Hydrocarbon accumulation in network and its application in the continental rift basin
Abstract The concept of hydrocarbon accumulation in network was presented on basis of the overall analysis of the formation and evolution characteristics of the continental faulted basin and of the systemic research on the major controlling factors on the hydrocarbon accumulation. The hydrocarbon ac...
Ausführliche Beschreibung
Autor*in: |
Pang, XiongQi [verfasserIn] Chen, DongXia [verfasserIn] Zhang, ShanWen [verfasserIn] Hao, Fang [verfasserIn] Liu, Zheng [verfasserIn] Liu, KeYu [verfasserIn] Song, GuoQi [verfasserIn] Wang, YongShi [verfasserIn] Luo, XiaoRong [verfasserIn] Wu, XiaoChun [verfasserIn] |
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Format: |
E-Artikel |
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Sprache: |
Englisch |
Erschienen: |
2008 |
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Schlagwörter: |
hydrocarbon accumulation theory |
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Übergeordnetes Werk: |
Enthalten in: Science in China - Heidelberg : Springer, 1997, 51(2008), Suppl 2 vom: Okt., Seite 88-100 |
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Übergeordnetes Werk: |
volume:51 ; year:2008 ; number:Suppl 2 ; month:10 ; pages:88-100 |
Links: |
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DOI / URN: |
10.1007/s11430-008-6026-5 |
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Katalog-ID: |
SPR019229267 |
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520 | |a Abstract The concept of hydrocarbon accumulation in network was presented on basis of the overall analysis of the formation and evolution characteristics of the continental faulted basin and of the systemic research on the major controlling factors on the hydrocarbon accumulation. The hydrocarbon accumulation in network can be defined as hydrocarbon accumulation in a three-dimensional network system which is constituted by the hydrocarbon migration passages under multiple dynamics, following the hydrocarbon generation from source rocks. The research shows that the hydrocarbon accumulation in network is composed of four elements, i.e., hydrocarbon source (source rock kitchen), hydrocarbon accumulation terminal (trap), network pathway connecting source and terminal (transporting system), and network potential driving hydrocarbon migration in the network pathway (migration dynamics). Compared with other networks, hydrocarbon accumulation in network has three basic characteristics: the irreversible geological process of material and information flow in the network; the loss of material and information in the flow process in the network; the multiple dynamics in the flow process. Interaction of all the elements in the geological process can be called hydrocarbon accumulation in network. There are three basic models for hydrocarbon accumulation in network, that is, hydrocarbon accumulation in the network source area, hydrocarbon accumulation in the network pathway, and hydrocarbon accumulation in the network terminal. The key in the application of the hydrocarbon accumulation models in network in practice is to confirm the major accumulation stage and the function range of the four elements controlling the hydrocarbon firstly, to predict the profitable accumulation region by superposition of the favorable areas confirmed by four elements consequently, and to evaluate the oil-bearing property of the trap as well as confirm drilling targets. This paper takes the Dongying Depression in the Bohai Bay Basin as an application example. | ||
650 | 4 | |a continental rift basin |7 (dpeaa)DE-He213 | |
650 | 4 | |a hydrocarbon accumulation theory |7 (dpeaa)DE-He213 | |
650 | 4 | |a hydrocarbon network |7 (dpeaa)DE-He213 | |
650 | 4 | |a hydrocarbon accumulation in network |7 (dpeaa)DE-He213 | |
650 | 4 | |a Bohai Bay Basin |7 (dpeaa)DE-He213 | |
700 | 1 | |a Chen, DongXia |e verfasserin |4 aut | |
700 | 1 | |a Zhang, ShanWen |e verfasserin |4 aut | |
700 | 1 | |a Hao, Fang |e verfasserin |4 aut | |
700 | 1 | |a Liu, Zheng |e verfasserin |4 aut | |
700 | 1 | |a Liu, KeYu |e verfasserin |4 aut | |
700 | 1 | |a Song, GuoQi |e verfasserin |4 aut | |
700 | 1 | |a Wang, YongShi |e verfasserin |4 aut | |
700 | 1 | |a Luo, XiaoRong |e verfasserin |4 aut | |
700 | 1 | |a Wu, XiaoChun |e verfasserin |4 aut | |
