Geochemical characteristics and accumulation of marine oil and gas around Halahatang depression, Tarim Basin, China
Abstract There exists a petroleum system rich of oil and gas around Halahatang depression, where the oil and gas possess obvious local distinctions of properties in different parts. The research proved that the discovered crude oil and natural gas in the region derived mainly from $ O_{2+3} $ source...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Lu, YuHong [verfasserIn] |
|---|
| Format: |
Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2008 |
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| Schlagwörter: |
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| Anmerkung: |
© Science in China Press and Springer-Verlag GmbH 2008 |
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| Übergeordnetes Werk: |
Enthalten in: Science in China / D - SP Science in China Press, 1996, 51(2008), Suppl 1 vom: Mai, Seite 195-206 |
|---|---|
| Übergeordnetes Werk: |
volume:51 ; year:2008 ; number:Suppl 1 ; month:05 ; pages:195-206 |
| Links: |
|---|
| DOI / URN: |
10.1007/s11430-008-5006-0 |
|---|
| Katalog-ID: |
OLC2063782903 |
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| 245 | 1 | 0 | |a Geochemical characteristics and accumulation of marine oil and gas around Halahatang depression, Tarim Basin, China |
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| 520 | |a Abstract There exists a petroleum system rich of oil and gas around Halahatang depression, where the oil and gas possess obvious local distinctions of properties in different parts. The research proved that the discovered crude oil and natural gas in the region derived mainly from $ O_{2+3} $ source rock, and the differences of its properties were controlled by the oil and gas filling intensity. The comprehensive study result shows the oil and gas reservoirs of the region mainly underwent three important accumulation phases: late Caledonian-Early Hercynian epoch, late Hercynian epoch, and Yanshan-Himalayan epoch. In the first phase, the oil and gas derived mostly from Cambrian source rock, which formed the primary ancient oil reservoirs, then suffered strong degradation and remained a great quantity of pyrobitumen in the high position of Tabei uplift in the present. In the second phase, the $ O_{2+3} $ source rock of Manjia’er depression started its generation of hydrocarbon, which accumulated in the high position of Tabei up-lift afterwards, and then biodegradated to heavy oil in the late Hercynian epoch. In the last phase, the $ O_{2+3} $ source rock of southern Halahatang depression and margin of Manjia’er depression started its peak of generating liquid hydrocarbon, which mostly accumulated in the trap formed before the Indo-China and Yanshan epoch, and in somewhere the heavy oil suffered dilutions in various degrees or serious gas invading, to lead to obvious crude oil divergence. | ||
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10.1007/s11430-008-5006-0 doi (DE-627)OLC2063782903 (DE-He213)s11430-008-5006-0-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Lu, YuHong verfasserin aut Geochemical characteristics and accumulation of marine oil and gas around Halahatang depression, Tarim Basin, China 2008 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Science in China Press and Springer-Verlag GmbH 2008 Abstract There exists a petroleum system rich of oil and gas around Halahatang depression, where the oil and gas possess obvious local distinctions of properties in different parts. The research proved that the discovered crude oil and natural gas in the region derived mainly from $ O_{2+3} $ source rock, and the differences of its properties were controlled by the oil and gas filling intensity. The comprehensive study result shows the oil and gas reservoirs of the region mainly underwent three important accumulation phases: late Caledonian-Early Hercynian epoch, late Hercynian epoch, and Yanshan-Himalayan epoch. In the first phase, the oil and gas derived mostly from Cambrian source rock, which formed the primary ancient oil reservoirs, then suffered strong degradation and remained a great quantity of pyrobitumen in the high position of Tabei uplift in the present. In the second phase, the $ O_{2+3} $ source rock of Manjia’er depression started its generation of hydrocarbon, which accumulated in the high position of Tabei up-lift afterwards, and then