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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
remote
sensing
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
remote
sensing
data.
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