Natural gas origins of large and medium-scale gas fields in China sedimentary basins
Abstract China sedimentary basins present abundant natural gas resource thanks to its unique geological settings. Marine highly-matured hydrocarbon source rocks, widespread coal-measure strata and low temperature Quaternary saline strata, etc., indicate the wide foreground of China natural gas resou...
Ausführliche Beschreibung
Autor*in: |
Zhang, ShuiChang [verfasserIn] Zhu, GuangYou [verfasserIn] |
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Format: |
E-Artikel |
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Sprache: |
Englisch |
Erschienen: |
2008 |
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Schlagwörter: |
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Übergeordnetes Werk: |
Enthalten in: Science in China - Heidelberg : Springer, 1997, 51(2008), Suppl 1 vom: Mai, Seite 1-13 |
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Übergeordnetes Werk: |
volume:51 ; year:2008 ; number:Suppl 1 ; month:05 ; pages:1-13 |
Links: |
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DOI / URN: |
10.1007/s11430-008-5013-1 |
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Katalog-ID: |
SPR019228910 |
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520 | |a Abstract China sedimentary basins present abundant natural gas resource thanks to its unique geological settings. Marine highly-matured hydrocarbon source rocks, widespread coal-measure strata and low temperature Quaternary saline strata, etc., indicate the wide foreground of China natural gas resources. Up to now, most of the petroliferous basins have been discovered to have wholesale natural gas accumulation from Precambrian, Paleozoic, Mesozoic to Cenozoic in the east, the central, the west and the coast of China. These large and medium-scale gas reservoirs are mainly composed of hydrocarbon gas with big dry coefficient, tiny non-hydrocarbon, wide carbon isotope distribution and varying origin types, the hydrocarbon gas includes coal-formed gas, oil-formed gas, biogenic gas and inorganic gas, etc. Coal-formed gas is the main type of China natural gas resources, in particular several explored large-scale gas fields (>100 billion cubic meter) of Kela 2, Sulige and Daniudi, etc., they all belong to coal-formed gas fields or the gas fields consisting mostly of coal-formed gas. Oil-formed gas is also abundant in China marine basins, for example marine natural gas of Sichuan Basin generated from crude oil cracking gas. Primary and secondary biogenic gas fields were discovered respectively in the Qaidam Basin and Western Slope of Songliao Basin. In addition, inorganic gases are mainly distributed in the eastern China, in particular the Songliao Basin with abundant carbon dioxide accumulation, indicating that the eastern China present large exploration potential of inorganic gas. | ||
650 | 4 | |a natural gas origin |7 (dpeaa)DE-He213 | |
650 | 4 | |a sedimentary basin |7 (dpeaa)DE-He213 | |
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700 | 1 | |a Zhu, GuangYou |e verfasserin |4 aut | |
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10.1007/s11430-008-5013-1 doi (DE-627)SPR019228910 (SPR)s11430-008-5013-1-e DE-627 ger DE-627 rakwb eng 550 ASE 38.00 bkl Zhang, ShuiChang verfasserin aut Natural gas origins of large and medium-scale gas fields in China sedimentary basins 2008 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract China sedimentary basins present abundant natural gas resource thanks to its unique geological settings. Marine highly-matured hydrocarbon source rocks, widespread coal-measure strata and low temperature Quaternary saline strata, etc., indicate the wide foreground of China natural gas resources. Up to now, most of the petroliferous basins have been discovered to have wholesale natural gas accumulation from Precambrian, Paleozoic, Mesozoic to Cenozoic in the east, the central, the west and the coast of China. These large and medium-scale gas reservoirs are mainly composed of hydrocarbon gas with big dry coefficient, tiny non-hydrocarbon, wide carbon isotope distribution and varying origin types, the hydrocarbon gas includes coal-formed gas, oil-formed gas, biogenic gas and inorganic gas, etc. Coal-formed gas is the main type of China natural gas resources, in particular several explored large-scale gas fields (>100 billion cubic meter) of Kela 2, Sulige and Daniudi, etc., they all belong to coal-formed gas fields or the gas fields consisting mostly of coal-formed gas. Oil-formed gas is also abundant in China marine basins, for example marine natural gas of Sichuan Basin generated from crude oil cracking gas. Primary and secondary biogenic gas fields were discovered respectively in the Qaidam Basin and Western Slope of Songliao Basin. In addition, inorganic gases are mainly distributed in the eastern China, in particular the Songliao Basin with abundant carbon dioxide accumulation, indicating that the eastern China present large exploration potential of inorganic gas. natural gas origin (dpeaa)DE-He213 sedimentary basin (dpeaa)DE-He213 large and medium-scale gas field (dpeaa)DE-He213 Zhu, GuangYou verfasserin aut Enthalten in Science in China Heidelberg : Springer, 1997 51(2008), Suppl 1 vom: Mai, Seite 1-13 (DE-627)385614748 (DE-600)2142896-7 1862-2801 nnns volume:51 year:2008 number:Suppl 1 month:05 pages:1-13 https://dx.doi.org/10.1007/s11430-008-5013-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_266 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.00 ASE AR 51 2008 Suppl 1 05 1-13 |
