Effect of tectonic evolution on hydrocarbon charging time: A case study from Lower Shihezi Formation (Guadalupian), the Hangjinqi area, northern Ordos, China

A giant gas field has been discovered in the Lower Shihezi Formation in the Hangjinqi area, northern Ordos Basin, China. Coal seams and mudstone in the Taiyuan and Shanxi Formation are considered as source rocks and sandstone in the Lower Shihezi Formation is treated as reservoirs for gas. The charg...
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Autor*in:	Bai, Donglai [verfasserIn] Yang, Minghui [verfasserIn] Lei, Zhibin [verfasserIn] Zhang, Yue [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2019

Schlagwörter:	Charging time Lower Shihezi Formation Tectonic evolution Northern Ordos Basin

Übergeordnetes Werk:	Enthalten in: Journal of petroleum science and engineering - Amsterdam [u.a.] : Elsevier Science, 1987, 184
Übergeordnetes Werk:	volume:184

DOI / URN:	10.1016/j.petrol.2019.106465

Katalog-ID:	ELV003281752

Internformat


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520			\|a A giant gas field has been discovered in the Lower Shihezi Formation in the Hangjinqi area, northern Ordos Basin, China. Coal seams and mudstone in the Taiyuan and Shanxi Formation are considered as source rocks and sandstone in the Lower Shihezi Formation is treated as reservoirs for gas. The charging time in the sandstone reservoirs was studied based on the homogenization temperature of aqueous inclusions, thermal and burial history simulation and K-Ar dating of authigenic illite. Two episodes of gas charging in the northern part and one episode in the southern part were delineated in the reservoirs of the Hangjinqi area, evidenced by microscopic observation of the occurrence of fluid inclusions and the analysis of salinity in aqueous inclusions. In the southern part of the study area gas charging occurred between circa 171-162 Ma, whereas in the northern part gas charging was between 158-144 Ma and 120-109 Ma, respectively. The gas charging events appeared to be influenced by the tectonic evolution of northern Ordos Basin. Paleo topography caused reduction in thickness of source rocks northwards, and contributed to differences in hydrocarbon generation potential and thermal evolution between the northern and the southern part of the study area. Therefore, gas charging occurred in the southern part prior to that in the northern part. Furthermore, tilting occurred in Middle Jurassic and provided the driver and pathways for gas, leading to a first charging event in the northern part of the study area.
650		4	\|a Charging time
650		4	\|a Lower Shihezi Formation
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700	1		\|a Lei, Zhibin \|e verfasserin \|4 aut
700	1		\|a Zhang, Yue \|e verfasserin \|4 aut
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Indexfelder

