A new hydrothermal scenario for the 2006 Lusi eruption, Indonesia. Insights from gas geochemistry

Earth and Planetary Science Letters

Volumn 317-318, Issue , 2012, Pages 305-318

  Mazzini, Adriano ^a   Etiope, Giuseppe ^b   Svensen, Henrik ^a  

^a UNIVERSITY OF OSLO   (Norway)

^b BABE BOLYAI UNIVERSITY   (Romania)

Author keywords

CO 2 and CH 4; Gas origin; Lusi eruption; Mantle; Mud volcanoes; Sediment hosted hydrothermal system

Indexed keywords

DEEP ROCKS; EQUILIBRIUM TEMPERATURES; GAS GENERATION; GAS GEOCHEMISTRY; HYDROTHERMAL FLUIDS; HYDROTHERMAL SYSTEM; HYDROTHERMAL VENT; INDONESIA; ISOTOPIC COMPOSITION; LUSI ERUPTION; MAGMATIC INTRUSIONS; MANTLE; MUD VOLCANOES; NEW MODEL; ORGANIC SOURCES; SEDIMENT-HOSTED HYDROTHERMAL SYSTEM; SEISMIC ACTIVITY; SOURCE ROCKS; VOLCANIC COMPLEX;

ANOXIC SEDIMENTS; CARBOXYLATION; GASES; HELIUM; HOT SPRINGS; HYDROCARBONS; KEROGEN; NATURAL GAS FIELDS; SEDIMENTOLOGY; VOLCANOES;

CARBON DIOXIDE;

BRECCIA; FLUID PRESSURE; HYDROCARBON; HYDROTHERMAL VENT; ISOTOPIC COMPOSITION; KEROGEN; MUD VOLCANO; ORGANIC MATTER; VOLCANIC ERUPTION;

GREATER SUNDA ISLANDS; JAVA; SUNDA ISLES;

EID: 84455170846     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.epsl.2011.11.016     Document Type: Article

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