidence (Kies et al., 2004) as well as rock bursts, and gas or rock outbursts in mines (Lebecka et al., 1990; Mnich and Lebecka, 1992; Wysocka, 2010) or to identify active fault zones (Steele, 1981; Toutain and Baubron, 1999; Baubron et al., 2002; Ioannides et al., 2003; Al-Tai et al., 2004; Pizzino et al., 2004; Ramola, 2009; Utkin and Yurkov, 2010) and earth tides (Walia et al., 2003, 2013; Yang et al., 2005; Hartmann, 2005). A wide range of possible applications of radon as a tracer in a variety of processes occurring in the natural environment inspired us to launch joint research.
Experimental evidence on formation of imminent and short-term hydrochemical precursors for earthquakes
2010, Applied GeochemistryStreamflow response to the Nisqually earthquake
2003, Earth and Planetary Science Letters