Structural control on carbon dioxide diffuse degassing at the Caviahue ? Copahue Volcanic Complex, Argentina

STEFANIA VENTURI; DIEGO WINOCUR; FRANCO TASSI; LAMBERTI, MARIA CLARA; MARIANO AGUSTO; HERNÁN BARCELONA; NICOLÁS VIGIDE; DANIEL YAGUPSKY; MARÍA LAURA VELEZ

Viena

Congreso; EGU General Assembly 2019; 2019

Caviahue ? Copahue Volcanic Complex (CCVC) is located within the Andean Cordillera, in the Neuquénprovince, Argentina. This tectono-magmatic system lies within the northern termination of the Liquiñe ? Ofquifault zone, a 1,200-km-long intra-arc strike-slip fault system. Fluid emissions are fed by a hydrothermal reservoirlocated at 800 m depth, mostly recharged by meteoric water and heated by a magmatic chamber located at 5km depth. Over 200 tons per day of CO2 are released by this system thorough diffuse degassing from the soil.The aim of this study is to evaluate the control that the local structural architecture exerts on CO2 flow, from thehydrothermal reservoir to the surface.The correlation between diffuse degassing anomalies and geological brittle structures (i.e. faults and fractures) wasbased on punctual diffuse degassing measurements coupled with structural data. A total of 1,819 measurements ofCO2 flux and soil temperature were carried out, over an area of ∼10 km2. The CO2 flux database was processedin order to map the spatial distribution of diffuse emissions. The local structure was characterized by means of akinematic analysis of fault-slip data.The geochemical analysis showed well-defined CO2 diffuse degassing anomalies in four hydrothermal siteswithin the CCVC. These anomalies follow clear linear trends that can be clustered in different domains regardingtheir orientations. The principal domain strikes NE-SW. The analysis of the fault-slip data gave as a result anextensional stress regime. This is evidenced by three fault sets. The main set consists of NE-SW normal faults,which result in horst-and-graben structures. The second set is constituted by NW-SE faults, that act as transferzones between the main extensional structures. These faults present strike-slip kinematics with minor normalcomponents. The third set consists of E-W oriented dextral strike-slip faults. Two length-weighted rose diagramswere computed, plotting diffuse degassing anomalies directions and fault planes directions. The similarity of theseplots suggests that the main NE-SW normal faults constitute the preferential pathways for soil diffuse CO2. Thisalso suggests that the two secondary fault sets act as fluids pathways as well. The position of diffuse degassinganomalies with respect to the fault traces suggests that diffuse degassing occurs in several structural settings. CO2rises through fault planes; it also rises through areas between fault segments and terminations of individual faults,characterized by relatively high structural damage.