Please use this identifier to cite or link to this item:
http://hdl.handle.net/2122/4520| DC Field | Value | Language |
|---|---|---|
| dc.contributor.authorall | Mazot, A.; Department of Earth and Environmental Sciences, CP 160/02, Université Libre de Bruxelles, 50 Ave. Roosevelt, 1050 Brussels, Belgium | en |
| dc.contributor.authorall | Bernard, A.; Department of Earth and Environmental Sciences, CP 160/02, Université Libre de Bruxelles, 50 Ave. Roosevelt, 1050 Brussels, Belgium | en |
| dc.contributor.authorall | Fischer, T.; Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, NM 87131-0001, USA | en |
| dc.contributor.authorall | Inguaggiato, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italia | en |
| dc.contributor.authorall | Sutawidjaja, I. S.; Directorate of Volcanology and Geological Hazard Mitigation, Jalan Diponegoro 57, Bandung 40122, Indonesia | en |
| dc.date.accessioned | 2008-12-09T09:53:07Z | en |
| dc.date.available | 2008-12-09T09:53:07Z | en |
| dc.date.issued | 2008-06-27 | en |
| dc.identifier.uri | http://hdl.handle.net/2122/4520 | en |
| dc.description.abstract | Papandayan is a stratovolcano situated in West Java, Indonesia. Since the last magmatic eruption in 1772,only few hydrothermal explosions have occurred. An explosive eruption occurred in November 2002 and ejected ash and altered rocks. The altered rocks show that an advanced argillic alteration took place in the hydrothermal system by interaction between acid fluids and rocks. Four zones of alteration have been defined and are limited in extension and shape along faults or across permeable structures at different levels beneath the active crater of the volcano. At the present time, the activity is centered in the northeast crater with discharge of low temperature fumaroles and acid hot springs. Two types of acid fluids are emitted in the crater of Papandayan volcano: (1) acid sulfate-chloride waters with pH between 1.6 and 4.6 and (2) acid sulfate waters with pH between 1.2 and 2.5. The water samples collected after the eruption on January 2003 reveal an increase in the SO4/Cl and Mg/Cl ratios. This evolution is likely explained by an increase in the neutralization of acid fluids and tends to show that water–rock interactions were more significant after the eruption. The evolution in the chemistry observed since 2003 is the consequence of the opening of new fractures at depth where unaltered (or less altered) volcanic rocks were in contact with the ascending acid waters. The high δ34S values (9–17‰) observed in acid sulfatechloride waters before the November 2002 eruption suggest that a significant fraction of dissolved sulfates was formed by the disproportionation of magmatic SO2. On the other hand, the low δ34S (−0.3–7‰) observed in hot spring waters sampled after the eruption suggest that the hydrothermal contribution (i.e. the surficial oxidation of hydrogen sulfide) has increased. | en |
| dc.language.iso | English | en |
| dc.publisher.name | Elsevier | en |
| dc.relation.ispartof | Journal of Volcanology and Geothermal Research | en |
| dc.relation.ispartofseries | /178(2008) | en |
| dc.subject | Papandayan volcano | en |
| dc.subject | Indonesia | en |
| dc.subject | phreatic eruption | en |
| dc.subject | hydrothermal system | en |
| dc.subject | fluid geochemistry | en |
| dc.subject | advanced argillic alteration | en |
| dc.subject | gas geochemistry | en |
| dc.title | Chemical evolution of thermal waters and changes in the hydrothermal system of Papandayan volcano (West Java, Indonesia) after the November 2002 eruption | en |
| dc.type | article | en |
| dc.description.status | Published | en |
| dc.type.QualityControl | Peer-reviewed | en |
| dc.description.pagenumber | 276-286 | en |
| dc.identifier.URL | http://www.elsevier.com/wps/find/homepage.cws_home | en |
| dc.subject.INGV | 04. Solid Earth::04.08. Volcanology::04.08.01. Gases | en |
| dc.subject.INGV | 04. Solid Earth::04.08. Volcanology::04.08.05. Volcanic rocks | en |
| dc.subject.INGV | 04. Solid Earth::04.08. Volcanology::04.08.06. Volcano monitoring | en |
| dc.subject.INGV | 05. General::05.02. Data dissemination::05.02.01. Geochemical data | en |
| dc.subject.INGV | 05. General::05.02. Data dissemination::05.02.03. Volcanic eruptions | en |
| dc.identifier.doi | 10.1016/j.jvolgeores.2008.06.022 | en |
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Mazot et al. / Journal of Volcanology and Geothermal Research 178 (2008) 276–286 | en |
| dc.description.obiettivoSpecifico | 1.2. TTC - Sorveglianza geochimica delle aree vulcaniche attive | en |
| dc.description.obiettivoSpecifico | 2.4. TTC - Laboratori di geochimica dei fluidi | en |
| dc.description.journalType | JCR Journal | en |
| dc.description.fulltext | reserved | en |
| dc.contributor.author | Mazot, A. | en |
| dc.contributor.author | Bernard, A. | en |
| dc.contributor.author | Fischer, T. | en |
| dc.contributor.author | Inguaggiato, S. | en |
| dc.contributor.author | Sutawidjaja, I. S. | en |
| dc.contributor.department | Department of Earth and Environmental Sciences, CP 160/02, Université Libre de Bruxelles, 50 Ave. Roosevelt, 1050 Brussels, Belgium | en |
| dc.contributor.department | Department of Earth and Environmental Sciences, CP 160/02, Université Libre de Bruxelles, 50 Ave. Roosevelt, 1050 Brussels, Belgium | en |
| dc.contributor.department | Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, NM 87131-0001, USA | en |
| dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italia | en |
| dc.contributor.department | Directorate of Volcanology and Geological Hazard Mitigation, Jalan Diponegoro 57, Bandung 40122, Indonesia | en |
| item.openairetype | article | - |
| item.cerifentitytype | Publications | - |
| item.languageiso639-1 | en | - |
| item.grantfulltext | restricted | - |
| item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
| item.fulltext | With Fulltext | - |
| crisitem.author.dept | Instituto de Geofisica, UNAM, Mexico | - |
| crisitem.author.dept | Université Libre de Bruxelles, Département des Sciences de la Terre et de l'Environnement. | - |
| crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Palermo, Palermo, Italia | - |
| crisitem.author.dept | Directorate of Volcanology and Geological Hazard Mitigation, Jalan Diponegoro 57, Bandung 40122, Indonesia | - |
| crisitem.author.orcid | 0000-0002-4419-5618 | - |
| crisitem.author.orcid | 0000-0003-3726-9946 | - |
| crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
| crisitem.classification.parent | 04. Solid Earth | - |
| crisitem.classification.parent | 04. Solid Earth | - |
| crisitem.classification.parent | 04. Solid Earth | - |
| crisitem.classification.parent | 05. General | - |
| crisitem.classification.parent | 05. General | - |
| crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
| Appears in Collections: | Article published / in press | |
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| Mazot et al_JVGR2088.pdf | Main Article | 1.87 MB | Adobe PDF |
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