Processes controlling porosity and permeability in volcanic reservoirs from the Austral and Neuquén basins, Argentina

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 por...

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Autor principal: Sruoga, P.
Otros Autores: Rubinstein, N.
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Lenguaje:Inglés
Publicado: 2007
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100 1 |a Sruoga, P. 
245 1 0 |a Processes controlling porosity and permeability in volcanic reservoirs from the Austral and Neuquén basins, Argentina 
260 |c 2007 
270 1 0 |m Sruoga, P.; CONICET-SEGEMAR, Avda. Julio A. Roca 651, Ciudad de Buenos Aires, Argentina; email: psruog@minproduccion.gov.ar 
506 |2 openaire  |e Política editorial 
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504 |a Phillips, W.J., Hydraulic fracturing and mineralization (1972) Journal of the Geological Society (London), 128, pp. 337-359 
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504 |a Smith, J., Miyake, Y., Oikawa, T., Interpretation of porosity in dacite lava domes as ductile-brittle failure textures (2001) Journal of Volcanology and Geothermal Research, 112, pp. 25-35 
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504 |a Stimac, J., Powell, T., Golla, G., Porosity and permeability of the Tiwi geothermal field, Philippines, based on continuous and spot core measurement (2004) Geothermic, 33, pp. 87-107 
504 |a Storey, B.C., Alabaster, T., Hole, M.J., Pankhurst, R.J., Wever, H.E., Role of subduction-plate boundary forces during the initial stages of Gondwana break-up: Evidence from the proto-Pacific margin of Antarctica (1992) Magmatism and the Causes of Continental Break-Up, pp. 149-164. , in B. C. Storey, T. Alabaster, and R. J. Pankhurst, eds., Geological Society (London) Special Publication 68 
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504 |a Uliana, M.A., Biddle, K.T., Cerdán, J., Mesozoic extension and formation of Argentina sedimentary basin: Extensional tectonics and stratigraphy of the North Atlantic margin (1989) AAPG Memoir, 46, pp. 599-613 
504 |a Vergani, G.D., Tankard, A.J., Belotti, H.J., Welkink, H.J., Tectonic evolution and paleogeography of the Neuquén Basin, Argentina (1995) Petroleum Basins of South America, pp. 383-402. , in A. J. Tankard, R. Suarez Soruco, and H. Welsink, eds., AAPG Memoir 62 
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504 |a Zöllner, W., Amos, A., Descripción geológica de la hoja 32b Chos Malal, Provincia del Neuquén: Carta geólogico-económica de la República Argentina, escala 1:200,000 (1973) Servicio Nacional De Minería Y Geología Boletin, 143, p. 91 
520 3 |a 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 gaspipe 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. Copyright © 2007. The American Association of Petroleum Geologists. All rights reserved.  |l eng 
593 |a CONICET-SEGEMAR, Avda. Julio A. Roca 651, Ciudad de Buenos Aires, Argentina 
593 |a Universidad de Buenos Aires, Consejo Nacional de Investigaciones Cientificas y Tecnicas (UBA-CONICET), Depto. de Geología, Pabellón 2, Ciudad de Buenos Aires, Argentina 
651 4 |a ARGENTINA 
651 4 |a ARGENTINA 
651 4 |a NEUQUEN BASIN 
651 4 |a SOUTH AMERICA 
690 1 0 |a PETROPHYSICAL DATA 
690 1 0 |a RESERVOIR QUALITY 
690 1 0 |a DISSOLUTION 
690 1 0 |a HYDRAULIC FRACTURING 
690 1 0 |a LITHOLOGY 
690 1 0 |a MECHANICAL PERMEABILITY 
690 1 0 |a PETROLEUM PROSPECTING 
690 1 0 |a POROSITY 
690 1 0 |a VOLCANIC ROCKS 
690 1 0 |a PETROLEUM RESERVOIRS 
690 1 0 |a IGNIMBRITE 
690 1 0 |a LITHOLOGY 
690 1 0 |a PERMEABILITY 
690 1 0 |a POROSITY 
690 1 0 |a RESERVOIR 
690 1 0 |a AUSTRAL BASIN 
690 1 0 |a PATAGONIA 
700 1 |a Rubinstein, N. 
773 0 |d 2007  |g v. 91  |h pp. 115-129  |k n. 1  |p AAPG Bull.  |x 01491423  |w (AR-BaUEN)CENRE-786  |t AAPG Bulletin 
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