Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/7237
DC FieldValueLanguage
dc.contributor.authorallDe Paola, N.; Rock Mechanics Laboratory, Earth Sciences Department, University of Durham, South Road, DH1 3LE Durham, UKen
dc.contributor.authorallChiodini, G.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.authorallHirose, T.; Kochi Institute for Core Sample Research, Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Japanen
dc.contributor.authorallCardellini, C.; Dipartimento di Scienze della Terra, Università di Perugia, Piazza Università, 06123 Perugia, Italyen
dc.contributor.authorallCaliro, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.authorallShimamoto, T.; Institute of Geology, China Earthquake Administration, Beijing, Chinaen
dc.date.accessioned2011-12-20T13:05:05Zen
dc.date.available2011-12-20T13:05:05Zen
dc.date.issued2011en
dc.identifier.urihttp://hdl.handle.net/2122/7237en
dc.description.abstractFriction laboratory experiments have been performed at sub-seismic (≈ 0.01 m/s) to seismic slip rates (N1 m/s) on dolomite gouges of the Triassic evaporites, which hosted the five mainshocks (5bMw b6) of the 1997 Colfiorito earthquakes in the Northern Apennines (Italy). Experimental faults are lubricated as marked falls of the steady state sliding friction coefficients, μss≈0.2, are observed at seismic slip rates, as opposed to values of μss≥0.6 attained for sub-seismic slip rates. At seismic slip rates decarbonation reactions, triggered by frictional heating in the experimental slip zone, produced: 1) new fluid (CO2) and mineral phases (e.g. Mg-calcite, periclase/brucite, lime/portlandite); 2) isotopic fractionation between the reaction products and the reactant mineral phases. The variations of total dissolved inorganic carbon (TIDC) in concentration Δ(TDIC) and isotopic composition Δ(δ13CTIDC) in a carbonate aquifer, with geochemical parameters similar to those of an aquifer located in the seismic belt of the Northern Apennines, have been modelled after an input of earthquake-produced CO2. Modelling results show that variation in Δ(δ13CTIDC) can be detected in volumes of groundwater which are about three times larger than those calculated for the variations in Δ(TDIC). For amounts of CO2 produced by coseismic decarbonation of ≤5 wt.% of the slip zone gouge, modelling results show that a detectable geochemical anomaly is obtained if the produced CO2 is dissolved into volumes of water comparable to those of the shallower aquifers feeding the springs in the 1997 Colfiorito earthquakes area. We conclude that the integration of results from laboratory experiments, performed at seismic condition, and geochemical analyses can potentially aid in the calibration of monitoring strategies of geochemical properties of water in seismically active areas and provide insights into seismic fault zone processes (e.g. constraints on the temperature rise during earthquake propagation).en
dc.language.isoEnglishen
dc.publisher.nameElsevieren
dc.relation.ispartofEarth and Planetary Science Lettersen
dc.relation.ispartofseries/310 (2011)en
dc.subjectearthquakesen
dc.subjectfrictionen
dc.subjectisotopesen
dc.titleThe geochemical signature caused by earthquake propagation in carbonate-hosted faultsen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber225-232en
dc.subject.INGV04. Solid Earth::04.06. Seismology::04.06.01. Earthquake faults: properties and evolutionen
dc.subject.INGV04. Solid Earth::04.06. Seismology::04.06.10. Instruments and techniquesen
dc.identifier.doi10.1016/j.epsl.2011.09.001en
dc.relation.referencesBoni, C., Petitta, M., 2008. Redazione informatizzata della cartografia idrogeologica tematica del territorio della Regione Umbria. Final Report of “Contratto di ricerca Regione Umbria - Giunta Regionale Direzione Regionale Ambiente, Territorio e Infrastrutture Servizi tecnici Regionali-Dipartimento di Scienze della Terra Università di Roma, La Sapienza", p. 128. Boni, C., Bono, P., Capelli, G., 1986. Schema idrogeologico dell'Italia centrale. Mem. Soc. Geol. It. 35, 991–1012. Bottinga, Y., 1968. Calculation of fractionation factors for carbon and oxygen isotopic exchange in system calcite-carbon