spelling |
10.1007/s11430-008-5013-1 doi (DE-627)SPR019228910 (SPR)s11430-008-5013-1-e DE-627 ger DE-627 rakwb eng 550 ASE 38.00 bkl Zhang, ShuiChang verfasserin aut Natural gas origins of large and medium-scale gas fields in China sedimentary basins 2008 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract China sedimentary basins present abundant natural gas resource thanks to its unique geological settings. Marine highly-matured hydrocarbon source rocks, widespread coal-measure strata and low temperature Quaternary saline strata, etc., indicate the wide foreground of China natural gas resources. Up to now, most of the petroliferous basins have been discovered to have wholesale natural gas accumulation from Precambrian, Paleozoic, Mesozoic to Cenozoic in the east, the central, the west and the coast of China. These large and medium-scale gas reservoirs are mainly composed of hydrocarbon gas with big dry coefficient, tiny non-hydrocarbon, wide carbon isotope distribution and varying origin types, the hydrocarbon gas includes coal-formed gas, oil-formed gas, biogenic gas and inorganic gas, etc. Coal-formed gas is the main type of China natural gas resources, in particular several explored large-scale gas fields (>100 billion cubic meter) of Kela 2, Sulige and Daniudi, etc., they all belong to coal-formed gas fields or the gas fields consisting mostly of coal-formed gas. Oil-formed gas is also abundant in China marine basins, for example marine natural gas of Sichuan Basin generated from crude oil cracking gas. Primary and secondary biogenic gas fields were discovered respectively in the Qaidam Basin and Western Slope of Songliao Basin. In addition, inorganic gases are mainly distributed in the eastern China, in particular the Songliao Basin with abundant carbon dioxide accumulation, indicating that the eastern China present large exploration potential of inorganic gas. natural gas origin (dpeaa)DE-He213 sedimentary basin (dpeaa)DE-He213 large and medium-scale gas field (dpeaa)DE-He213 Zhu, GuangYou verfasserin aut Enthalten in Science in China Heidelberg : Springer, 1997 51(2008), Suppl 1 vom: Mai, Seite 1-13 (DE-627)385614748 (DE-600)2142896-7 1862-2801 nnns volume:51 year:2008 number:Suppl 1 month:05 pages:1-13 https://dx.doi.org/10.1007/s11430-008-5013-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_266 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.00 ASE AR 51 2008 Suppl 1 05 1-13 |
allfields_unstemmed |
10.1007/s11430-008-5013-1 doi (DE-627)SPR019228910 (SPR)s11430-008-5013-1-e DE-627 ger DE-627 rakwb eng 550 ASE 38.00 bkl Zhang, ShuiChang verfasserin aut Natural gas origins of large and medium-scale gas fields in China sedimentary basins 2008 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract China sedimentary basins present abundant natural gas resource thanks to its unique geological settings. Marine highly-matured hydrocarbon source rocks, widespread coal-measure strata and low temperature Quaternary saline strata, etc., indicate the wide foreground of China natural gas resources. Up to now, most of the petroliferous basins have been discovered to have wholesale natural gas accumulation from Precambrian, Paleozoic, Mesozoic to Cenozoic in the east, the central, the west and the coast of China. These large and medium-scale gas reservoirs are mainly composed of hydrocarbon gas with big dry coefficient, tiny non-hydrocarbon, wide carbon isotope distribution and varying origin types, the hydrocarbon gas includes coal-formed gas, oil-formed gas, biogenic gas and inorganic gas, etc. Coal-formed gas is the main type of China natural gas resources, in particular several explored large-scale gas fields (>100 billion cubic meter) of Kela 2, Sulige and Daniudi, etc., they all belong to coal-formed gas fields or the gas fields consisting mostly of coal-formed gas. Oil-formed gas is also abundant in China marine basins, for example marine natural gas of Sichuan Basin generated from crude oil cracking gas. Primary and secondary biogenic gas fields were discovered respectively in the Qaidam Basin and Western Slope of Songliao Basin. In addition, inorganic gases are mainly distributed in the eastern China, in particular the Songliao Basin with abundant carbon dioxide accumulation, indicating that the eastern China present large exploration potential of inorganic gas. natural gas origin (dpeaa)DE-He213 sedimentary basin (dpeaa)DE-He213 large and medium-scale gas field (dpeaa)DE-He213 Zhu, GuangYou verfasserin aut Enthalten in Science in China Heidelberg : Springer, 1997 51(2008), Suppl 1 vom: Mai, Seite 1-13 (DE-627)385614748 (DE-600)2142896-7 1862-2801 nnns volume:51 year:2008 number:Suppl 1 month:05 pages:1-13 https://dx.doi.org/10.1007/s11430-008-5013-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_266 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.00 ASE AR 51 2008 Suppl 1 05 1-13 |