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matchkey_str	baidonglaiyangminghuileizhibinzhangyue:2019----:fetfetncvltoohdoabnhrigiecssuyrmoesieiomtogaauin
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publishDate	2019
allfields	10.1016/j.petrol.2019.106465 doi (DE-627)ELV003281752 (ELSEVIER)S0920-4105(19)30886-1 DE-627 ger DE-627 rda eng 660 DE-600 38.51 bkl 57.36 bkl Bai, Donglai verfasserin aut Effect of tectonic evolution on hydrocarbon charging time: A case study from Lower Shihezi Formation (Guadalupian), the Hangjinqi area, northern Ordos, China 2019 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier A giant gas field has been discovered in the Lower Shihezi Formation in the Hangjinqi area, northern Ordos Basin, China. Coal seams and mudstone in the Taiyuan and Shanxi Formation are considered as source rocks and sandstone in the Lower Shihezi Formation is treated as reservoirs for gas. The charging time in the sandstone reservoirs was studied based on the homogenization temperature of aqueous inclusions, thermal and burial history simulation and K-Ar dating of authigenic illite. Two episodes of gas charging in the northern part and one episode in the southern part were delineated in the reservoirs of the Hangjinqi area, evidenced by microscopic observation of the occurrence of fluid inclusions and the analysis of salinity in aqueous inclusions. In the southern part of the study area gas charging occurred between circa 171-162 Ma, whereas in the northern part gas charging was between 158-144 Ma and 120-109 Ma, respectively. The gas charging events appeared to be influenced by the tectonic evolution of northern Ordos Basin. Paleo topography caused reduction in thickness of source rocks northwards, and contributed to differences in hydrocarbon generation potential and thermal evolution between the northern and the southern part of the study area. Therefore, gas charging occurred in the southern part prior to that in the northern part. Furthermore, tilting occurred in Middle Jurassic and provided the driver and pathways for gas, leading to a first charging event in the northern part of the study area. Charging time Lower Shihezi Formation Tectonic evolution Northern Ordos Basin Yang, Minghui verfasserin aut Lei, Zhibin verfasserin aut Zhang, Yue verfasserin aut Enthalten in Journal of petroleum science and engineering Amsterdam [u.a.] : Elsevier Science, 1987 184 Online-Ressource (DE-627)303393076 (DE-600)1494872-2 (DE-576)259484024 nnns volume:184 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OLC-PHA SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 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_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.51 Geologie fossiler Brennstoffe 57.36 Erdölgewinnung Erdgasgewinnung AR 184
spelling	10.1016/j.petrol.2019.106465 doi (DE-627)ELV003281752 (ELSEVIER)S0920-4105(19)30886-1 DE-627 ger DE-627 rda eng 660 DE-600 38.51 bkl 57.36 bkl Bai, Donglai verfasserin aut Effect of tectonic evolution on hydrocarbon charging time: A case study from Lower Shihezi Formation (Guadalupian), the Hangjinqi area, northern Ordos, China 2019 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier A giant gas field has been discovered in the Lower Shihezi Formation in the Hangjinqi area, northern Ordos Basin, China. Coal seams and mudstone in the Taiyuan and Shanxi Formation are considered as source rocks and sandstone in the Lower Shihezi Formation is treated as reservoirs for gas. The charging time in the sandstone reservoirs was studied based on the homogenization temperature of aqueous inclusions, thermal and burial history simulation and K-Ar dating of authigenic illite. Two episodes of gas charging in the northern part and one episode in the southern part were delineated in the reservoirs of the Hangjinqi area, evidenced by microscopic observation of the occurrence of fluid inclusions and the analysis of salinity in aqueous inclusions. In the southern part of the study area gas charging occurred between circa 171-162 Ma, whereas in the northern part gas charging was between 158-144 Ma and 120-109 Ma, respectively. The gas charging events appeared to be influenced by the tectonic evolution of northern Ordos Basin. Paleo topography caused reduction in thickness of source rocks northwards, and contributed to differences in hydrocarbon generation potential and thermal evolution between the northern and the southern part of the study area. Therefore, gas charging occurred in the southern part prior to that in the northern part. Furthermore, tilting occurred in Middle Jurassic and provided the driver and pathways for gas, leading to a first charging event in the northern part of the study area. Charging time Lower Shihezi Formation Tectonic evolution Northern Ordos Basin Yang, Minghui verfasserin aut Lei, Zhibin verfasserin aut Zhang, Yue verfasserin aut Enthalten in Journal of petroleum science and engineering Amsterdam [u.a.] : Elsevier Science, 1987 184 Online-Ressource (DE-627)303393076 (DE-600)1494872-2 (DE-576)259484024 nnns volume:184 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OLC-PHA SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 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_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.51 Geologie fossiler Brennstoffe 57.36 Erdölgewinnung Erdgasgewinnung AR 184