biodegradated to heavy oil in the late Hercynian epoch. In the last phase, the $ O_{2+3} $ source rock of southern Halahatang depression and margin of Manjia’er depression started its peak of generating liquid hydrocarbon, which mostly accumulated in the trap formed before the Indo-China and Yanshan epoch, and in somewhere the heavy oil suffered dilutions in various degrees or serious gas invading, to lead to obvious crude oil divergence. marine facies Mid-Upper Ordovician source rock oil and gas source accumulation stage Halahatang depression Tarim Basin Xiao, ZhongYao aut Gu, QiaoYuan aut Zhang, QiuCha aut Enthalten in Science in China / D SP Science in China Press, 1996 51(2008), Suppl 1 vom: Mai, Seite 195-206 (DE-627)193118238 (DE-600)1307899-9 (DE-576)062316923 1006-9313 nnns volume:51 year:2008 number:Suppl 1 month:05 pages:195-206 https://doi.org/10.1007/s11430-008-5006-0 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-OAS SSG-OLC-MFO SSG-OPC-GGO GBV_ILN_70 GBV_ILN_267 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4082 AR 51 2008 Suppl 1 05 195-206 |
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10.1007/s11430-008-5006-0 doi (DE-627)OLC2063782903 (DE-He213)s11430-008-5006-0-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Lu, YuHong verfasserin aut Geochemical characteristics and accumulation of marine oil and gas around Halahatang depression, Tarim Basin, China 2008 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Science in China Press and Springer-Verlag GmbH 2008 Abstract There exists a petroleum system rich of oil and gas around Halahatang depression, where the oil and gas possess obvious local distinctions of properties in different parts. The research proved that the discovered crude oil and natural gas in the region derived mainly from $ O_{2+3} $ source rock, and the differences of its properties were controlled by the oil and gas filling intensity. The comprehensive study result shows the oil and gas reservoirs of the region mainly underwent three important accumulation phases: late Caledonian-Early Hercynian epoch, late Hercynian epoch, and Yanshan-Himalayan epoch. In the first phase, the oil and gas derived mostly from Cambrian source rock, which formed the primary ancient oil reservoirs, then suffered strong degradation and remained a great quantity of pyrobitumen in the high position of Tabei uplift in the present. In the second phase, the $ O_{2+3} $ source rock of Manjia’er depression started its generation of hydrocarbon, which accumulated in the high position of Tabei up-lift afterwards, and then biodegradated to heavy oil in the late Hercynian epoch. In the last phase, the $ O_{2+3} $ source rock of southern Halahatang depression and margin of Manjia’er depression started its peak of generating liquid hydrocarbon, which mostly accumulated in the trap formed before the Indo-China and Yanshan epoch, and in somewhere the heavy oil suffered dilutions in various degrees or serious gas invading, to lead to obvious crude oil divergence. marine facies Mid-Upper Ordovician source rock oil and gas source accumulation stage Halahatang depression Tarim Basin Xiao, ZhongYao aut Gu, QiaoYuan aut Zhang, QiuCha aut Enthalten in Science in China / D SP Science in China Press, 1996 51(2008), Suppl 1 vom: Mai, Seite 195-206 (DE-627)193118238 (DE-600)1307899-9 (DE-576)062316923 1006-9313 nnns volume:51 year:2008 number:Suppl 1 month:05 pages:195-206 https://doi.org/10.1007/s11430-008-5006-0 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-OAS SSG-OLC-MFO SSG-OPC-GGO GBV_ILN_70 GBV_ILN_267 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4082 AR 51 2008 Suppl 1 05 195-206 |
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10.1007/s11430-008-5006-0 doi (DE-627)OLC2063782903 (DE-He213)s11430-008-5006-0-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Lu, YuHong verfasserin aut Geochemical characteristics and accumulation of marine oil and gas around Halahatang depression, Tarim Basin, China 2008 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Science in China Press and Springer-Verlag GmbH 2008 Abstract There exists a petroleum system rich of oil and gas around Halahatang depression, where the oil and gas possess obvious local distinctions of properties in different parts. The research proved that the discovered crude oil and natural gas in the region derived mainly from $ O_{2+3} $ source rock, and the differences