allfieldsGer |
10.1007/s11430-008-5013-1 doi (DE-627)SPR019228910 (SPR)s11430-008-5013-1-e DE-627 ger DE-627 rakwb eng 550 ASE 38.00 bkl Zhang, ShuiChang verfasserin aut Natural gas origins of large and medium-scale gas fields in China sedimentary basins 2008 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract China sedimentary basins present abundant natural gas resource thanks to its unique geological settings. Marine highly-matured hydrocarbon source rocks, widespread coal-measure strata and low temperature Quaternary saline strata, etc., indicate the wide foreground of China natural gas resources. Up to now, most of the petroliferous basins have been discovered to have wholesale natural gas accumulation from Precambrian, Paleozoic, Mesozoic to Cenozoic in the east, the central, the west and the coast of China. These large and medium-scale gas reservoirs are mainly composed of hydrocarbon gas with big dry coefficient, tiny non-hydrocarbon, wide carbon isotope distribution and varying origin types, the hydrocarbon gas includes coal-formed gas, oil-formed gas, biogenic gas and inorganic gas, etc. Coal-formed gas is the main type of China natural gas resources, in particular several explored large-scale gas fields (>100 billion cubic meter) of Kela 2, Sulige and Daniudi, etc., they all belong to coal-formed gas fields or the gas fields consisting mostly of coal-formed gas. Oil-formed gas is also abundant in China marine basins, for example marine natural gas of Sichuan Basin generated from crude oil cracking gas. Primary and secondary biogenic gas fields were discovered respectively in the Qaidam Basin and Western Slope of Songliao Basin. In addition, inorganic gases are mainly distributed in the eastern China, in particular the Songliao Basin with abundant carbon dioxide accumulation, indicating that the eastern China present large exploration potential of inorganic gas. natural gas origin (dpeaa)DE-He213 sedimentary basin (dpeaa)DE-He213 large and medium-scale gas field (dpeaa)DE-He213 Zhu, GuangYou verfasserin aut Enthalten in Science in China Heidelberg : Springer, 1997 51(2008), Suppl 1 vom: Mai, Seite 1-13 (DE-627)385614748 (DE-600)2142896-7 1862-2801 nnns volume:51 year:2008 number:Suppl 1 month:05 pages:1-13 https://dx.doi.org/10.1007/s11430-008-5013-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_266 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.00 ASE AR 51 2008 Suppl 1 05 1-13 |
allfieldsSound |
10.1007/s11430-008-5013-1 doi (DE-627)SPR019228910 (SPR)s11430-008-5013-1-e DE-627 ger DE-627 rakwb eng 550 ASE 38.00 bkl Zhang, ShuiChang verfasserin aut Natural gas origins of large and medium-scale gas fields in China sedimentary basins 2008 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract China sedimentary basins present abundant natural gas resource thanks to its unique geological settings. Marine highly-matured hydrocarbon source rocks, widespread coal-measure strata and low temperature Quaternary saline strata, etc., indicate the wide foreground of China natural gas resources. Up to now, most of the petroliferous basins have been discovered to have wholesale natural gas accumulation from Precambrian, Paleozoic, Mesozoic to Cenozoic in the east, the central, the west and the coast of China. These large and medium-scale gas reservoirs are mainly composed of hydrocarbon gas with big dry coefficient, tiny non-hydrocarbon, wide carbon isotope distribution and varying origin types, the hydrocarbon gas includes coal-formed gas, oil-formed gas, biogenic gas and inorganic gas, etc. Coal-formed gas is the main type of China natural gas resources, in particular several explored large-scale gas fields (>100 billion cubic meter) of Kela 2, Sulige and Daniudi, etc., they all belong to coal-formed gas fields or the gas fields consisting mostly of coal-formed gas. Oil-formed gas is also abundant in China marine basins, for example marine natural gas of Sichuan Basin generated from crude oil cracking gas. Primary and secondary biogenic gas fields were discovered respectively in the Qaidam Basin and Western Slope of Songliao Basin. In addition, inorganic gases are mainly distributed in the eastern China, in particular the Songliao Basin with abundant carbon dioxide accumulation, indicating that the eastern China present large exploration potential of inorganic gas. natural gas origin (dpeaa)DE-He213 sedimentary basin (dpeaa)DE-He213 large and medium-scale gas field (dpeaa)DE-He213 Zhu, GuangYou verfasserin aut Enthalten in Science in China Heidelberg : Springer, 1997 51(2008), Suppl 1 vom: Mai, Seite 1-13 (DE-627)385614748 (DE-600)2142896-7 1862-2801 nnns volume:51 year:2008 number:Suppl 1 month:05 pages:1-13 https://dx.doi.org/10.1007/s11430-008-5013-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_266 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.00 ASE AR 51 2008 Suppl 1 05 1-13 |
