Changes

file:oiloil-and-oilsource-rock-correlations_fig8-5.png|{{figure number|1}}Gas chromatogram of a high-wax oil of terrestrial origin with an odd-carbon preference in the wax region and a high pristane-phytane ratio typical of coaly or certain nearshore aquatic environments. From Robinson;<ref name=ch08r46>Robinson, K., M., 1987, An overview of [[source rock]]s and oils in Indonesia: Proceedings, Indonesian Petroleum Association 16th Annual Convention, p. 97–122.</ref> reprinted with permission from the Indonesian Petroleum Association.

file:oiloil-and-oilsource-rock-correlations_fig8-5.png|{{figure number|1}}Gas chromatogram of a high-wax oil of terrestrial origin with an odd-carbon preference in the wax region and a high pristane-phytane ratio typical of coaly or certain nearshore aquatic environments. From Robinson;<ref name=ch08r46>Robinson, K., M., 1987, An overview of [[source rock]]s and oils in Indonesia: Proceedings, Indonesian Petroleum Association 16th Annual Convention, p. 97–122.</ref> reprinted with permission from the Indonesian Petroleum Association.

file:oiloil-and-oilsource-rock-correlations_fig8-6.png|{{figure number|2}}Gas chromatogram of an extremely waxy oil from the Paradox basin, Utah. Copyright: Unocal.

file:oiloil-and-oilsource-rock-correlations_fig8-6.png|{{figure number|2}}Gas chromatogram of an extremely waxy oil from the Paradox basin, Utah. Copyright: Unocal.

</gallery>

</gallery>

===Example: oil of terrestrial origin===

===Example: oil of terrestrial origin===

===Example: oil of marine algal origin===

===Example: oil of marine algal origin===

[[:file:oiloil-and-oilsource-rock-correlations_fig8-7.png|Figure 3]] shows a gas chromatogram of a low-wax oil derived from typical marine algae. Pristane-phytane ratios for such oils tend to be slightly above 1.0. This Alaskan oil was derived from a source rock containing predominantly marine algal organic matter.

[[:file:oiloil-and-oilsource-rock-correlations_fig8-7.png|Figure 3]] shows a gas chromatogram of a low-wax oil derived from typical marine algae. Pristane-phytane ratios for such oils tend to be slightly above 1.0. This Alaskan oil was derived from a source rock containing predominantly marine algal organic matter.

===Example: Oil derived from ''G. prisca''===

===Example: Oil derived from ''G. prisca''===

[[file:oiloil-and-oilsource-rock-correlations_fig8-8.png|thumb|{{figure number|4}}From Hatch et al.<ref name=ch08r18 />); reprinted with permission from AAPG.]]

[[file:oiloil-and-oilsource-rock-correlations_fig8-8.png|thumb|{{figure number|4}}Gas chromatogram of saturates from an Ordovician-sourced oil from the Illinois basin. From Hatch et al.<ref name=ch08r18 />); reprinted with permission from AAPG.]]

[[:file:oiloil-and-oilsource-rock-correlations_fig8-8.png|figure 4]] is a gas chromatogram of saturates from an Ordovician-sourced oil from the Illinois basin. It shows a low-wax oil derived primarily from the primitive organism ''Gloeocapsamorpha prisca''. Samples derived from ''G. prisca'' show strong odd-carbon preferences up to ''n''-C₁₉, and have very low concentrations of both pristane and phytane.<ref name=ch08r44>Reed, J., D., Illich, H., A., Horsfield, B., 1986, Biochemical evolutionary significance of Ordovician oils and their sources: Organic Geochemistry, vol. 10, p. 347–358., 10., 1016/0146-6380(86)90035-5</ref><ref name=ch08r28>Longman, M., W., Palmer, S., E., 1987, [http://archives.datapages.com/data/bulletns/1986-87/data/pg/0071/0008/0900/0938.htm Organic geochemistry of mid-continent middle and late Ordovician oils]: AAPG Bulletin, vol. 71, p. 938–950.</ref><ref name=ch08r18>Hatch, J., R., Risatti, J., B., King, J., D., 1990, [http://archives.datapages.com/data/specpubs/basinar3/data/a134/a134/0001/0400/0403.htm Geochemistry of Illinois basin oils and hydrocarbon source rocks], in Leighton, M., W., Kolata, D., R., Oltz, D., F., Eidel, J., J., eds., Interior cratonic basins: [http://store.aapg.org/detail.aspx?id=1182 AAPG Memoir 51], p. 403–423.</ref><ref name=ch08r17>Guthrie, J., M., Pratt, L., M., 1995, [http://archives.datapages.com/data/bulletns/1994-96/data/pg/0079/0011/1600/1631.htm Geochemical character and origin of oils in Ordovician reservoir rock, Illinois and Indiana]: AAPG Bulletin, vol. 79, p. 1631–1649.</ref>

[[:file:oiloil-and-oilsource-rock-correlations_fig8-8.png|figure 4]] is a gas chromatogram of saturates from an Ordovician-sourced oil from the Illinois basin. It shows a low-wax oil derived primarily from the primitive organism ''Gloeocapsamorpha prisca''. Samples derived from ''G. prisca'' show strong odd-carbon preferences up to ''n''-C₁₉, and have very low concentrations of both pristane and phytane.<ref name=ch08r44>Reed, J., D., Illich, H., A., Horsfield, B., 1986, Biochemical evolutionary significance of Ordovician oils and their sources: Organic Geochemistry, vol. 10, p. 347–358., 10., 1016/0146-6380(86)90035-5</ref><ref name=ch08r28>Longman, M., W., Palmer, S., E., 1987, [http://archives.datapages.com/data/bulletns/1986-87/data/pg/0071/0008/0900/0938.htm Organic geochemistry of mid-continent middle and late Ordovician oils]: AAPG Bulletin, vol. 71, p. 938–950.</ref><ref name=ch08r18>Hatch, J., R., Risatti, J., B., King, J., D., 1990, [http://archives.datapages.com/data/specpubs/basinar3/data/a134/a134/0001/0400/0403.htm Geochemistry of Illinois basin oils and hydrocarbon source rocks], in Leighton, M., W., Kolata, D., R., Oltz, D., F., Eidel, J., J., eds., Interior cratonic basins: [http://store.aapg.org/detail.aspx?id=1182 AAPG Memoir 51], p. 403–423.</ref><ref name=ch08r17>Guthrie, J., M., Pratt, L., M., 1995, [http://archives.datapages.com/data/bulletns/1994-96/data/pg/0079/0011/1600/1631.htm Geochemical character and origin of oils in Ordovician reservoir rock, Illinois and Indiana]: AAPG Bulletin, vol. 79, p. 1631–1649.</ref>