Gallery
*click on image to enlarge*
![Drs. Jan Szewczyk and Gary Zielinski at the Polish Geological Institute museum in Warsaw, Poland, April 2007 (photo by Robyn Zielinski).](http://d10j3mvrs1suex.cloudfront.net/s:bzglfiles/u/24802/38e4f67dcef076075f21fe27b820d830c9b619f4/original/2870430-orig.jpg/!!/b%3AW1sic2l6ZSIsIjM1MHciXV0%3D/meta%3AeyJzcmNCdWNrZXQiOiJiemdsZmlsZXMifQ%3D%3D.jpg)
Drs. Jan Szewczyk and Gary Zielinski at the Polish Geological Institute museum in Warsaw, Poland, April 2007 (photo by Robyn Zielinski).
![Relative heat flow versus a suite of geochemical data for an active hydrocarbon seep, offshore north Borneo (after Zielinski et al., 2007).](http://d10j3mvrs1suex.cloudfront.net/s:bzglfiles/u/24802/aa416dd0c515687231e9207c43762bc76646287b/original/2370456-orig.jpg/!!/b%3AW1sic2l6ZSIsIjM1MHciXV0%3D/meta%3AeyJzcmNCdWNrZXQiOiJiemdsZmlsZXMifQ%3D%3D.jpg)
Relative heat flow versus a suite of geochemical data for an active hydrocarbon seep, offshore north Borneo (after Zielinski et al., 2007).
![Hydrothermics in the Wyoming Overthrust Belt (after Zielinski et al., 1985) from measurements performed in seismic shot holes. Flow axes coincide with hydrocarbon producing structures.](http://d10j3mvrs1suex.cloudfront.net/s:bzglfiles/u/24802/b1cf9aade01c1f941f51c34235901e993b978a4f/original/2365942-orig.jpg/!!/b%3AW1sic2l6ZSIsIjM1MHciXV0%3D/meta%3AeyJzcmNCdWNrZXQiOiJiemdsZmlsZXMifQ%3D%3D.jpg)
Hydrothermics in the Wyoming Overthrust Belt (after Zielinski et al., 1985) from measurements performed in seismic shot holes. Flow axes coincide with hydrocarbon producing structures.
![Relative heat flow due to fluid upwelling from depth in the Magellan Basin, Tierra del Fuego (after Zielinski and Bruchhausen, 1983).](http://d10j3mvrs1suex.cloudfront.net/s:bzglfiles/u/24802/392e045e15e1ed5884a053d5601ea74fb3cfc17d/original/2365933-orig.jpg/!!/b%3AW1sic2l6ZSIsIjM1MHciXV0%3D/meta%3AeyJzcmNCdWNrZXQiOiJiemdsZmlsZXMifQ%3D%3D.jpg)
Relative heat flow due to fluid upwelling from depth in the Magellan Basin, Tierra del Fuego (after Zielinski and Bruchhausen, 1983).
!['Real time' thermograd data over 2 days showing lowering/raising of heat-flow corer along ship's track, offshore north Borneo 2003. An active seep is indicated in center of record.](http://d10j3mvrs1suex.cloudfront.net/s:bzglfiles/u/24802/218ed7e9f35de761e85902a672216ca24f2663d3/original/2166787.jpg/!!/b%3AW1sic2l6ZSIsIjM1MHciXV0%3D/meta%3AeyJzcmNCdWNrZXQiOiJiemdsZmlsZXMifQ%3D%3D.jpg)
'Real time' thermograd data over 2 days showing lowering/raising of heat-flow corer along ship's track, offshore north Borneo 2003. An active seep is indicated in center of record.
!["Ewing Technique" of heat flow and piston coring pioneered by the Lamont-Doherty Earth Observatory of Columbia University.](http://d10j3mvrs1suex.cloudfront.net/s:bzglfiles/u/24802/4387fbc800c2a67a137ba158a253aa1c116e93c0/original/2155827.jpg/!!/b%3AW1sic2l6ZSIsIjM1MHciXV0%3D/meta%3AeyJzcmNCdWNrZXQiOiJiemdsZmlsZXMifQ%3D%3D.jpg)
"Ewing Technique" of heat flow and piston coring pioneered by the Lamont-Doherty Earth Observatory of Columbia University.