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Marine highly-matured hydrocarbon source rocks, widespread coal-measure strata and low temperature Quaternary saline strata, etc., indicate the wide foreground of China natural gas resources. Up to now, most of the petroliferous basins have been discovered to have wholesale natural gas accumulation from Precambrian, Paleozoic, Mesozoic to Cenozoic in the east, the central, the west and the coast of China. These large and medium-scale gas reservoirs are mainly composed of hydrocarbon gas with big dry coefficient, tiny non-hydrocarbon, wide carbon isotope distribution and varying origin types, the hydrocarbon gas includes coal-formed gas, oil-formed gas, biogenic gas and inorganic gas, etc. Coal-formed gas is the main type of China natural gas resources, in particular several explored large-scale gas fields (>100 billion cubic meter) of Kela 2, Sulige and Daniudi, etc., they all belong to coal-formed gas fields or the gas fields consisting mostly of coal-formed gas. Oil-formed gas is also abundant in China marine basins, for example marine natural gas of Sichuan Basin generated from crude oil cracking gas. Primary and secondary biogenic gas fields were discovered respectively in the Qaidam Basin and Western Slope of Songliao Basin. 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author |
Zhang, ShuiChang |
spellingShingle |
Zhang, ShuiChang ddc 550 bkl 38.00 misc natural gas origin misc sedimentary basin misc large and medium-scale gas field Natural gas origins of large and medium-scale gas fields in China sedimentary basins |
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550 ASE 38.00 bkl Natural gas origins of large and medium-scale gas fields in China sedimentary basins natural gas origin (dpeaa)DE-He213 sedimentary basin (dpeaa)DE-He213 large and medium-scale gas field (dpeaa)DE-He213 |
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ddc 550 bkl 38.00 misc natural gas origin misc sedimentary basin misc large and medium-scale gas field |
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Natural gas origins of large and medium-scale gas fields in China sedimentary basins |
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Natural gas origins of large and medium-scale gas fields in China sedimentary basins |
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Zhang, ShuiChang |
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Science in China |
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natural gas origins of large and medium-scale gas fields in china sedimentary basins |
title_auth |
Natural gas origins of large and medium-scale gas fields in China sedimentary basins |
abstract |
Abstract China sedimentary basins present abundant natural gas resource thanks to its unique geological settings. Marine highly-matured hydrocarbon source rocks, widespread coal-measure strata and low temperature Quaternary saline strata, etc., indicate the wide foreground of China natural gas resources. Up to now, most of the petroliferous basins have been discovered to have wholesale natural gas accumulation from Precambrian, Paleozoic, Mesozoic to Cenozoic in the east, the central, the west and the coast of China. These large and medium-scale gas reservoirs are mainly composed of hydrocarbon gas with big dry coefficient, tiny non-hydrocarbon, wide carbon isotope distribution and varying origin types, the hydrocarbon gas includes coal-formed gas, oil-formed gas, biogenic gas and inorganic gas, etc. Coal-formed gas is the main type of China natural gas resources, in particular several explored large-scale gas fields (>100 billion cubic meter) of Kela 2, Sulige and Daniudi, etc., they all belong to coal-formed gas fields or the gas fields consisting mostly of coal-formed gas. Oil-formed gas is also abundant in China marine basins, for example marine natural gas of Sichuan Basin generated from crude oil cracking gas. Primary and secondary biogenic gas fields were discovered respectively in the Qaidam Basin and Western Slope of Songliao Basin. In addition, inorganic gases are mainly distributed in the eastern China, in particular the Songliao Basin with abundant carbon dioxide accumulation, indicating that the eastern China present large exploration potential of inorganic gas. |