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10.1007/s11430-008-6026-5 doi (DE-627)SPR019229267 (SPR)s11430-008-6026-5-e DE-627 ger DE-627 rakwb eng 550 ASE 38.00 bkl Pang, XiongQi verfasserin aut Hydrocarbon accumulation in network and its application in the continental rift basin 2008 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The concept of hydrocarbon accumulation in network was presented on basis of the overall analysis of the formation and evolution characteristics of the continental faulted basin and of the systemic research on the major controlling factors on the hydrocarbon accumulation. The hydrocarbon accumulation in network can be defined as hydrocarbon accumulation in a three-dimensional network system which is constituted by the hydrocarbon migration passages under multiple dynamics, following the hydrocarbon generation from source rocks. The research shows that the hydrocarbon accumulation in network is composed of four elements, i.e., hydrocarbon source (source rock kitchen), hydrocarbon accumulation terminal (trap), network pathway connecting source and terminal (transporting system), and network potential driving hydrocarbon migration in the network pathway (migration dynamics). Compared with other networks, hydrocarbon accumulation in network has three basic characteristics: the irreversible geological process of material and information flow in the network; the loss of material and information in the flow process in the network; the multiple dynamics in the flow process. Interaction of all the elements in the geological process can be called hydrocarbon accumulation in network. There are three basic models for hydrocarbon accumulation in network, that is, hydrocarbon accumulation in the network source area, hydrocarbon accumulation in the network pathway, and hydrocarbon accumulation in the network terminal. The key in the application of the hydrocarbon accumulation models in network in practice is to confirm the major accumulation stage and the function range of the four elements controlling the hydrocarbon firstly, to predict the profitable accumulation region by superposition of the favorable areas confirmed by four elements consequently, and to evaluate the oil-bearing property of the trap as well as confirm drilling targets. This paper takes the Dongying Depression in the Bohai Bay Basin as an application example. continental rift basin (dpeaa)DE-He213 hydrocarbon accumulation theory (dpeaa)DE-He213 hydrocarbon network (dpeaa)DE-He213 hydrocarbon accumulation in network (dpeaa)DE-He213 Bohai Bay Basin (dpeaa)DE-He213 Chen, DongXia verfasserin aut Zhang, ShanWen verfasserin aut Hao, Fang verfasserin aut Liu, Zheng verfasserin aut Liu, KeYu verfasserin aut Song, GuoQi verfasserin aut Wang, YongShi verfasserin aut Luo, XiaoRong verfasserin aut Wu, XiaoChun verfasserin aut Enthalten in Science in China Heidelberg : Springer, 1997 51(2008), Suppl 2 vom: Okt., Seite 88-100 (DE-627)385614748 (DE-600)2142896-7 1862-2801 nnns volume:51 year:2008 number:Suppl 2 month:10 pages:88-100 https://dx.doi.org/10.1007/s11430-008-6026-5 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 2 10 88-100 |
spelling |
10.1007/s11430-008-6026-5 doi (DE-627)SPR019229267 (SPR)s11430-008-6026-5-e DE-627 ger DE-627 rakwb eng 550 ASE 38.00 bkl Pang, XiongQi verfasserin aut Hydrocarbon accumulation in network and its application in the continental rift basin 2008 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The concept of hydrocarbon accumulation in network was presented on basis of the overall analysis of the formation and evolution characteristics of the continental faulted basin and of the systemic research on the major controlling factors on the hydrocarbon accumulation. The hydrocarbon accumulation in network can be defined as hydrocarbon accumulation in a three-dimensional network system which is constituted by the hydrocarbon migration passages under multiple dynamics, following the hydrocarbon generation from source rocks. The research shows that the hydrocarbon accumulation in network is composed of four elements, i.e., hydrocarbon source (source rock kitchen), hydrocarbon accumulation terminal (trap), network pathway connecting source and terminal (transporting system), and network potential driving hydrocarbon migration in the network pathway (migration dynamics). Compared with other networks, hydrocarbon accumulation in network has three basic characteristics: the irreversible geological process of material and information flow in the network; the loss of material and information in the flow