!["Outrigger" thermistor probe supported at two ends used for the first TDI-BI heat flow survey offshore Angola, 1997.](http://d10j3mvrs1suex.cloudfront.net/s:bzglfiles/u/24802/7d65843412589d30758af7b5247c25d0cc5ec01d/original/2155825.jpg/!!/b%3AW1sic2l6ZSIsIjM1MHciXV0%3D/meta%3AeyJzcmNCdWNrZXQiOiJiemdsZmlsZXMifQ%3D%3D.jpg)
"Outrigger" thermistor probe supported at two ends used for the first TDI-BI heat flow survey offshore Angola, 1997.
![Temperatures at 4 meters depth in sediments at 100 meters water depth in the Gulf of Mexico (unpublished Elva Bruce data).](http://d10j3mvrs1suex.cloudfront.net/s:bzglfiles/u/24802/6753063877423e15cd73f7f009964dc9dfeb681b/original/2155822.jpg/!!/b%3AW1sic2l6ZSIsIjM1MHciXV0%3D/meta%3AeyJzcmNCdWNrZXQiOiJiemdsZmlsZXMifQ%3D%3D.jpg)
Temperatures at 4 meters depth in sediments at 100 meters water depth in the Gulf of Mexico (unpublished Elva Bruce data).
![Texas A&M 'Benthic Lander' adapted to measure metabloc heat flow and oxygen uptake (Zielinski, 1991).](http://d10j3mvrs1suex.cloudfront.net/s:bzglfiles/u/24802/634faf31c0e9e5c92aad76afc69021050ad8c2f6/original/2155785.jpg/!!/b%3AW1sic2l6ZSIsIjM1MHciXV0%3D/meta%3AeyJzcmNCdWNrZXQiOiJiemdsZmlsZXMifQ%3D%3D.jpg)
Texas A&M 'Benthic Lander' adapted to measure metabloc heat flow and oxygen uptake (Zielinski, 1991).
![Heat flow during shallow geotechnical drilling in the Barents Sea north of Norway (Zielinski et al., 1986).](http://d10j3mvrs1suex.cloudfront.net/s:bzglfiles/u/24802/a6ba32c3ede297d05627b36dbaee09267133fd3e/original/2155787.jpg/!!/b%3AW1sic2l6ZSIsIjM1MHciXV0%3D/meta%3AeyJzcmNCdWNrZXQiOiJiemdsZmlsZXMifQ%3D%3D.jpg)
Heat flow during shallow geotechnical drilling in the Barents Sea north of Norway (Zielinski et al., 1986).
![Drs. Jan Szewczyk and Gary Zielinski at the Polish Geological Institute museum in Warsaw, Poland, April 2007 (photo by Robyn Zielinski).](http://d10j3mvrs1suex.cloudfront.net/s:bzglfiles/u/24802/38e4f67dcef076075f21fe27b820d830c9b619f4/original/2870430-orig.jpg/!!/b%3AW1sic2l6ZSIsIjM1MHciXV0%3D/meta%3AeyJzcmNCdWNrZXQiOiJiemdsZmlsZXMifQ%3D%3D.jpg)
Drs. Jan Szewczyk and Gary Zielinski at the Polish Geological Institute museum in Warsaw, Poland, April 2007 (photo by Robyn Zielinski).
![Relative heat flow versus a suite of geochemical data for an active hydrocarbon seep, offshore north Borneo (after Zielinski et al., 2007).](http://d10j3mvrs1suex.cloudfront.net/s:bzglfiles/u/24802/aa416dd0c515687231e9207c43762bc76646287b/original/2370456-orig.jpg/!!/b%3AW1sic2l6ZSIsIjM1MHciXV0%3D/meta%3AeyJzcmNCdWNrZXQiOiJiemdsZmlsZXMifQ%3D%3D.jpg)
Relative heat flow versus a suite of geochemical data for an active hydrocarbon seep, offshore north Borneo (after Zielinski et al., 2007).
![Hydrothermics in the Wyoming Overthrust Belt (after Zielinski et al., 1985) from measurements performed in seismic shot holes. Flow axes coincide with hydrocarbon producing structures.](http://d10j3mvrs1suex.cloudfront.net/s:bzglfiles/u/24802/b1cf9aade01c1f941f51c34235901e993b978a4f/original/2365942-orig.jpg/!!/b%3AW1sic2l6ZSIsIjM1MHciXV0%3D/meta%3AeyJzcmNCdWNrZXQiOiJiemdsZmlsZXMifQ%3D%3D.jpg)
Hydrothermics in the Wyoming Overthrust Belt (after Zielinski et al., 1985) from measurements performed in seismic shot holes. Flow axes coincide with hydrocarbon producing structures.
