Composition and stable-isotope geochemistry of natural gases from Kansas, Midcontinent, U.S.A.
Identifieur interne : 002257 ( Main/Exploration ); précédent : 002256; suivant : 002258Composition and stable-isotope geochemistry of natural gases from Kansas, Midcontinent, U.S.A.
Auteurs : P. D. Jenden [États-Unis] ; K. D. Newell [États-Unis] ; I. R. Kaplan [États-Unis] ; W. L. Watney [États-Unis]Source :
- Chemical Geology [ 0009-2541 ] ; 1988.
English descriptors
- Teeft :
- Anadarko, Anadarko basin, Assoc, Bartlesville, Basin, Bennett, Carbon dioxide, Carbon dioxide reduction, Carbonate, Carbonate reservoirs, Central kansas, Central kansas uplift, Cherokee, Cherokee basin, Cherokee group, Chung, Dioxide, Dolomite, Early thermogenic gases, Early thermogenic origin, Eastern kansas, Embayment, Ethane, Forest city, Forest city basin, Forest city basins, Formation water, Geochemistry, Geol, Hugoton, Hugoton embayment, Hugoton field, Hydrocarbon, Isotope, Isotopic, Isotopic composition, Jenden, Kans, Kansas gases, Kaplan, Limestone, Local source rocks, Logsden, Mature source rocks, Mclouth, Methane, Microbial, Microbial carbon dioxide reduction, Microbial gasfield, Microbial methane, Midcontinent, Migration, Mill creek, Mississippian, Mississippian pennsylvanian, Mississippian rocks, Natural gases, Nemaha, Nemaha uplift, Newell, Northern nemaha uplifts, Older rocks, Ordovician, Ordovician gases, Organic geochemistry, Orth, Paleozoic, Pennsylvanian, Pennsylvanian reservoirs, Pennsylvanian rocks, Permian, Petroleum, Petroleum geologists, Pomona, Porous zones, Propane, Province classification, Reflectance, Respec, Sacramento basin, Salina, Salina basin, Sample locations, Sandstone, Sandstone reservoirs, Schoell, Sedgwick basin, Shale, Shallow reservoirs, Silver city, Snake creek field, Source rock maturity, Source rocks, Southwestern kansas, Springs field, Stahl, Stratigraphic, Subpennsylvanian unconformity, Sundberg, Thermogenic, Thermogenic gases, Unconformity, Unpublished data, Uplift, Vitrinite, Watney, Western kansas, Wetness, Wilde, Wilde field.
Abstract
Abstract: More than 28·1012 ft.3 (79·1010 m3) of natural gas and 5.3·109 bbl (8.4·108 m3) of oil have been produced in Kansas, U.S.A., from Paleozoic carbonate and sandstone reservoirs on structural uplifts and shallow embayments along the northern margin of the Anadarko basin. A heavily-explored, geologically well-characterized state, Kansas is an excellent place to study hydrocarbon migration and to test geochemical models for the origin of natural gases.Immature to marginally-mature rocks of eastern Kansas (Cherokee and Forest City basins) produce mixed microbial and thermogenic gases. Gases in this region have wetness = 0.03–51%, methane δ13C = −65 to −43‰ and methane δD = −260 to −150‰. Gases from central and western Kansas (Nemaha uplift to Hugoton embayment) are entirely thermogenic and have wetness =4–51%, methane δ13C = −48 to −39‰ and methane δD = −195 to −140‰. Ethane and propane δ13C-values throughout Kansas vary from −38 to −28‰ and from −35 to −24‰, respectively.Mature thermogenic gas (generated from source rocks in southwestern Kansas and the Anadarko basin with 1.0% ≤ Ro ≤ 1.4%) is recognized throughout the state. Lateral migration into shallow reservoirs on the Central Kansas and northern Nemaha uplifts and in the Cherokee basin probably occurred along basal Pennsylvanian conglomerates and weathered Lower Paleozoic carbonates at the regional sub-Pennsylvanian unconformity. Early thermogenic gas (generated by local source rocks with Ro ≤ 0.7%) is recognized in isolated fields in the Salina and Forest City basins, in Ordovician reservoirs beneath the sub-Pennsylvanian unconformity in the Cherokee basin, and in reservoirs generally above the unconformity in the Cherokee and Sedgwick basins, the eastern Central Kansas uplift and the Hugoton embayment.
