Please use this identifier to cite or link to this item:
http://hdl.handle.net/2122/5073| DC Field | Value | Language |
|---|---|---|
| dc.contributor.authorall | Rouwet, D.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italia | en |
| dc.contributor.authorall | Inguaggiato, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italia | en |
| dc.contributor.authorall | Taran, Y.; Instituto de Geofisica UNAM, Mexico | en |
| dc.contributor.authorall | Varley, N.; universidad de Colima, Colima Mexico | en |
| dc.contributor.authorall | Santiago, J. A.; Instituto de Geofisica UNAM, Mexico | en |
| dc.date.accessioned | 2009-06-11T13:13:39Z | en |
| dc.date.available | 2009-06-11T13:13:39Z | en |
| dc.date.issued | 2009 | en |
| dc.identifier.uri | http://hdl.handle.net/2122/5073 | en |
| dc.description.abstract | This study presents baseline data for future geochemical monitoring of the active Tacaná volcano– hydrothermal system (Mexico–Guatemala). Seven groups of thermal springs, related to a NW/SE-oriented fault scarp cutting the summit area (4,100m a.s.l.), discharge at the northwest foot of the volcano (1,500–2,000m a.s.l.); another one on the southern ends of Tacaná (La Calera). The near-neutral (pH from 5.8 to 6.9) thermal (T from 25.7°C to 63.0°C) HCO3–SO4 waters are thought to have formed by the absorption of a H2S/SO2–CO2-enriched steam into a Cl-rich geothermal aquifer, afterwards mixed by Na/HCO3-enriched meteoric waters originating from the higher elevations of the volcano as stated by the isotopic composition (δD and δ18O) of meteoric and spring waters. Boiling temperature fumaroles (89°C at ~3,600m a.s.l. NW of the summit), formed after the May 1986 phreatic explosion, emit isotopically light vapour (δD and δ18O as low as −128 and −19.9‰, respectively) resulting from steam separation from the summit aquifer. Fumarolic as well as bubbling gases at five springs are CO2-dominated. The δ13CCO2 for all gases show typical magmatic values of −3.6 ± 1.3‰ vs V-PDB. The large range in 3He/4He ratios for bubbling, dissolved and fumarolic gases [from 1.3 to 6.9 atmospheric 3He/4He ratio (RA)] is ascribed to a different degree of near-surface boiling processes inside a heterogeneous aquifer at the contact between the volcanic edifice and the crystalline basement (4He source). Tacaná volcano offers a unique opportunity to give insight into shallow hydrothermal and deep magmatic processes affecting the CO2/3He ratio of gases: bubbling springs with lower gas/water ratios show higher 3He/4He ratios and consequently lower CO2/3He ratios (e.g. Zarco spring). Typical Central American CO2/3He and 3He/4He ratios are found for the fumarolic Agua Caliente and Zarco gases (3.1 ± 1.6 × 1010 and 6.0 ± 0.9 RA, respectively). The L/S (5.9 ± 0.5) and (L + S)/M ratios (9.2 ± 0.7) for the same gases are almost identical to the ones calculated for gases in El Salvador, suggesting an enhanced slab contribution as far as the northern extreme of the Central American Volcanic Arc, Tacaná. | en |
| dc.description.sponsorship | This study was financially supported by DGAPA UNAM #IN101706 and INGVPalermo. | en |
| dc.language.iso | English | en |
| dc.publisher.name | Springer-Verlag | en |
| dc.relation.ispartof | Bulletin of Volcanology | en |
| dc.relation.ispartofseries | /71(2009) | en |
| dc.relation.isversionof | http://hdl.handle.net/2122/4511 | en |
| dc.subject | Tacaná volcano | en |
| dc.subject | Fluid geochemistry | en |
| dc.subject | Volcano–hydrothermal system | en |
| dc.subject | Bubbling gases | en |
| dc.subject | Fumaroles | en |
| dc.subject | Isotopes | en |
| dc.subject | Volcanic surveillance | en |
| dc.title | Chemical and isotopic compositions of thermal springs, fumaroles and bubbling gases at Tacaná Volcano (Mexico–Guatemala): implications for volcanic surveillance | en |
| dc.type | article | en |
| dc.description.status | Published | en |
| dc.type.QualityControl | Peer-reviewed | en |
| dc.description.pagenumber | 319-335 | en |
| dc.subject.INGV | 01. Atmosphere::01.01. Atmosphere::01.01.07. Volcanic effects | en |
| dc.identifier.doi | 10.1007/s00445-008-0226-x | en |
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J Volcanol Geotherm Res 88:99–107 Zimbelman DR, Rye RO, Landis GP (2000) Fumaroles in ice caves on the summit of Mount Rainier—preliminary stable isotope, gas, and geochemical studies. J Volcanol Geotherm Res 97:457–473 Zimmer MM, Fischer TP, Hilton DR, Alvarado GE, Sharp ZD, Walker JA (2004) Nitrogen systematics and gas fluxes of subduction zones: Insights from Costa Rica arc volatiles. Geochem Geophys Geosyst 5:Q05J11 doi:10.1029/2003GC000651 | en |
| dc.description.obiettivoSpecifico | 1.3. TTC - Sorveglianza geodetica delle aree vulcaniche attive | en |
| dc.description.journalType | JCR Journal | en |
| dc.description.fulltext | partially_open | en |
| dc.contributor.author | Rouwet, D. | en |
| dc.contributor.author | Inguaggiato, S. | en |
| dc.contributor.author | Taran, Y. | en |
| dc.contributor.author | Varley, N. | en |
| dc.contributor.author | Santiago, J. A. | en |
| dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italia | en |
| dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italia | en |
| dc.contributor.department | Instituto de Geofisica UNAM, Mexico | en |
| dc.contributor.department | Instituto de Geofisica UNAM, Mexico | en |
| item.openairetype | article | - |
| item.cerifentitytype | Publications | - |
| item.languageiso639-1 | en | - |
| item.grantfulltext | open | - |
| item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
| item.fulltext | With Fulltext | - |
| crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Bologna, Bologna, Italia | - |
| crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Palermo, Palermo, Italia | - |
| crisitem.author.dept | Institute of Geophysics, Universidad Nacional Autonoma de Mexico, Ciudad Universitario, Del. Coyocan, 04510 Mexico, DF, Mexico | - |
| crisitem.author.dept | Servicio Sismológico Nacional, Instituto de Geofísica, UNAM,Ciudad Universitaria, Ciudad Universitaria, Circuito Exterior s/n, CP 04510 Del. Coyoacán, México, DF, Mexico | - |
| crisitem.author.orcid | 0000-0003-3366-3882 | - |
| crisitem.author.orcid | 0000-0003-3726-9946 | - |
| crisitem.author.orcid | 0000-0003-3390-4316 | - |
| crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
| crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
| crisitem.classification.parent | 01. Atmosphere | - |
| crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
| crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
| Appears in Collections: | Article published / in press | |
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| Rouwet et al Tacaná BV 2008.pdf | Main article PDF MS | 1.22 MB | Adobe PDF | View/Open |
| Rouwet Tacana BV 2009.pdf | 706.45 kB | Adobe PDF |
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