process in the network; the multiple dynamics in the flow process. Interaction of all the elements in the geological process can be called hydrocarbon accumulation in network. There are three basic models for hydrocarbon accumulation in network, that is, hydrocarbon accumulation in the network source area, hydrocarbon accumulation in the network pathway, and hydrocarbon accumulation in the network terminal. The key in the application of the hydrocarbon accumulation models in network in practice is to confirm the major accumulation stage and the function range of the four elements controlling the hydrocarbon firstly, to predict the profitable accumulation region by superposition of the favorable areas confirmed by four elements consequently, and to evaluate the oil-bearing property of the trap as well as confirm drilling targets. This paper takes the Dongying Depression in the Bohai Bay Basin as an application example. continental rift basin (dpeaa)DE-He213 hydrocarbon accumulation theory (dpeaa)DE-He213 hydrocarbon network (dpeaa)DE-He213 hydrocarbon accumulation in network (dpeaa)DE-He213 Bohai Bay Basin (dpeaa)DE-He213 Chen, DongXia verfasserin aut Zhang, ShanWen verfasserin aut Hao, Fang verfasserin aut Liu, Zheng verfasserin aut Liu, KeYu verfasserin aut Song, GuoQi verfasserin aut Wang, YongShi verfasserin aut Luo, XiaoRong verfasserin aut Wu, XiaoChun verfasserin aut Enthalten in Science in China Heidelberg : Springer, 1997 51(2008), Suppl 2 vom: Okt., Seite 88-100 (DE-627)385614748 (DE-600)2142896-7 1862-2801 nnns volume:51 year:2008 number:Suppl 2 month:10 pages:88-100 https://dx.doi.org/10.1007/s11430-008-6026-5 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 2 10 88-100 |
allfields_unstemmed |
10.1007/s11430-008-6026-5 doi (DE-627)SPR019229267 (SPR)s11430-008-6026-5-e DE-627 ger DE-627 rakwb eng 550 ASE 38.00 bkl Pang, XiongQi verfasserin aut Hydrocarbon accumulation in network and its application in the continental rift basin 2008 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The concept of hydrocarbon accumulation in network was presented on basis of the overall analysis of the formation and evolution characteristics of the continental faulted basin and of the systemic research on the major controlling factors on the hydrocarbon accumulation. The hydrocarbon accumulation in network can be defined as hydrocarbon accumulation in a three-dimensional network system which is constituted by the hydrocarbon migration passages under multiple dynamics, following the hydrocarbon generation from source rocks. The research shows that the hydrocarbon accumulation in network is composed of four elements, i.e., hydrocarbon source (source rock kitchen), hydrocarbon accumulation terminal (trap), network pathway connecting source and terminal (transporting system), and network potential driving hydrocarbon migration in the network pathway (migration dynamics). Compared with other networks, hydrocarbon accumulation in network has three basic characteristics: the irreversible geological process of material and information flow in the network; the loss of material and information in the flow process in the network; the multiple dynamics in the flow process. Interaction of all the elements in the geological process can be called hydrocarbon accumulation in network. There are three basic models for hydrocarbon accumulation in network, that is, hydrocarbon accumulation in the network source area, hydrocarbon accumulation in the network pathway, and hydrocarbon accumulation in the network terminal. The key in the application of the hydrocarbon accumulation models in network in practice is to confirm the major accumulation stage and the function range of the four elements controlling the hydrocarbon firstly, to predict the profitable accumulation region by superposition of the favorable areas confirmed by four elements consequently, and to evaluate the oil-bearing property of the trap as well as confirm drilling targets. This paper takes the Dongying Depression in the Bohai Bay Basin as an application example. continental rift basin (dpeaa)DE-He213 hydrocarbon accumulation theory (dpeaa)DE-He213 hydrocarbon network (dpeaa)DE-He213 hydrocarbon accumulation in network (dpeaa)DE-He213 Bohai Bay Basin (dpeaa)DE-He213 Chen, DongXia verfasserin aut Zhang, ShanWen verfasserin aut Hao, Fang verfasserin aut Liu, Zheng verfasserin aut Liu, KeYu verfasserin aut Song, GuoQi verfasserin aut Wang, YongShi verfasserin aut Luo, XiaoRong verfasserin aut Wu, XiaoChun verfasserin aut Enthalten in Science in China Heidelberg : Springer, 1997 51(2008), Suppl 2 vom: Okt., Seite 88-100 (DE-627)385614748 (DE-600)2142896-7 1862-2801 nnns volume:51 year:2008 number:Suppl 2 month:10 pages:88-100 https://dx.doi.org/10.1007/s11430-008-6026-5 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 2 10 88-100 |