Url:
DOI: 10.1016/0009-2541(88)90110-6
Affiliations:
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Watney</name></author></titleStmt><publicationStmt><idno type="wicri:source">ISTEX</idno><idno type="RBID">ISTEX:99A3DC8A5AEEBF7BE7BEC140359371A0C36365EF</idno><date when="1988" year="1988">1988</date><idno type="doi">10.1016/0009-2541(88)90110-6</idno><idno type="url">https://api.istex.fr/ark:/67375/6H6-M79QT8RC-3/fulltext.pdf</idno><idno type="wicri:Area/Istex/Corpus">001837</idno><idno type="wicri:explorRef" wicri:stream="Istex" wicri:step="Corpus" wicri:corpus="ISTEX">001837</idno><idno type="wicri:Area/Istex/Curation">001837</idno><idno type="wicri:Area/Istex/Checkpoint">000F70</idno><idno type="wicri:explorRef" wicri:stream="Istex" wicri:step="Checkpoint">000F70</idno><idno type="wicri:doubleKey">0009-2541:1988:Jenden P:composition:and:stable</idno><idno type="wicri:Area/Main/Merge">002365</idno><idno type="wicri:Area/Main/Curation">002257</idno><idno type="wicri:Area/Main/Exploration">002257</idno></publicationStmt><sourceDesc><biblStruct><analytic><title level="a" type="main" xml:lang="en">Composition and stable-isotope geochemistry of natural gases from Kansas, Midcontinent, U.S.A.</title><author><name sortKey="Jenden, P D" sort="Jenden, P D" uniqKey="Jenden P" first="P. D." last="Jenden">P. D. Jenden</name><affiliation wicri:level="2"><country xml:lang="fr">États-Unis</country><placeName><region type="state">Californie</region></placeName><wicri:cityArea>Global Geochemistry Corporation, Canoga Park</wicri:cityArea></affiliation><affiliation wicri:level="2"><country xml:lang="fr">États-Unis</country><wicri:regionArea>∗Present address: Chevron Oil Field Research Company, La Habra, CA 90633</wicri:regionArea><placeName><region type="state">Californie</region></placeName></affiliation></author><author><name sortKey="Newell, K D" sort="Newell, K D" uniqKey="Newell K" first="K. D." last="Newell">K. D. Newell</name><affiliation wicri:level="2"><country xml:lang="fr">États-Unis</country><placeName><region type="state">Kansas</region></placeName><wicri:cityArea>Kansas Geological Survey, The University of Kansas, Lawrence</wicri:cityArea></affiliation></author><author><name sortKey="Kaplan, I R" sort="Kaplan, I R" uniqKey="Kaplan I" first="I. R." last="Kaplan">I. R. Kaplan</name><affiliation wicri:level="2"><country xml:lang="fr">États-Unis</country><placeName><region type="state">Californie</region></placeName><wicri:cityArea>Global Geochemistry Corporation, Canoga Park</wicri:cityArea></affiliation></author><author><name sortKey="Watney, W L" sort="Watney, W L" uniqKey="Watney W" first="W. L." last="Watney">W. L. Watney</name><affiliation wicri:level="2"><country xml:lang="fr">États-Unis</country><placeName><region type="state">Kansas</region></placeName><wicri:cityArea>Kansas Geological Survey, The University of Kansas, Lawrence</wicri:cityArea></affiliation></author></analytic><monogr></monogr><series><title level="j">Chemical Geology</title><title level="j" type="abbrev">CHEMGE</title><idno type="ISSN">0009-2541</idno><imprint><publisher>ELSEVIER</publisher><date type="published" when="1988">1988</date><biblScope unit="volume">71</biblScope><biblScope unit="issue">1–3</biblScope><biblScope unit="page" from="117">117</biblScope><biblScope unit="page" to="147">147</biblScope></imprint><idno type="ISSN">0009-2541</idno></series></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">0009-2541</idno></seriesStmt></fileDesc><profileDesc><textClass><keywords scheme="Teeft" xml:lang="en"><term>Anadarko</term><term>Anadarko basin</term><term>Assoc</term><term>Bartlesville</term><term>Basin</term><term>Bennett</term><term>Carbon dioxide</term><term>Carbon dioxide reduction</term><term>Carbonate</term><term>Carbonate reservoirs</term><term>Central kansas</term><term>Central kansas uplift</term><term>Cherokee</term><term>Cherokee basin</term><term>Cherokee group</term><term>Chung</term><term>Dioxide</term><term>Dolomite</term><term>Early thermogenic gases</term><term>Early thermogenic origin</term><term>Eastern kansas</term><term>Embayment</term><term>Ethane</term><term>Forest city</term><term>Forest city basin</term><term>Forest city basins</term><term>Formation water</term><term>Geochemistry</term><term>Geol</term><term>Hugoton</term><term>Hugoton embayment</term><term>Hugoton field</term><term>Hydrocarbon</term><term>Isotope</term><term>Isotopic</term><term>Isotopic composition</term><term>Jenden</term><term>Kans</term><term>Kansas gases</term><term>Kaplan</term><term>Limestone</term><term>Local