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AAPG Bulletin; January 2007; v. 91; no. 1; p. 115-129; DOI: 10.1306/08290605173
© 2007 American Association of Petroleum Geologists (AAPG)
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Processes controlling porosity and permeability in volcanic reservoirs from the Austral and Neuquén basins, Argentina

Patricia Sruoga1 and Nora Rubinstein2

1 Consejo Nacional de Investigaciones Cientificas y Tecnicas-Servicio Geologico Minero Argentino (CONICET-SEGEMAR), Avda. Julio A. Roca 651, Ciudad de Buenos Aires, Argentina; psruog{at}minproduccion.gov.ar; patySruoga{at}yahoo.com.ar
2 Universidad de Buenos Aires-Consejo Nacional de Investigaciones Cientificas y Tecnicas (UBA-CONICET), Depto. de Geología, Pabellón 2, Ciudad Universitaria, Ciudad de Buenos Aires, Argentina; nora{at}gl.fcen.uba.ar

Patricia Sruoga (Ph.D., University of La Plata) is an associate researcher at the National Council of Scientific and Technical Research (CONICET) and works as a volcanologist at the Argentine Geological and Mining Service (SEGEMAR). Her research focuses on ancient and modern volcanic sequences. Since 2000, she has worked as a consultant for local oil companies, studying volcanic reservoirs in the Neuquén and Austral basins.

Nora Rubinstein (Ph.D., University of Buenos Aires, 1996) is an assistant professor in mineralogy at the University of Buenos Aires and an associate researcher of the CONICET. Her research focuses on hydrothermal, deuteric, and supergenic processes and products. Recently, she worked as a consultant for oil companies in Neuquén and Austral basins.

Volcanic rocks develop primary and secondary porosity and permeability, depending on both their lithology and the sequence of processes involved in their formation. Primary processes (welding, deuteric crystal dissolution, gas release, flow fragmentation, and crystal shattering) may lead to high porosity and permeability, the best example of which is a nonwelded ignimbrite with well-developed gas-pipe zones. Secondary processes (different types of alteration), however, tend to decrease primary porosity. However, certain secondary processes, such as dissolution and hydraulic fracturing, may contribute to enhance total porosity and permeability. These conclusions were developed through a systematic review of reservoir quality in volcanic rocks, integrating lithology and process interpretation with petrophysical data. The said information was taken from selected cores of volcanic rocks from the Serie Tobífera unit in the Austral Basin and the Precuyano unit in the Neuquén Basin, Argentina.

A clear understanding of both primary and secondary processes may serve to predict the quality of volcanic reservoirs and could be used as a guide for oil and gas exploration and development in many parts of the world.







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