Page 260 - Geochemical Remote Sensing of The Sub-Surface
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Geochemical Remote Sensing of the Subsurface
           Edited by M. Hale
           Handbook of Exploration Geochemistry, Vol. 7 (G.J.S.  Govett,  Editor)
            9   Elsevier Science B.V.  All rights reserved                      233
           Chapter 7





           AEROSPACE DETECTION OF HYDROCARBON-INDUCED  ALTERATION

           H. YANG, F.D. Van der MEER and J. ZHANG






           INTRODUCTION

              The continuing development of remote sensing has been of considerable significance
           to  earth  scientists  in  general  and  exploration  geologists  in  particular.  Beginning  in  the
           1930s,  aerial photography was used to map  structure  and stratigraphy.  Since  the  1970s,
           imagery  from  satellite  platforms  equipped  with  the  multispectral  scanning  system
           (MSS),  the  thematic  mapper  (TM),  SPOT  and  radar  systems  has  been  used  to  obtain
           synoptic views of the geology of an area and conduct basin-wide assessments (Halbotay,
           1980;  Moore  and  Anderson,  1985).  Airborne  platforms  carrying  multispectral  scanning
           systems  and  imaging  spectrometers,  have  been  used  routinely  to  provide  imagery  for
           geological  mapping  and  identification  of  prospect-scale  structures.  The  use  of  side-
           looking radar images and synthetic aperture radar (Goetz and Rowan,  1981; Froidevaux,
           1980)  provided  the  possibility  to  enhance  subtle  expression  of  subsurface  geologic
           structures.  In general the key to the successful  application of remote  sensing  imagery in
           hydrocarbon  exploration  is  its  integration  with  other  exploration  data  such  as  seismic,
           well,  gravity and magnetic data.  Researchers  have  also attempted to use  remote-sensing
           imagery  to  detect  the  distinct  spectral  characteristics  of  surface  manifestations  of
           hydrocarbon  microseepages,  originating  from  oil  and  gas  reservoirs  at  depth.  This
           chapter  provides  an  overview  of  the  background  to  the  direct  detection  of  onshore
           hydrocarbon  microseepage  by  remote  sensing  techniques  and  the  results  achieved  to
           date.


           Hydrocarbon microseepage


              The  occurrence  at surface  of hydrocarbon seeps  suggests that an oil or gas  reservoir
           leaks  even  though  it  acts  as  a  trap  for  hydrocarbons.  Macroseepage  is  the  visible
           presence  of oil  and  gas  seeping  to  the  surface.  Macroseeps  have  been  documented  in
           various  parts  of  the  world  (Davidson,  1963;  Sittig,  1980;  Hunt,  1981;  Davis,  1967;
           Tedosco,  1995).  Microseeps are invisible trace quantities of hydrocarbons seeping to the
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