source rocks</term><term>Logsden</term><term>Mature source rocks</term><term>Mclouth</term><term>Methane</term><term>Microbial</term><term>Microbial carbon dioxide reduction</term><term>Microbial gasfield</term><term>Microbial methane</term><term>Midcontinent</term><term>Migration</term><term>Mill creek</term><term>Mississippian</term><term>Mississippian pennsylvanian</term><term>Mississippian rocks</term><term>Natural gases</term><term>Nemaha</term><term>Nemaha uplift</term><term>Newell</term><term>Northern nemaha uplifts</term><term>Older rocks</term><term>Ordovician</term><term>Ordovician gases</term><term>Organic geochemistry</term><term>Orth</term><term>Paleozoic</term><term>Pennsylvanian</term><term>Pennsylvanian reservoirs</term><term>Pennsylvanian rocks</term><term>Permian</term><term>Petroleum</term><term>Petroleum geologists</term><term>Pomona</term><term>Porous zones</term><term>Propane</term><term>Province classification</term><term>Reflectance</term><term>Respec</term><term>Sacramento basin</term><term>Salina</term><term>Salina basin</term><term>Sample locations</term><term>Sandstone</term><term>Sandstone reservoirs</term><term>Schoell</term><term>Sedgwick basin</term><term>Shale</term><term>Shallow reservoirs</term><term>Silver city</term><term>Snake creek field</term><term>Source rock maturity</term><term>Source rocks</term><term>Southwestern kansas</term><term>Springs field</term><term>Stahl</term><term>Stratigraphic</term><term>Subpennsylvanian unconformity</term><term>Sundberg</term><term>Thermogenic</term><term>Thermogenic gases</term><term>Unconformity</term><term>Unpublished data</term><term>Uplift</term><term>Vitrinite</term><term>Watney</term><term>Western kansas</term><term>Wetness</term><term>Wilde</term><term>Wilde field</term></keywords></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">Abstract: More than 28·1012 ft.3 (79·1010 m3) of natural gas and 5.3·109 bbl (8.4·108 m3) of oil have been produced in Kansas, U.S.A., from Paleozoic carbonate and sandstone reservoirs on structural uplifts and shallow embayments along the northern margin of the Anadarko basin. A heavily-explored, geologically well-characterized state, Kansas is an excellent place to study hydrocarbon migration and to test geochemical models for the origin of natural gases.Immature to marginally-mature rocks of eastern Kansas (Cherokee and Forest City basins) produce mixed microbial and thermogenic gases. Gases in this region have wetness = 0.03–51%, methane δ13C = −65 to −43‰ and methane δD = −260 to −150‰. Gases from central and western Kansas (Nemaha uplift to Hugoton embayment) are entirely thermogenic and have wetness =4–51%, methane δ13C = −48 to −39‰ and methane δD = −195 to −140‰. Ethane and propane δ13C-values throughout Kansas vary from −38 to −28‰ and from −35 to −24‰, respectively.Mature thermogenic gas (generated from source rocks in southwestern Kansas and the Anadarko basin with 1.0% ≤ Ro ≤ 1.4%) is recognized throughout the state. Lateral migration into shallow reservoirs on the Central Kansas and northern Nemaha uplifts and in the Cherokee basin probably occurred along basal Pennsylvanian conglomerates and weathered Lower Paleozoic carbonates at the regional sub-Pennsylvanian unconformity. Early thermogenic gas (generated by local source rocks with Ro ≤ 0.7%) is recognized in isolated fields in the Salina and Forest City basins, in Ordovician reservoirs beneath the sub-Pennsylvanian unconformity in the Cherokee basin, and in reservoirs generally above the unconformity in the Cherokee and Sedgwick basins, the eastern Central Kansas uplift and the Hugoton embayment.</div></front></TEI><affiliations><list><country><li>États-Unis</li></country><region><li>Californie</li><li>Kansas</li></region></list><tree><country name="États-Unis"><region name="Californie"><name sortKey="Jenden, P D" sort="Jenden, P D" uniqKey="Jenden P" first="P. D." last="Jenden">P. D. Jenden</name></region><name sortKey="Jenden, P D" sort="Jenden, P D" uniqKey="Jenden P" first="P. D." last="Jenden">P. D. Jenden</name><name sortKey="Kaplan, I R" sort="Kaplan, I R" uniqKey="Kaplan I" first="I. R." last="Kaplan">I. R. Kaplan</name><name sortKey="Newell, K D" sort="Newell, K D" uniqKey="Newell K" first="K. D." last="Newell">K. D. Newell</name><name sortKey="Watney, W L" sort="Watney, W L" uniqKey="Watney W" first="W. L." last="Watney">W. L. Watney</name></country></tree></affiliations></record>Pour manipuler ce document sous Unix (Dilib)
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