dioxide-water. J. Phys. Chem. Us 72, 800. Boullier, A.M., Fujimoto, K.,Ohtani, T., Roman-Ross, G., Lewin, E., Ito, H., Pezard, P., Ildefonse, B., 2004. Textural evidence for recent co-seismic circulation of fluids in the Nojima fault zone, Awaji island, Japan. Tectonophysics 378, 165–181.Chiaraluce, L., Barchi,M., Collettini, C., Mirabella, F., Pucci, S., 2005. Connecting seismically active normal faults with Quaternary geological structures in a complex extensional environment: the Colfiorito 1997 case history (northern Apennines, Italy). Tectonics 24, TC1002. doi:10.1029/2004TC001627. Chiodini, G., Frondini, F., Cardellini, C., Parello, F., Peruzzi, L., 2000. Rate of diffuse carbon dioxide Earth degassing estimated from carbon balance of regional aquifers: the case of central Apennine, Italy. J. Geophys. Res. Earth Surf. 105, 8423–8434. Chiodini, G., Cardellini, C., Amato, A., Boschi, E., Caliro, S., Frondini, F., Ventura, G., 2004. Carbon dioxide Earth degassing and seismogenesis in central and southern Italy. Geophys. Res. Lett. 31, L07615. doi:10.1029/2004GL019480. Chiodini, G., Caliro, S., Cardellini, C., Frondini, F., Inguaggiato, S., Matteucci, F., 2011. Geochemical evidence for and characterization of CO2 rich gas sources in the epicentral area of the Abruzzo 2009 earthquakes. Earth Planet. Sci. Lett. 304, 389–398. Collettini, C., De Paola, N., Faulkner, D.R., 2009. Insights on the geometry and mechanics of the Umbria-Marche earthquakes (Central Italy) from the integration of field and laboratory data. Tectonophysics 476, 99–109. De Paola, N., Collettini, C., Faulkner, D.R., Trippetta, F., 2008. Fault zone architecture and deformation processes within evaporitic rocks in the upper crust. Tectonics 27, TC4017. doi:10.1029/2007TC002230. De Paola, N.,Hirose, T., Mitchell, T., Di Toro,G., Viti, C., Shimamoto, T., 2011. Fault lubrication and earthquake propagation in thermally unstable rocks. Geology 39, 35–38. Dresen, G., 1991. Stress-distribution and the orientation of Riedel shears. Tectonophysics 188 (3–4), 239–247. Famin, V., Nakashima, S., Boullier, A.M., Fujimoto, K., Hirono, T., 2008. Earthquakes produce carbon dioxide in crustal faults. Earth Planet. Sci. Lett. 265, 487–497. Gu, Y.J., Wong, T.F., 1994. Development of shear localization in simulated quartz gouge—effect of cumulative slip and gouge particle-size. Pure Appl. Geophys. 143 (1–3), 387–423. Han, R., Shimamoto, T., Hirose, T., Ree, J.H., Ando, J., 2007. Ultralow friction of carbonate faults caused by thermal decomposition. Science 316, 878–881. Hirono, T., Yokoyama, T., Hamada, Y., Tanikawa, W., Mishima, T., Ikehara, M., Famin, V., Tanimizu, M., Lin,W., Soh,W., Song, S.R., 2007. A chemical kinetic approach to estimate dynamic shear stress during the 1999 Taiwan Chi-Chi earthquake. Geophys. Res. Lett. 34, L16303. doi:10.1029/2008GL034476. Hirose, T., Shimamoto, T., 2005. Slip-weakening distance of faults during frictional melting as inferred from experimental and natural pseudotachylytes. Bull. Seismol. Soc. Am. 95, 1666–1673. Ishikawa, T., Tanimizu, M., Nagaishi, K., Matsuoka, J., Tadai, O., Sakaguchi,M., Hirono, T., Mishima, T., Tanikawa,W., Lin,W.,Kikuta, H., Soh,W., Song, S.R., 2008. Coseismic fluid-rock interactions at high temperatures in the Chelungpu fault. Nat. Geosci. 1, 679–683. Logan, J., Dengo, C., Higgs, N., Wang, Z., 1992. Fabrics of experimental fault zones: their development and relationship to mechanical behaviour. In: Evans, B., Wong, T.-F. (Eds.), Fault Mechanics and Transport Properties of Rocks. : International Geophysics Series, vol. 51. Academic Press Ltd., London, pp. 33–67. Mastrolillo, L., Baldoni, T., Banzato, F., Boscherini, A., Cascone, D., Checcucci, R., Petitta, M., Boni, C., 2009. Quantitative hydrogeological analysis of the carbonate domain of the Umbria region (Central Italy). Ital. J. Eng. Geol. Environ. 