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PSNon-Seismic Detection of Hydrocarbons: An Overview*

 

Dietmar “Deet” Schumacher1

 

Search and Discovery Article #40392 (2009)

Posted May 1, 2009

 

*Adapted from poster presentation at 2008 AAPG International Conference and Exhibition, Cape Town, South Africa, October 26-29, 2008 

1Terralliance Technologies, Newport Beach, CA USA ([email protected])

 

Abstract 

The surface expression of hydrocarbon seepage and hydrocarbon-induced alteration of soils and sediments can take many forms including (1) anomalous hydrocarbon concentrations in soils, sediments, and waters; (2) microbiological anomalies and the formation of “paraffin dirt”; (3) mineralogic changes such as formation of calcite, pyrite, uranium, elemental sulfur, and certain magnetic iron oxides and sulfides; (4) bleaching of redbeds; (5) clay mineral alteration; (6) electrochemical changes; (7) electromagnetic and telluric changes, (8) radiation anomalies; and (9) biogeochemical and geobotanical anomalies. These different manifestations have led to development of an equally varied number of geochemical and non-seismic geophysical exploration techniques. These include direct and indirect geochemical methods, magnetic and electrical methods, radioactivity-based methods, and Previous HitremoteNext Hit Previous HitsensingNext Hit methods.  

What are the benefits of using geochemical and non-seismic hydrocarbon detection methods in conjunction with conventional exploration methods? In a review of more than 1100 US and International wildcat wells - all drilled after completion of geochemical or non-seismic hydrocarbon detection surveys - more than 80% of wells drilled on prospects associated with positive hydrocarbon anomalies resulted in commercial discoveries; in contrast, only 13% of wells drilled on prospects not associated with such anomalies resulted in discoveries. Although these methods cannot replace conventional exploration methods, they can be a powerful complement to them. The need for such an integrated exploration strategy cannot be overemphasized. This presentation will be illustrated with examples from geochemical surveys, aeromagnetic-micromagnetic surveys, passive and active electromagnetic surveys, and Previous HitremoteNext Hit Previous HitsensingNext Hit data.

  

References 

Lytle, R.J., and D.L. Lager, 1976, Using the natural frequency concept in Previous HitremoteNext Hit probing of the earth: Radio Science, v. 7/3, p. 245-250. 

MacDonald, I.R., J.F., Reilly, Jr., S.E. Best, R. Venkataramaiah, R. Sassen, N.L. Guinasso, Jr., and J. Amos, 1996, Previous HitRemoteNext Hit Previous HitsensingNext Hit inventory of active oil seeps and chemosynthetic communities in the northern Gulf of Mexico, in  Hydrocarbon Migration and its Near-surface Expression: AAPG Memoir 66, p. 27-37. 

Van den Bark, E., and O.D. Thomas, 1980, Ekofisk, First of the giant oil fields in Western Europe, in Giant Oil and Gas Fields of the Decade 1968-1978: AAPG Memoir 66, p. 195-224. 

Williams, A., and G. Lawrence, 2002, The Role of satellite seep detection in exploring the South Atlantic’s ultradeep water, in Surface Exploration Case Histories: Applications of Geochemistry, Magnetics, and Previous HitRemoteNext Hit Previous HitSensingTop: AAPG Studies in Geology 48, p. 327-344.