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10.1007/s11430-008-6026-5 doi (DE-627)SPR019229267 (SPR)s11430-008-6026-5-e DE-627 ger DE-627 rakwb eng 550 ASE 38.00 bkl Pang, XiongQi verfasserin aut Hydrocarbon accumulation in network and its application in the continental rift basin 2008 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The concept of hydrocarbon accumulation in network was presented on basis of the overall analysis of the formation and evolution characteristics of the continental faulted basin and of the systemic research on the major controlling factors on the hydrocarbon accumulation. The hydrocarbon accumulation in network can be defined as hydrocarbon accumulation in a three-dimensional network system which is constituted by the hydrocarbon migration passages under multiple dynamics, following the hydrocarbon generation from source rocks. The research shows that the hydrocarbon accumulation in network is composed of four elements, i.e., hydrocarbon source (source rock kitchen), hydrocarbon accumulation terminal (trap), network pathway connecting source and terminal (transporting system), and network potential driving hydrocarbon migration in the network pathway (migration dynamics). Compared with other networks, hydrocarbon accumulation in network has three basic characteristics: the irreversible geological process of material and information flow in the network; the loss of material and information in the flow process in the network; the multiple dynamics in the flow process. Interaction of all the elements in the geological process can be called hydrocarbon accumulation in network. There are three basic models for hydrocarbon accumulation in network, that is, hydrocarbon accumulation in the network source area, hydrocarbon accumulation in the network pathway, and hydrocarbon accumulation in the network terminal. The key in the application of the hydrocarbon accumulation models in network in practice is to confirm the major accumulation stage and the function range of the four elements controlling the hydrocarbon firstly, to predict the profitable accumulation region by superposition of the favorable areas confirmed by four elements consequently, and to evaluate the oil-bearing property of the trap as well as confirm drilling targets. This paper takes the Dongying Depression in the Bohai Bay Basin as an application example. continental rift basin (dpeaa)DE-He213 hydrocarbon accumulation theory (dpeaa)DE-He213 hydrocarbon network (dpeaa)DE-He213 hydrocarbon accumulation in network (dpeaa)DE-He213 Bohai Bay Basin (dpeaa)DE-He213 Chen, DongXia verfasserin aut Zhang, ShanWen verfasserin aut Hao, Fang verfasserin aut Liu, Zheng verfasserin aut Liu, KeYu verfasserin aut Song, GuoQi verfasserin aut Wang, YongShi verfasserin aut Luo, XiaoRong verfasserin aut Wu, XiaoChun verfasserin aut Enthalten in Science in China Heidelberg : Springer, 1997 51(2008), Suppl 2 vom: Okt., Seite 88-100 (DE-627)385614748 (DE-600)2142896-7 1862-2801 nnns volume:51 year:2008 number:Suppl 2 month:10 pages:88-100 https://dx.doi.org/10.1007/s11430-008-6026-5 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 2 10 88-100 |
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10.1007/s11430-008-6026-5 doi (DE-627)SPR019229267 (SPR)s11430-008-6026-5-e DE-627 ger DE-627 rakwb eng 550 ASE 38.00 bkl Pang, XiongQi verfasserin aut Hydrocarbon accumulation in network and its application in the continental rift basin 2008 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The concept of hydrocarbon accumulation in network was presented on basis of the overall analysis of the formation and evolution characteristics of the continental faulted basin and of the systemic research on the major controlling factors on the hydrocarbon accumulation. The hydrocarbon accumulation in network can be defined as hydrocarbon accumulation in a three-dimensional network system which is constituted by the hydrocarbon migration passages under multiple dynamics, following the hydrocarbon generation from source rocks. The research shows that the hydrocarbon accumulation