![Relative heat flow due to fluid upwelling from depth in the Magellan Basin, Tierra del Fuego (after Zielinski and Bruchhausen, 1983).](http://d10j3mvrs1suex.cloudfront.net/s:bzglfiles/u/24802/392e045e15e1ed5884a053d5601ea74fb3cfc17d/original/2365933-orig.jpg/!!/b%3AW1sic2l6ZSIsIjM1MHciXV0%3D/meta%3AeyJzcmNCdWNrZXQiOiJiemdsZmlsZXMifQ%3D%3D.jpg)
Relative heat flow due to fluid upwelling from depth in the Magellan Basin, Tierra del Fuego (after Zielinski and Bruchhausen, 1983).
!['Real time' thermograd data over 2 days showing lowering/raising of heat-flow corer along ship's track, offshore north Borneo 2003. An active seep is indicated in center of record.](http://d10j3mvrs1suex.cloudfront.net/s:bzglfiles/u/24802/218ed7e9f35de761e85902a672216ca24f2663d3/original/2166787.jpg/!!/b%3AW1sic2l6ZSIsIjM1MHciXV0%3D/meta%3AeyJzcmNCdWNrZXQiOiJiemdsZmlsZXMifQ%3D%3D.jpg)
'Real time' thermograd data over 2 days showing lowering/raising of heat-flow corer along ship's track, offshore north Borneo 2003. An active seep is indicated in center of record.
!["Ewing Technique" of heat flow and piston coring pioneered by the Lamont-Doherty Earth Observatory of Columbia University.](http://d10j3mvrs1suex.cloudfront.net/s:bzglfiles/u/24802/4387fbc800c2a67a137ba158a253aa1c116e93c0/original/2155827.jpg/!!/b%3AW1sic2l6ZSIsIjM1MHciXV0%3D/meta%3AeyJzcmNCdWNrZXQiOiJiemdsZmlsZXMifQ%3D%3D.jpg)
"Ewing Technique" of heat flow and piston coring pioneered by the Lamont-Doherty Earth Observatory of Columbia University.
!["Outrigger" thermistor probe supported at two ends used for the first TDI-BI heat flow survey offshore Angola, 1997.](http://d10j3mvrs1suex.cloudfront.net/s:bzglfiles/u/24802/7d65843412589d30758af7b5247c25d0cc5ec01d/original/2155825.jpg/!!/b%3AW1sic2l6ZSIsIjM1MHciXV0%3D/meta%3AeyJzcmNCdWNrZXQiOiJiemdsZmlsZXMifQ%3D%3D.jpg)
"Outrigger" thermistor probe supported at two ends used for the first TDI-BI heat flow survey offshore Angola, 1997.
![Temperatures at 4 meters depth in sediments at 100 meters water depth in the Gulf of Mexico (unpublished Elva Bruce data).](http://d10j3mvrs1suex.cloudfront.net/s:bzglfiles/u/24802/6753063877423e15cd73f7f009964dc9dfeb681b/original/2155822.jpg/!!/b%3AW1sic2l6ZSIsIjM1MHciXV0%3D/meta%3AeyJzcmNCdWNrZXQiOiJiemdsZmlsZXMifQ%3D%3D.jpg)
Temperatures at 4 meters depth in sediments at 100 meters water depth in the Gulf of Mexico (unpublished Elva Bruce data).
![Texas A&M 'Benthic Lander' adapted to measure metabloc heat flow and oxygen uptake (Zielinski, 1991).](http://d10j3mvrs1suex.cloudfront.net/s:bzglfiles/u/24802/634faf31c0e9e5c92aad76afc69021050ad8c2f6/original/2155785.jpg/!!/b%3AW1sic2l6ZSIsIjM1MHciXV0%3D/meta%3AeyJzcmNCdWNrZXQiOiJiemdsZmlsZXMifQ%3D%3D.jpg)
Texas A&M 'Benthic Lander' adapted to measure metabloc heat flow and oxygen uptake (Zielinski, 1991).
![Heat flow during shallow geotechnical drilling in the Barents Sea north of Norway (Zielinski et al., 1986).](http://d10j3mvrs1suex.cloudfront.net/s:bzglfiles/u/24802/a6ba32c3ede297d05627b36dbaee09267133fd3e/original/2155787.jpg/!!/b%3AW1sic2l6ZSIsIjM1MHciXV0%3D/meta%3AeyJzcmNCdWNrZXQiOiJiemdsZmlsZXMifQ%3D%3D.jpg)
Heat flow during shallow geotechnical drilling in the Barents Sea north of Norway (Zielinski et al., 1986).