of its properties were controlled by the oil and gas filling intensity. The comprehensive study result shows the oil and gas reservoirs of the region mainly underwent three important accumulation phases: late Caledonian-Early Hercynian epoch, late Hercynian epoch, and Yanshan-Himalayan epoch. In the first phase, the oil and gas derived mostly from Cambrian source rock, which formed the primary ancient oil reservoirs, then suffered strong degradation and remained a great quantity of pyrobitumen in the high position of Tabei uplift in the present. In the second phase, the $ O_{2+3} $ source rock of Manjia’er depression started its generation of hydrocarbon, which accumulated in the high position of Tabei up-lift afterwards, and then biodegradated to heavy oil in the late Hercynian epoch. In the last phase, the $ O_{2+3} $ source rock of southern Halahatang depression and margin of Manjia’er depression started its peak of generating liquid hydrocarbon, which mostly accumulated in the trap formed before the Indo-China and Yanshan epoch, and in somewhere the heavy oil suffered dilutions in various degrees or serious gas invading, to lead to obvious crude oil divergence. marine facies Mid-Upper Ordovician source rock oil and gas source accumulation stage Halahatang depression Tarim Basin Xiao, ZhongYao aut Gu, QiaoYuan aut Zhang, QiuCha aut Enthalten in Science in China / D SP Science in China Press, 1996 51(2008), Suppl 1 vom: Mai, Seite 195-206 (DE-627)193118238 (DE-600)1307899-9 (DE-576)062316923 1006-9313 nnns volume:51 year:2008 number:Suppl 1 month:05 pages:195-206 https://doi.org/10.1007/s11430-008-5006-0 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-OAS SSG-OLC-MFO SSG-OPC-GGO GBV_ILN_70 GBV_ILN_267 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4082 AR 51 2008 Suppl 1 05 195-206 |
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10.1007/s11430-008-5006-0 doi (DE-627)OLC2063782903 (DE-He213)s11430-008-5006-0-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Lu, YuHong verfasserin aut Geochemical characteristics and accumulation of marine oil and gas around Halahatang depression, Tarim Basin, China 2008 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Science in China Press and Springer-Verlag GmbH 2008 Abstract There exists a petroleum system rich of oil and gas around Halahatang depression, where the oil and gas possess obvious local distinctions of properties in different parts. The research proved that the discovered crude oil and natural gas in the region derived mainly from $ O_{2+3} $ source rock, and the differences of its properties were controlled by the oil and gas filling intensity. The comprehensive study result shows the oil and gas reservoirs of the region mainly underwent three important accumulation phases: late Caledonian-Early Hercynian epoch, late Hercynian epoch, and Yanshan-Himalayan epoch. In the first phase, the oil and gas derived mostly from Cambrian source rock, which formed the primary ancient oil reservoirs, then suffered strong degradation and remained a great quantity of pyrobitumen in the high position of Tabei uplift in the present. In the second phase, the $ O_{2+3} $ source rock of Manjia’er depression started its generation of hydrocarbon, which accumulated in the high position of Tabei up-lift afterwards, and then biodegradated to heavy oil in the late Hercynian epoch. In the last phase, the $ O_{2+3} $ source rock of southern Halahatang depression and margin of Manjia’er depression started its peak of generating liquid hydrocarbon, which mostly accumulated in the trap formed before the Indo-China and Yanshan epoch, and in somewhere the heavy oil suffered dilutions in various degrees or serious gas invading, to lead to obvious crude oil divergence. marine facies Mid-Upper Ordovician source rock oil and gas source accumulation stage Halahatang depression Tarim Basin Xiao, ZhongYao aut Gu, QiaoYuan aut Zhang, QiuCha aut Enthalten in Science in China / D SP Science in China Press, 1996 51(2008), Suppl 1 vom: Mai, Seite 195-206 (DE-627)193118238 (DE-600)1307899-9 (DE-576)062316923 1006-9313 nnns volume:51 year:2008 number:Suppl 1 month:05 pages:195-206 https://doi.org/10.1007/s11430-008-5006-0 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-OAS SSG-OLC-MFO SSG-OPC-GGO GBV_ILN_70 GBV_ILN_267 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4082 AR 51 2008 Suppl 1 05 195-206 |