in network is composed of four elements, i.e., hydrocarbon source (source rock kitchen), hydrocarbon accumulation terminal (trap), network pathway connecting source and terminal (transporting system), and network potential driving hydrocarbon migration in the network pathway (migration dynamics). Compared with other networks, hydrocarbon accumulation in network has three basic characteristics: the irreversible geological process of material and information flow in the network; the loss of material and information in the flow process in the network; the multiple dynamics in the flow process. Interaction of all the elements in the geological process can be called hydrocarbon accumulation in network. There are three basic models for hydrocarbon accumulation in network, that is, hydrocarbon accumulation in the network source area, hydrocarbon accumulation in the network pathway, and hydrocarbon accumulation in the network terminal. The key in the application of the hydrocarbon accumulation models in network in practice is to confirm the major accumulation stage and the function range of the four elements controlling the hydrocarbon firstly, to predict the profitable accumulation region by superposition of the favorable areas confirmed by four elements consequently, and to evaluate the oil-bearing property of the trap as well as confirm drilling targets. This paper takes the Dongying Depression in the Bohai Bay Basin as an application example. continental rift basin (dpeaa)DE-He213 hydrocarbon accumulation theory (dpeaa)DE-He213 hydrocarbon network (dpeaa)DE-He213 hydrocarbon accumulation in network (dpeaa)DE-He213 Bohai Bay Basin (dpeaa)DE-He213 Chen, DongXia verfasserin aut Zhang, ShanWen verfasserin aut Hao, Fang verfasserin aut Liu, Zheng verfasserin aut Liu, KeYu verfasserin aut Song, GuoQi verfasserin aut Wang, YongShi verfasserin aut Luo, XiaoRong verfasserin aut Wu, XiaoChun verfasserin aut Enthalten in Science in China Heidelberg : Springer, 1997 51(2008), Suppl 2 vom: Okt., Seite 88-100 (DE-627)385614748 (DE-600)2142896-7 1862-2801 nnns volume:51 year:2008 number:Suppl 2 month:10 pages:88-100 https://dx.doi.org/10.1007/s11430-008-6026-5 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 2 10 88-100 |
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English |
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Enthalten in Science in China 51(2008), Suppl 2 vom: Okt., Seite 88-100 volume:51 year:2008 number:Suppl 2 month:10 pages:88-100 |
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Enthalten in Science in China 51(2008), Suppl 2 vom: Okt., Seite 88-100 volume:51 year:2008 number:Suppl 2 month:10 pages:88-100 |
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continental rift basin hydrocarbon accumulation theory hydrocarbon network hydrocarbon accumulation in network Bohai Bay Basin |
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Science in China |
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Pang, XiongQi @@aut@@ Chen, DongXia @@aut@@ Zhang, ShanWen @@aut@@ Hao, Fang @@aut@@ Liu, Zheng @@aut@@ Liu, KeYu @@aut@@ Song, GuoQi @@aut@@ Wang, YongShi @@aut@@ Luo, XiaoRong @@aut@@ Wu, XiaoChun @@aut@@ |
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2008-10-01T00:00:00Z |
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The hydrocarbon accumulation in network can be defined as hydrocarbon accumulation in a three-dimensional network system which is constituted by the hydrocarbon migration passages under multiple dynamics, following the hydrocarbon generation from source rocks. The research shows that the hydrocarbon accumulation in network is composed of four elements, i.e., hydrocarbon source (source rock kitchen), hydrocarbon accumulation terminal (trap), network pathway connecting source and terminal (transporting system), and network potential driving hydrocarbon migration in the network pathway (migration dynamics). Compared with other networks, hydrocarbon accumulation in network has three basic characteristics: the irreversible geological process of material and information flow in the network; the loss of material and information in the flow process in the network; the multiple dynamics in the flow process. Interaction of all the elements in the geological process can be called hydrocarbon accumulation in network. There are three basic models for hydrocarbon accumulation in network, that is, hydrocarbon accumulation in the network source area, hydrocarbon accumulation in the network pathway, and hydrocarbon accumulation in the network terminal. The key in the application of the hydrocarbon accumulation models in network in practice is to confirm the major accumulation stage and the function range of the four elements controlling the hydrocarbon firstly, to predict the profitable accumulation region by superposition of the favorable areas confirmed by four elements consequently, and to evaluate the oil-bearing property of the trap as well as confirm drilling targets. 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|
