1980
DOI: 10.1029/jb085ib06p03115
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Tectonic relations of carbon dioxide discharges and earthquakes

Abstract: CO2‐rich springs occur worldwide along major zones of seismicity. They are mostly in young orogenic belts, but some are in areas of rifting continental platforms. Analyses of 13C content indicate that much of the CO2 is derived from the mantle and that other important sources are the metamorphism of marine carbonate‐bearing sedimentary rocks and the degradation of organic material. The presence of calc‐silicate minerals, such as pumpellyite in metagraywacke, is evidence of former conversion of carbonate‐bearin… Show more

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Cited by 254 publications
(143 citation statements)
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“…A close relationship is suggested be tween CO2 outgassing and volcanic activities. Similar observations based on the world-wide data were reported by Irwin and Barnes (1980). While they stated that C02-rich hot springs in the world are situated mostly along the circum Pacific orogenic belt, our results in the Tohoku district show that C02 outgassing is only limited to the back-arc region.…”
Section: General Trends In Chemical Compositionssupporting
confidence: 79%
“…A close relationship is suggested be tween CO2 outgassing and volcanic activities. Similar observations based on the world-wide data were reported by Irwin and Barnes (1980). While they stated that C02-rich hot springs in the world are situated mostly along the circum Pacific orogenic belt, our results in the Tohoku district show that C02 outgassing is only limited to the back-arc region.…”
Section: General Trends In Chemical Compositionssupporting
confidence: 79%
“…This is consistent with those found in hydrothermal systems in subduction zones (Urabe et al, 1985;Giggenbach et al, 1993). Note that the distribution of CO 2 discharges generally coincides with major zones of seismicity throughout the world (Irwin and Barnes, 1980). …”
Section: Sampling Site and Analytical Methodssupporting
confidence: 79%
“…Changes in gas emissions from thermal and nonthermal wells and the discharge of odorous or flammable gases from the earth have been prominently reported in accounts ofpreseismic phenomena for well over 100 years (IRWIN and BARNES, 1980;WAKITA, 1982;ZIA, 1984;GoLD and SOTER, 1985;KING, 1986). Among the more spectacular phenomena reported are descriptions of gas jets from dry wells, sand geysers, and large increases of gas effervescing from springs (JIANG and L1, 1981a;L1 et a/., 1985).…”
Section: Dissolved Gas Precursorsmentioning
confidence: 99%