Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/5311
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dc.contributor.authorallEtiope, G.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.contributor.authorallMartinelli, G.; ARPA Emilia Romagna, Via Amendola 2, 42100 Reggio Emilia, Italyen
dc.date.accessioned2009-12-03T08:33:42Zen
dc.date.available2009-12-03T08:33:42Zen
dc.date.issued2009-10en
dc.identifier.urihttp://hdl.handle.net/2122/5311en
dc.description.abstractBonini (2009) has recently written an interesting paper dealing with the structural setting and relationships to seismicity of a CO2(carbon dioxide)-driven mud volcano, called Pieve S. Stefano (PSS), located in the Northern Apennines of Italy.We outline here that PSS is not a mud volcano at all. The author erroneously attributes the term ‘‘mud volcano’’ (also featured in the title of the article) to a CO2-dominant gas manifestation, which should be considered as a ‘‘mofette’’ or more generally a dry CO2-vent (or ‘‘gas pool’’; Minissale et al., 2000; Heinicke et al., 2006). Our comment does not dispute Bonini’s data interpretations and conclusions (for which a first comment has already been made by Collettini, in press), but discusses why misuse of the term ‘‘mud volcano’’ may lead to misquotations in future mud volcano literature.en
dc.language.isoEnglishen
dc.publisher.nameElsevier Ltd.en
dc.relation.ispartofJournal of Structural Geologyen
dc.relation.ispartofseries10/31 (2009)en
dc.subjectMud volcanoen
dc.subjectMofetteen
dc.subjectCarbon dioxideen
dc.subjectGas manifestationen
dc.title‘‘Pieve Santo Stefano’’ is not a mud volcano: Comment on ‘‘Structural controls on a carbon dioxide-driven mud volcano field in the Northern Apennines’’ (by Bonini, 2009)en
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber1270-1271en
dc.subject.INGV03. Hydrosphere::03.04. Chemical and biological::03.04.05. Gasesen
dc.identifier.doi10.1016/j.jsg.2009.06.009en
dc.relation.referencesBaciu, C.L., Caracausi, A., Etiope, G., Italiano, F., 2007. Mud volcanoes and methane seeps in Romania: main features and gas flux. Ann. Geophys. 50 (4), 501–512. Bonini, M., 2009. Structural controls on a carbon dioxide-driven mud volcano field in the Northern Apennines (Pieve Santo Stefano, Italy): relations with preexisting steep discontinuities and seismicity. J. Struct. Geol. 31, 44–54. Collettini, C. Comment on ‘‘Structural controls on a carbon dioxide-driven mud volcano field in the Northern Apennines (Pieve Santo Stefano, Italy): relations with pre-existing steep discontinuities and seismicity’’. J. Struct. Geol., in press. doi:10.1016/j.jsg.2009.02.002. Dimitrov, L., 2002. Mud volcanoesdthe most important pathway for degassing deeply buried sediments. Earth Sci. Rev. 59, 49–76. Etiope, G., Feyzullayev, A., Baciu, C.L., 2009a. Terrestrial methane seeps and mud volcanoes: a global perspective of gas origin. Mar. Petrol. Geol. 26, 333–344. Etiope, G., Feyzullayev, A., Milkov, A.V., Waseda, A., Mizobe, K., Sun, C.H., 2009b. Evidence of subsurface anaerobic biodegradation of hydrocarbons and potential secondary methanogenesis in terrestrial mud volcanoes. Mar. Petrol. Geol.. doi:10.1016/j.marpetgeo.2008.12.002. Etiope, G., Martinelli, G., Caracausi, A., Italiano, F., 2007. Methane seeps volcanoes in Italy: gas origin, fractionation and emission to the atmosphere. Geophys. Res. Lett. 34, L14303. doi:10.1029/2007GL030341. Etiope, G., Papatheodorou, G., Christodoulou, D., Ferentinos, G., Sokos, E., Favali, P., 2006. Methane and hydrogen sulfide seepage in the NW Peloponnesus petroliferous basin (Greece): origin and geohazard. AAPG Bull. 90 (5), 701–713. Heinicke, J., Braun, T., Burgassi, P., Italiano, F., Martinelli, G., 2006. Gas flow anomalies in seismogenic zones in the Upper Tiber Valley, Central Italy. Geophys. J. Int. 167, 794–806. Kopf, A.J., 2002. Significance of mud volcanism. Rev. Geophys. 40 (2), 1005. doi:10.1029/2000RG000093. Magoon, L.B., Schmoker, J.W., 2000. The total petroleum system – the natural fluid network that constraints the assessment units. In: U.S. Geological SurveyWorld Petroleum Assessment 2000dDescription and Results. USGS Digital Data Series 60, World Energy Assessment Team, p. 31. Martinelli, G., Judd, A., 2004. Mud volcanoes of Italy. Geol. J. 39, 49–61. Minissale, A., Magro, G., Martinelli, G., Vaselli, O., Tassi, G.F., 2000. Fluid geochemical transect in the Northern Apennines (Central–Northern Italy): fluid genesis and migration and tectonic implications. Tectonophysics 319, 199–222. Motyka, R.J., Poreda, R.J., Jeffrey, W.A., 1989. Geochemistry, isotopic composition, and origin of fluids emanating from mud volcanoes in the Copper River basin Alaska. Geochim. Cosmochim. Acta 53, 29–41. Skinner, J.A., Mazzini, A. Martian mud volcanism: terrestrial analogs and implications for formational scenarios. Mar. Petrol. Geol., in press. doi:10.1016/j. marpetgeo.2009.02.006. Vaselli, O., Tassi, F., Minissale, A., Capaccioni, B., Magro, G., Evans, W.C., 1997. Geochemistry of natural gas manifestations from the Upper Tiber Valley (Central Italy). Miner. Petrogr. Acta XL, 201–212. G. Etiope, G. Martinelli / Journal of Structural Geology 31 (2009) 1270–1271 1271en
dc.description.obiettivoSpecifico4.5. Studi sul degassamento naturale e sui gas petroliferien
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorEtiope, G.en
dc.contributor.authorMartinelli, G.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.contributor.departmentARPA Emilia Romagna, Via Amendola 2, 42100 Reggio Emilia, Italyen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia-
crisitem.author.deptARPA Emilia-Romagna-
crisitem.author.orcid0000-0001-8614-4221-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent03. Hydrosphere-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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