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Pang, XiongQi |
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Pang, XiongQi ddc 550 bkl 38.00 misc continental rift basin misc hydrocarbon accumulation theory misc hydrocarbon network misc hydrocarbon accumulation in network misc Bohai Bay Basin Hydrocarbon accumulation in network and its application in the continental rift basin |
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550 ASE 38.00 bkl Hydrocarbon accumulation in network and its application in the continental rift basin continental rift basin (dpeaa)DE-He213 hydrocarbon accumulation theory (dpeaa)DE-He213 hydrocarbon network (dpeaa)DE-He213 hydrocarbon accumulation in network (dpeaa)DE-He213 Bohai Bay Basin (dpeaa)DE-He213 |
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Pang, XiongQi Chen, DongXia Zhang, ShanWen Hao, Fang Liu, Zheng Liu, KeYu Song, GuoQi Wang, YongShi Luo, XiaoRong Wu, XiaoChun |
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Elektronische Aufsätze |
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Pang, XiongQi |
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10.1007/s11430-008-6026-5 |
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title_sort |
hydrocarbon accumulation in network and its application in the continental rift basin |
title_auth |
Hydrocarbon accumulation in network and its application in the continental rift basin |
abstract |
Abstract The concept of hydrocarbon accumulation in network was presented on basis of the overall analysis of the formation and evolution characteristics of the continental faulted basin and of the systemic research on the major controlling factors on the hydrocarbon accumulation. The hydrocarbon accumulation in network can be defined as hydrocarbon accumulation in a three-dimensional network system which is constituted by the hydrocarbon migration passages under multiple dynamics, following the hydrocarbon generation from source rocks. The research shows that the hydrocarbon accumulation in network is composed of four elements, i.e., hydrocarbon source (source rock kitchen), hydrocarbon accumulation terminal (trap), network pathway connecting source and terminal (transporting system), and network potential driving hydrocarbon migration in the network pathway (migration dynamics). Compared with other networks, hydrocarbon accumulation in network has three basic characteristics: the irreversible geological process of material and information flow in the network; the loss of material and information in the flow process in the network; the multiple dynamics in the flow process. Interaction of all the elements in the geological process can be called hydrocarbon accumulation in network. There are three basic models for hydrocarbon accumulation in network, that is, hydrocarbon accumulation in the network source area, hydrocarbon accumulation in the network pathway, and hydrocarbon accumulation in the network terminal. The key in the application of the hydrocarbon accumulation models in network in practice is to confirm the major accumulation stage and the function range of the four elements controlling the hydrocarbon firstly, to predict the profitable accumulation region by superposition of the favorable areas confirmed by four elements consequently, and to evaluate the oil-bearing property of the trap as well as confirm drilling targets. This paper takes the Dongying Depression in the Bohai Bay Basin as an application example. |
abstractGer |