abstractGer |
Abstract China sedimentary basins present abundant natural gas resource thanks to its unique geological settings. Marine highly-matured hydrocarbon source rocks, widespread coal-measure strata and low temperature Quaternary saline strata, etc., indicate the wide foreground of China natural gas resources. Up to now, most of the petroliferous basins have been discovered to have wholesale natural gas accumulation from Precambrian, Paleozoic, Mesozoic to Cenozoic in the east, the central, the west and the coast of China. These large and medium-scale gas reservoirs are mainly composed of hydrocarbon gas with big dry coefficient, tiny non-hydrocarbon, wide carbon isotope distribution and varying origin types, the hydrocarbon gas includes coal-formed gas, oil-formed gas, biogenic gas and inorganic gas, etc. Coal-formed gas is the main type of China natural gas resources, in particular several explored large-scale gas fields (>100 billion cubic meter) of Kela 2, Sulige and Daniudi, etc., they all belong to coal-formed gas fields or the gas fields consisting mostly of coal-formed gas. Oil-formed gas is also abundant in China marine basins, for example marine natural gas of Sichuan Basin generated from crude oil cracking gas. Primary and secondary biogenic gas fields were discovered respectively in the Qaidam Basin and Western Slope of Songliao Basin. In addition, inorganic gases are mainly distributed in the eastern China, in particular the Songliao Basin with abundant carbon dioxide accumulation, indicating that the eastern China present large exploration potential of inorganic gas. |
abstract_unstemmed |
Abstract China sedimentary basins present abundant natural gas resource thanks to its unique geological settings. Marine highly-matured hydrocarbon source rocks, widespread coal-measure strata and low temperature Quaternary saline strata, etc., indicate the wide foreground of China natural gas resources. Up to now, most of the petroliferous basins have been discovered to have wholesale natural gas accumulation from Precambrian, Paleozoic, Mesozoic to Cenozoic in the east, the central, the west and the coast of China. These large and medium-scale gas reservoirs are mainly composed of hydrocarbon gas with big dry coefficient, tiny non-hydrocarbon, wide carbon isotope distribution and varying origin types, the hydrocarbon gas includes coal-formed gas, oil-formed gas, biogenic gas and inorganic gas, etc. Coal-formed gas is the main type of China natural gas resources, in particular several explored large-scale gas fields (>100 billion cubic meter) of Kela 2, Sulige and Daniudi, etc., they all belong to coal-formed gas fields or the gas fields consisting mostly of coal-formed gas. Oil-formed gas is also abundant in China marine basins, for example marine natural gas of Sichuan Basin generated from crude oil cracking gas. Primary and secondary biogenic gas fields were discovered respectively in the Qaidam Basin and Western Slope of Songliao Basin. In addition, inorganic gases are mainly distributed in the eastern China, in particular the Songliao Basin with abundant carbon dioxide accumulation, indicating that the eastern China present large exploration potential of inorganic gas. |
collection_details |
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container_issue |
Suppl 1 |
title_short |
Natural gas origins of large and medium-scale gas fields in China sedimentary basins |
url |
https://dx.doi.org/10.1007/s11430-008-5013-1 |
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true |
author2 |
Zhu, GuangYou |
author2Str |
Zhu, GuangYou |
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385614748 |
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doi_str |
10.1007/s11430-008-5013-1 |
up_date |
2024-07-04T00:43:28.148Z |
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Marine highly-matured hydrocarbon source rocks, widespread coal-measure strata and low temperature Quaternary saline strata, etc., indicate the wide foreground of China natural gas resources. Up to now, most of the petroliferous basins have been discovered to have wholesale natural gas accumulation from Precambrian, Paleozoic, Mesozoic to Cenozoic in the east, the central, the west and the coast of China. These large and medium-scale gas reservoirs are mainly composed of hydrocarbon gas with big dry coefficient, tiny non-hydrocarbon, wide carbon isotope distribution and varying origin types, the hydrocarbon gas includes coal-formed gas, oil-formed gas, biogenic gas and inorganic gas, etc. Coal-formed gas is the main type of China natural gas resources, in particular several explored large-scale gas fields (>100 billion cubic meter) of Kela 2, Sulige and Daniudi, etc., they all belong to coal-formed gas fields or the gas fields consisting mostly of coal-formed gas. 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score |
7.3988647 |