Chapopote asphalt volcano may have been generated by supercritical water

Eos

Volumn 86, Issue 42, 2005, Pages

  Hovland, M ^a   Macdonald, I R ^b   Rueslatten H ^c   Johnsen, H K ^a   Naehr, T ^b   Bohrmann, G ^d  

^a STATOIL   (Norway)

^b TEXAS A AND M UNIVERSITY CORPUS CHRISTI   (United States)

^c Numerical Rocks ASA   (Norway)

^d UNIVERSITY OF BREMEN   (Germany)

Author keywords

[No Author keywords available]

Indexed keywords

ASPHALT; SUPERCRITICAL FLOW; VOLCANIC LANDFORM; VOLCANO;

EID: 33645939982     PISSN: 00963941     EISSN: None     Source Type: Journal    
DOI: 10.1029/2005EO420002     Document Type: Review

References (6)

1. Bellissent-Funel, M.-C. (2001), Structure of supercritical water, J. Mol. Liq., 90, 313-322.
2. Feyzullayev, A.A., I.S. Guliyev, and M.F. Tagiyev (2001), Source potential of the Mesozoic-Cenozoic rocks in the South Caspian Basin and their role in forming the oil accumulations In the Lower Pliocene reservoirs,Pet. Geosci., 7, 409-117.
3. Hovland, M. (2005), Is there a close link between salt diapirs and mud volcanoes?, paper presented at the International Workshop on Methane in Sediments and Water Column of the Black Sea, Res. Cent.Ocean Margins, Univ. of Bremen,Sevastopol, Ukraine, 17-22 May
4. MacDonald, I. R., et al. (2004), Asphalt volcanism and chemosynthetic life in the Campeche Knolls, Gulf of Mexico, Science, 304, 909-1002.
5. Tester, J., H. R. Holgate, F.J. Armellini, P. A.Webley, W. R. Killilea, G.T. Hong, and H. E. Berner (1993), Supercritical water oxidation technology in Emerging Technologies in Hazardous Waste Management III, Am. Chem. Soc. Symp. Ser., vol.518, pp.35-76, Oxford Univ. Press, New York.
6. Vendeville, B.C., and M. P. A. Jackson (1992), The rise of diapirs during thin-skinned extension, Mar, Pet. Geol., 9, 331-354.