Abstract The concept of hydrocarbon accumulation in network was presented on basis of the overall analysis of the formation and evolution characteristics of the continental faulted basin and of the systemic research on the major controlling factors on the hydrocarbon accumulation. The hydrocarbon accumulation in network can be defined as hydrocarbon accumulation in a three-dimensional network system which is constituted by the hydrocarbon migration passages under multiple dynamics, following the hydrocarbon generation from source rocks. The research shows that the hydrocarbon accumulation in network is composed of four elements, i.e., hydrocarbon source (source rock kitchen), hydrocarbon accumulation terminal (trap), network pathway connecting source and terminal (transporting system), and network potential driving hydrocarbon migration in the network pathway (migration dynamics). Compared with other networks, hydrocarbon accumulation in network has three basic characteristics: the irreversible geological process of material and information flow in the network; the loss of material and information in the flow process in the network; the multiple dynamics in the flow process. Interaction of all the elements in the geological process can be called hydrocarbon accumulation in network. There are three basic models for hydrocarbon accumulation in network, that is, hydrocarbon accumulation in the network source area, hydrocarbon accumulation in the network pathway, and hydrocarbon accumulation in the network terminal. The key in the application of the hydrocarbon accumulation models in network in practice is to confirm the major accumulation stage and the function range of the four elements controlling the hydrocarbon firstly, to predict the profitable accumulation region by superposition of the favorable areas confirmed by four elements consequently, and to evaluate the oil-bearing property of the trap as well as confirm drilling targets. This paper takes the Dongying Depression in the Bohai Bay Basin as an application example. |
abstract_unstemmed |
Abstract The concept of hydrocarbon accumulation in network was presented on basis of the overall analysis of the formation and evolution characteristics of the continental faulted basin and of the systemic research on the major controlling factors on the hydrocarbon accumulation. The hydrocarbon accumulation in network can be defined as hydrocarbon accumulation in a three-dimensional network system which is constituted by the hydrocarbon migration passages under multiple dynamics, following the hydrocarbon generation from source rocks. The research shows that the hydrocarbon accumulation in network is composed of four elements, i.e., hydrocarbon source (source rock kitchen), hydrocarbon accumulation terminal (trap), network pathway connecting source and terminal (transporting system), and network potential driving hydrocarbon migration in the network pathway (migration dynamics). Compared with other networks, hydrocarbon accumulation in network has three basic characteristics: the irreversible geological process of material and information flow in the network; the loss of material and information in the flow process in the network; the multiple dynamics in the flow process. Interaction of all the elements in the geological process can be called hydrocarbon accumulation in network. There are three basic models for hydrocarbon accumulation in network, that is, hydrocarbon accumulation in the network source area, hydrocarbon accumulation in the network pathway, and hydrocarbon accumulation in the network terminal. The key in the application of the hydrocarbon accumulation models in network in practice is to confirm the major accumulation stage and the function range of the four elements controlling the hydrocarbon firstly, to predict the profitable accumulation region by superposition of the favorable areas confirmed by four elements consequently, and to evaluate the oil-bearing property of the trap as well as confirm drilling targets. This paper takes the Dongying Depression in the Bohai Bay Basin as an application example. |
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container_issue |
Suppl 2 |
title_short |
Hydrocarbon accumulation in network and its application in the continental rift basin |
url |
https://dx.doi.org/10.1007/s11430-008-6026-5 |
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Chen, DongXia Zhang, ShanWen Hao, Fang Liu, Zheng Liu, KeYu Song, GuoQi Wang, YongShi Luo, XiaoRong Wu, XiaoChun |
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Chen, DongXia Zhang, ShanWen Hao, Fang Liu, Zheng Liu, KeYu Song, GuoQi Wang, YongShi Luo, XiaoRong Wu, XiaoChun |
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10.1007/s11430-008-6026-5 |
up_date |
2024-07-04T00:43:34.126Z |
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|
score |
7.4006996 |