allfields_unstemmed	10.1016/j.petrol.2019.106465 doi (DE-627)ELV003281752 (ELSEVIER)S0920-4105(19)30886-1 DE-627 ger DE-627 rda eng 660 DE-600 38.51 bkl 57.36 bkl Bai, Donglai verfasserin aut Effect of tectonic evolution on hydrocarbon charging time: A case study from Lower Shihezi Formation (Guadalupian), the Hangjinqi area, northern Ordos, China 2019 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier A giant gas field has been discovered in the Lower Shihezi Formation in the Hangjinqi area, northern Ordos Basin, China. Coal seams and mudstone in the Taiyuan and Shanxi Formation are considered as source rocks and sandstone in the Lower Shihezi Formation is treated as reservoirs for gas. The charging time in the sandstone reservoirs was studied based on the homogenization temperature of aqueous inclusions, thermal and burial history simulation and K-Ar dating of authigenic illite. Two episodes of gas charging in the northern part and one episode in the southern part were delineated in the reservoirs of the Hangjinqi area, evidenced by microscopic observation of the occurrence of fluid inclusions and the analysis of salinity in aqueous inclusions. In the southern part of the study area gas charging occurred between circa 171-162 Ma, whereas in the northern part gas charging was between 158-144 Ma and 120-109 Ma, respectively. The gas charging events appeared to be influenced by the tectonic evolution of northern Ordos Basin. Paleo topography caused reduction in thickness of source rocks northwards, and contributed to differences in hydrocarbon generation potential and thermal evolution between the northern and the southern part of the study area. Therefore, gas charging occurred in the southern part prior to that in the northern part. Furthermore, tilting occurred in Middle Jurassic and provided the driver and pathways for gas, leading to a first charging event in the northern part of the study area. Charging time Lower Shihezi Formation Tectonic evolution Northern Ordos Basin Yang, Minghui verfasserin aut Lei, Zhibin verfasserin aut Zhang, Yue verfasserin aut Enthalten in Journal of petroleum science and engineering Amsterdam [u.a.] : Elsevier Science, 1987 184 Online-Ressource (DE-627)303393076 (DE-600)1494872-2 (DE-576)259484024 nnns volume:184 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OLC-PHA SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 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_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.51 Geologie fossiler Brennstoffe 57.36 Erdölgewinnung Erdgasgewinnung AR 184
allfieldsGer	10.1016/j.petrol.2019.106465 doi (DE-627)ELV003281752 (ELSEVIER)S0920-4105(19)30886-1 DE-627 ger DE-627 rda eng 660 DE-600 38.51 bkl 57.36 bkl Bai, Donglai verfasserin aut Effect of tectonic evolution on hydrocarbon charging time: A case study from Lower Shihezi Formation (Guadalupian), the Hangjinqi area, northern Ordos, China 2019 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier A giant gas field has been discovered in the Lower Shihezi Formation in the Hangjinqi area, northern Ordos Basin, China. Coal seams and mudstone in the Taiyuan and Shanxi Formation are considered as source rocks and sandstone in the Lower Shihezi Formation is treated as reservoirs for gas. The charging time in the sandstone reservoirs was studied based on the homogenization temperature of aqueous inclusions, thermal and burial history simulation and K-Ar dating of authigenic illite. Two episodes of gas charging in the northern part and one episode in the southern part were delineated in the reservoirs of the Hangjinqi area, evidenced by microscopic observation of the occurrence of fluid inclusions and the analysis of salinity in aqueous inclusions. In the southern part of the study area gas charging occurred between circa 171-162 Ma, whereas in the northern part gas charging was between 158-144 Ma and 120-109 Ma, respectively. The gas charging events appeared to be influenced by the tectonic evolution of northern Ordos Basin. Paleo topography caused reduction in thickness of source rocks northwards, and contributed to differences in hydrocarbon generation potential and thermal evolution between the northern and the southern part of the study area. Therefore, gas charging occurred in the southern part prior to that in the northern part. Furthermore, tilting occurred in Middle Jurassic and provided the driver and pathways for gas, leading to a first charging event in the northern part of the study area. Charging time Lower Shihezi Formation Tectonic evolution Northern Ordos Basin Yang, Minghui verfasserin aut Lei, Zhibin verfasserin aut Zhang, Yue verfasserin aut Enthalten in Journal of petroleum science and engineering Amsterdam [u.a.] : Elsevier Science, 1987 184 Online-Ressource (DE-627)303393076 (DE-600)1494872-2 (DE-576)259484024 nnns volume:184 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OLC-PHA SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 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_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.51 Geologie fossiler Brennstoffe 57.36 Erdölgewinnung Erdgasgewinnung AR 184