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10.1007/s11430-008-5006-0 doi (DE-627)OLC2063782903 (DE-He213)s11430-008-5006-0-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Lu, YuHong verfasserin aut Geochemical characteristics and accumulation of marine oil and gas around Halahatang depression, Tarim Basin, China 2008 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Science in China Press and Springer-Verlag GmbH 2008 Abstract There exists a petroleum system rich of oil and gas around Halahatang depression, where the oil and gas possess obvious local distinctions of properties in different parts. The research proved that the discovered crude oil and natural gas in the region derived mainly from $ O_{2+3} $ source rock, and the differences of its properties were controlled by the oil and gas filling intensity. The comprehensive study result shows the oil and gas reservoirs of the region mainly underwent three important accumulation phases: late Caledonian-Early Hercynian epoch, late Hercynian epoch, and Yanshan-Himalayan epoch. In the first phase, the oil and gas derived mostly from Cambrian source rock, which formed the primary ancient oil reservoirs, then suffered strong degradation and remained a great quantity of pyrobitumen in the high position of Tabei uplift in the present. In the second phase, the $ O_{2+3} $ source rock of Manjia’er depression started its generation of hydrocarbon, which accumulated in the high position of Tabei up-lift afterwards, and then biodegradated to heavy oil in the late Hercynian epoch. In the last phase, the $ O_{2+3} $ source rock of southern Halahatang depression and margin of Manjia’er depression started its peak of generating liquid hydrocarbon, which mostly accumulated in the trap formed before the Indo-China and Yanshan epoch, and in somewhere the heavy oil suffered dilutions in various degrees or serious gas invading, to lead to obvious crude oil divergence. marine facies Mid-Upper Ordovician source rock oil and gas source accumulation stage Halahatang depression Tarim Basin Xiao, ZhongYao aut Gu, QiaoYuan aut Zhang, QiuCha aut Enthalten in Science in China / D SP Science in China Press, 1996 51(2008), Suppl 1 vom: Mai, Seite 195-206 (DE-627)193118238 (DE-600)1307899-9 (DE-576)062316923 1006-9313 nnns volume:51 year:2008 number:Suppl 1 month:05 pages:195-206 https://doi.org/10.1007/s11430-008-5006-0 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-OAS SSG-OLC-MFO SSG-OPC-GGO GBV_ILN_70 GBV_ILN_267 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4082 AR 51 2008 Suppl 1 05 195-206 |
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Lu, YuHong |
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Lu, YuHong ddc 550 ssgn 13 misc marine facies misc Mid-Upper Ordovician source rock misc oil and gas source misc accumulation stage misc Halahatang depression misc Tarim Basin Geochemical characteristics and accumulation of marine oil and gas around Halahatang depression, Tarim Basin, China |
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550 VZ 13 ssgn Geochemical characteristics and accumulation of marine oil and gas around Halahatang depression, Tarim Basin, China marine facies Mid-Upper Ordovician source rock oil and gas source accumulation stage Halahatang depression Tarim Basin |
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Geochemical characteristics and accumulation of marine oil and gas around Halahatang depression, Tarim Basin, China |
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Geochemical characteristics and accumulation of marine oil and gas around Halahatang depression, Tarim Basin, China |
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geochemical characteristics and accumulation of marine oil and gas around halahatang depression, tarim basin, china |
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Geochemical characteristics and accumulation of marine oil and gas around Halahatang depression, Tarim Basin, China |