1, 137–155. Miller, S.A., Collettini, C., Chiaraluce, L., Cocco, M., Barchi, M., Kaus, B.J.P., 2004. Aftershocks driven by a high-pressure CO2 source at depth. Nature 427, 724–728. Mirabella, F., Barchi, M., Lupattelli, A., Stucchi, E., Ciaccio, M.G., 2008. Insights on the seismogenic layer thickness from the upper crust structure of the Umbria-Marche Apennines (central Italy). Tectonics 27, TC1010. doi:10.1029/2007TC002134. Mizoguchi, K., Hirose, T., Shimamoto, T., Fukuyama, E., 2007. Reconstruction of seismic faulting by high-velocity friction experiments: an example of the 1995 Kobe earthquake. Geophys. Res. Lett. 34, L01308. doi:10.1029/2006GL027931. Parkhurst, D.L., Appelo, C.A.J., 1999. User's guide to PHREEQC (version 2)—a computer program for speciation, batch-reaction, one-dimensional transport, and inverse geochemical calculations. U.S. Geological Survey Water-Resources Investigations Report, pp. 99–4259 (312 pp.). Pili, E., Poitrasson, F., Gratier, J.P., 2002. Carbon-oxygen isotope and trace element constraints on how fluids percolate faulted limestones from the San Andreas Fault system: partitioning of fluid sources and pathways. Chem. Geol. 190, 231–250. Rice, J.R., 2006. Heating and weakening of faults during earthquake slip. J. Geophys. Res. Earth Surf. 111, B05311. doi:10.1029/2005JB004006. Sato, T., Sakai, R., Furuya, K., Kodama, T., 2000. Coseismic spring flow changes associated with the 1995 Kobe earthquake. Geophys Res Lett 27, 1219–1222. Sato, K., Kumagai, H., Hirose, T., Tamura, H.,Mizoguchi, K., Shimamoto, T., 2009. Experimental study for noble gas release and exchange under high-speed frictional melting. Chem. Geol. 266, 96–103. Sheppard, S.M., Schwarcz, H.P., 1970. Fractionation of carbon and oxygen isotopes and magnesium between coexisting metamorphic calcite and dolomite. Contrib.Mineral. Petrol. 26, 161. Sibson, R.H., 2000. Fluid involvement in normal faulting. J. Geodyn. 29, 469–499. Tinti, E., Spudich, P., Cocco, M., 2005. Earthquake fracture energy inferred from kinematic rupture models on extended faults. J. Geophys. Res. Earth Surf. 110, B12303. doi:10.1029/2005JB003644. Tsunogai, U., Wakita, H., 1995. Precursory chemical-changes in-ground water — Kobe Earthquake, Japan. Science 269, 61–63. Wigley, T.M.L., 1979. Correction. Geochim. Cosmochim. Acta 43, 1395. Wigley, T.M.L., Plummer, L.N., Pearson, F.J., 1978. Mass-transfer and carbon isotope evolution in natural-water systems. Geochim. Cosmochim. Acta 42, 1117–1139.en
dc.description.obiettivoSpecifico2.4. TTC - Laboratori di geochimica dei fluidien
dc.description.obiettivoSpecifico4.5. Studi sul degassamento naturale e sui gas petroliferien
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorDe Paola, N.en
dc.contributor.authorChiodini, G.en
dc.contributor.authorHirose, T.en
dc.contributor.authorCardellini, C.en
dc.contributor.authorCaliro, S.en
dc.contributor.authorShimamoto, T.en
dc.contributor.departmentRock Mechanics Laboratory, Earth Sciences Department, University of Durham, South Road, DH1 3LE Durham, UKen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.departmentKochi Institute for Core Sample Research, Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Japanen
dc.contributor.departmentDipartimento di Scienze della Terra, Università di Perugia, Piazza Università, 06123 Perugia, Italyen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.departmentInstitute of Geology, China Earthquake Administration, Beijing, Chinaen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptUniv. Perugia, Italy-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Bologna, Bologna, Italia-
crisitem.author.deptKochi Institute for Core Sample Research, Japan Agency Marine Earth Science and Technology, Kochi, Japan.-
crisitem.author.deptDipartimento di fisica e Geologia di Perugia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia-
crisitem.author.deptDepartment of Earth and Planetary Systems Science, University of Hiroshima, Hiroshima, Japan.-
crisitem.author.orcid0000-0002-0628-8055-
crisitem.author.orcid0000-0002-5397-3346-
crisitem.author.orcid0000-0002-8522-6695-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
Appears in Collections:Article published / in press
Files in This Item:
File Description SizeFormat Existing users please Login
De Paola et al_EPSL 2011.pdf1.15 MBAdobe PDF
Show simple item record

WEB OF SCIENCETM
Citations 20

24
checked on Feb 10, 2021

Page view(s) 50

202
checked on Mar 27, 2024

Download(s)

37
checked on Mar 27, 2024

Google ScholarTM

Check

Altmetric