allfieldsSound	10.1016/j.petrol.2019.106465 doi (DE-627)ELV003281752 (ELSEVIER)S0920-4105(19)30886-1 DE-627 ger DE-627 rda eng 660 DE-600 38.51 bkl 57.36 bkl Bai, Donglai verfasserin aut Effect of tectonic evolution on hydrocarbon charging time: A case study from Lower Shihezi Formation (Guadalupian), the Hangjinqi area, northern Ordos, China 2019 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier A giant gas field has been discovered in the Lower Shihezi Formation in the Hangjinqi area, northern Ordos Basin, China. Coal seams and mudstone in the Taiyuan and Shanxi Formation are considered as source rocks and sandstone in the Lower Shihezi Formation is treated as reservoirs for gas. The charging time in the sandstone reservoirs was studied based on the homogenization temperature of aqueous inclusions, thermal and burial history simulation and K-Ar dating of authigenic illite. Two episodes of gas charging in the northern part and one episode in the southern part were delineated in the reservoirs of the Hangjinqi area, evidenced by microscopic observation of the occurrence of fluid inclusions and the analysis of salinity in aqueous inclusions. In the southern part of the study area gas charging occurred between circa 171-162 Ma, whereas in the northern part gas charging was between 158-144 Ma and 120-109 Ma, respectively. The gas charging events appeared to be influenced by the tectonic evolution of northern Ordos Basin. Paleo topography caused reduction in thickness of source rocks northwards, and contributed to differences in hydrocarbon generation potential and thermal evolution between the northern and the southern part of the study area. Therefore, gas charging occurred in the southern part prior to that in the northern part. Furthermore, tilting occurred in Middle Jurassic and provided the driver and pathways for gas, leading to a first charging event in the northern part of the study area. Charging time Lower Shihezi Formation Tectonic evolution Northern Ordos Basin Yang, Minghui verfasserin aut Lei, Zhibin verfasserin aut Zhang, Yue verfasserin aut Enthalten in Journal of petroleum science and engineering Amsterdam [u.a.] : Elsevier Science, 1987 184 Online-Ressource (DE-627)303393076 (DE-600)1494872-2 (DE-576)259484024 nnns volume:184 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OLC-PHA SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 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_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.51 Geologie fossiler Brennstoffe 57.36 Erdölgewinnung Erdgasgewinnung AR 184
language	English
source	Enthalten in Journal of petroleum science and engineering 184 volume:184
sourceStr	Enthalten in Journal of petroleum science and engineering 184 volume:184
format_phy_str_mv	Article
bklname	Geologie fossiler Brennstoffe Erdölgewinnung Erdgasgewinnung
institution	findex.gbv.de
topic_facet	Charging time Lower Shihezi Formation Tectonic evolution Northern Ordos Basin
dewey-raw	660
isfreeaccess_bool	false
container_title	Journal of petroleum science and engineering
authorswithroles_txt_mv	Bai, Donglai @@aut@@ Yang, Minghui @@aut@@ Lei, Zhibin @@aut@@ Zhang, Yue @@aut@@
publishDateDaySort_date	2019-01-01T00:00:00Z
hierarchy_top_id	303393076
dewey-sort	3660
id	ELV003281752
language_de	englisch
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author	Bai, Donglai
spellingShingle	Bai, Donglai ddc 660 bkl 38.51 bkl 57.36 misc Charging time misc Lower Shihezi Formation misc Tectonic evolution misc Northern Ordos Basin Effect of tectonic evolution on hydrocarbon charging time: A case study from Lower Shihezi Formation (Guadalupian), the Hangjinqi area, northern Ordos, China
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topic_title	660 DE-600 38.51 bkl 57.36 bkl Effect of tectonic evolution on hydrocarbon charging time: A case study from Lower Shihezi Formation (Guadalupian), the Hangjinqi area, northern Ordos, China Charging time Lower Shihezi Formation Tectonic evolution Northern Ordos Basin
topic	ddc 660 bkl 38.51 bkl 57.36 misc Charging time misc Lower Shihezi Formation misc Tectonic evolution misc Northern Ordos Basin
topic_unstemmed	ddc 660 bkl 38.51 bkl 57.36 misc Charging time misc Lower Shihezi Formation misc Tectonic evolution misc Northern Ordos Basin
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title	Effect of tectonic evolution on hydrocarbon charging time: A case study from Lower Shihezi Formation (Guadalupian), the Hangjinqi area, northern Ordos, China
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title_full	Effect of tectonic evolution on hydrocarbon charging time: A case study from Lower Shihezi Formation (Guadalupian), the Hangjinqi area, northern Ordos, China
author_sort	Bai, Donglai
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author_browse	Bai, Donglai Yang, Minghui Lei, Zhibin Zhang, Yue
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title_sort	effect of tectonic evolution on hydrocarbon charging time: a case study from lower shihezi formation (guadalupian), the hangjinqi area, northern ordos, china