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Abstract There exists a petroleum system rich of oil and gas around Halahatang depression, where the oil and gas possess obvious local distinctions of properties in different parts. The research proved that the discovered crude oil and natural gas in the region derived mainly from $ O_{2+3} $ source rock, and the differences of its properties were controlled by the oil and gas filling intensity. The comprehensive study result shows the oil and gas reservoirs of the region mainly underwent three important accumulation phases: late Caledonian-Early Hercynian epoch, late Hercynian epoch, and Yanshan-Himalayan epoch. In the first phase, the oil and gas derived mostly from Cambrian source rock, which formed the primary ancient oil reservoirs, then suffered strong degradation and remained a great quantity of pyrobitumen in the high position of Tabei uplift in the present. In the second phase, the $ O_{2+3} $ source rock of Manjia’er depression started its generation of hydrocarbon, which accumulated in the high position of Tabei up-lift afterwards, and then biodegradated to heavy oil in the late Hercynian epoch. In the last phase, the $ O_{2+3} $ source rock of southern Halahatang depression and margin of Manjia’er depression started its peak of generating liquid hydrocarbon, which mostly accumulated in the trap formed before the Indo-China and Yanshan epoch, and in somewhere the heavy oil suffered dilutions in various degrees or serious gas invading, to lead to obvious crude oil divergence. © Science in China Press and Springer-Verlag GmbH 2008 |
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Abstract There exists a petroleum system rich of oil and gas around Halahatang depression, where the oil and gas possess obvious local distinctions of properties in different parts. The research proved that the discovered crude oil and natural gas in the region derived mainly from $ O_{2+3} $ source rock, and the differences of its properties were controlled by the oil and gas filling intensity. The comprehensive study result shows the oil and gas reservoirs of the region mainly underwent three important accumulation phases: late Caledonian-Early Hercynian epoch, late Hercynian epoch, and Yanshan-Himalayan epoch. In the first phase, the oil and gas derived mostly from Cambrian source rock, which formed the primary ancient oil reservoirs, then suffered strong degradation and remained a great quantity of pyrobitumen in the high position of Tabei uplift in the present. In the second phase, the $ O_{2+3} $ source rock of Manjia’er depression started its generation of hydrocarbon, which accumulated in the high position of Tabei up-lift afterwards, and then biodegradated to heavy oil in the late Hercynian epoch. In the last phase, the $ O_{2+3} $ source rock of southern Halahatang depression and margin of Manjia’er depression started its peak of generating liquid hydrocarbon, which mostly accumulated in the trap formed before the Indo-China and Yanshan epoch, and in somewhere the heavy oil suffered dilutions in various degrees or serious gas invading, to lead to obvious crude oil divergence. © Science in China Press and Springer-Verlag GmbH 2008 |
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Abstract There exists a petroleum system rich of oil and gas around Halahatang depression, where the oil and gas possess obvious local distinctions of properties in different parts. The research proved that the discovered crude oil and natural gas in the region derived mainly from $ O_{2+3} $ source rock, and the differences of its properties were controlled by the oil and gas filling intensity. The comprehensive study result shows the oil and gas reservoirs of the region mainly underwent three important accumulation phases: late Caledonian-Early Hercynian epoch, late Hercynian epoch, and Yanshan-Himalayan epoch. In the first phase, the oil and gas derived mostly from Cambrian source rock, which formed the primary ancient oil reservoirs, then suffered strong degradation and remained a great quantity of pyrobitumen in the high position of Tabei uplift in the present. In the second phase, the $ O_{2+3} $ source rock of Manjia’er depression started its generation of hydrocarbon, which accumulated in the high position of Tabei up-lift afterwards, and then biodegradated to heavy oil in the late Hercynian epoch. In the last phase, the $ O_{2+3} $ source rock of southern Halahatang depression and margin of Manjia’er depression started its peak of generating liquid hydrocarbon, which mostly accumulated in the trap formed before the Indo-China and Yanshan epoch, and in somewhere the heavy oil suffered dilutions in various degrees or serious gas invading, to lead to obvious crude oil divergence. © Science in China Press and Springer-Verlag GmbH 2008 |
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