title_auth	Effect of tectonic evolution on hydrocarbon charging time: A case study from Lower Shihezi Formation (Guadalupian), the Hangjinqi area, northern Ordos, China
abstract	A giant gas field has been discovered in the Lower Shihezi Formation in the Hangjinqi area, northern Ordos Basin, China. Coal seams and mudstone in the Taiyuan and Shanxi Formation are considered as source rocks and sandstone in the Lower Shihezi Formation is treated as reservoirs for gas. The charging time in the sandstone reservoirs was studied based on the homogenization temperature of aqueous inclusions, thermal and burial history simulation and K-Ar dating of authigenic illite. Two episodes of gas charging in the northern part and one episode in the southern part were delineated in the reservoirs of the Hangjinqi area, evidenced by microscopic observation of the occurrence of fluid inclusions and the analysis of salinity in aqueous inclusions. In the southern part of the study area gas charging occurred between circa 171-162 Ma, whereas in the northern part gas charging was between 158-144 Ma and 120-109 Ma, respectively. The gas charging events appeared to be influenced by the tectonic evolution of northern Ordos Basin. Paleo topography caused reduction in thickness of source rocks northwards, and contributed to differences in hydrocarbon generation potential and thermal evolution between the northern and the southern part of the study area. Therefore, gas charging occurred in the southern part prior to that in the northern part. Furthermore, tilting occurred in Middle Jurassic and provided the driver and pathways for gas, leading to a first charging event in the northern part of the study area.
abstractGer	A giant gas field has been discovered in the Lower Shihezi Formation in the Hangjinqi area, northern Ordos Basin, China. Coal seams and mudstone in the Taiyuan and Shanxi Formation are considered as source rocks and sandstone in the Lower Shihezi Formation is treated as reservoirs for gas. The charging time in the sandstone reservoirs was studied based on the homogenization temperature of aqueous inclusions, thermal and burial history simulation and K-Ar dating of authigenic illite. Two episodes of gas charging in the northern part and one episode in the southern part were delineated in the reservoirs of the Hangjinqi area, evidenced by microscopic observation of the occurrence of fluid inclusions and the analysis of salinity in aqueous inclusions. In the southern part of the study area gas charging occurred between circa 171-162 Ma, whereas in the northern part gas charging was between 158-144 Ma and 120-109 Ma, respectively. The gas charging events appeared to be influenced by the tectonic evolution of northern Ordos Basin. Paleo topography caused reduction in thickness of source rocks northwards, and contributed to differences in hydrocarbon generation potential and thermal evolution between the northern and the southern part of the study area. Therefore, gas charging occurred in the southern part prior to that in the northern part. Furthermore, tilting occurred in Middle Jurassic and provided the driver and pathways for gas, leading to a first charging event in the northern part of the study area.
abstract_unstemmed	A giant gas field has been discovered in the Lower Shihezi Formation in the Hangjinqi area, northern Ordos Basin, China. Coal seams and mudstone in the Taiyuan and Shanxi Formation are considered as source rocks and sandstone in the Lower Shihezi Formation is treated as reservoirs for gas. The charging time in the sandstone reservoirs was studied based on the homogenization temperature of aqueous inclusions, thermal and burial history simulation and K-Ar dating of authigenic illite. Two episodes of gas charging in the northern part and one episode in the southern part were delineated in the reservoirs of the Hangjinqi area, evidenced by microscopic observation of the occurrence of fluid inclusions and the analysis of salinity in aqueous inclusions. In the southern part of the study area gas charging occurred between circa 171-162 Ma, whereas in the northern part gas charging was between 158-144 Ma and 120-109 Ma, respectively. The gas charging events appeared to be influenced by the tectonic evolution of northern Ordos Basin. Paleo topography caused reduction in thickness of source rocks northwards, and contributed to differences in hydrocarbon generation potential and thermal evolution between the northern and the southern part of the study area. Therefore, gas charging occurred in the southern part prior to that in the northern part. Furthermore, tilting occurred in Middle Jurassic and provided the driver and pathways for gas, leading to a first charging event in the northern part of the study area.
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title_short	Effect of tectonic evolution on hydrocarbon charging time: A case study from Lower Shihezi Formation (Guadalupian), the Hangjinqi area, northern Ordos, China
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Effect of tectonic evolution on hydrocarbon charging time: A case study from Lower Shihezi Formation (Guadalupian), the Hangjinqi area, northern Ordos, China

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