The Chang 7 member of the upper Triassic in the southwest Ordos Basin: Carbon isotope studay of dispersed organic matter and its paleoclimate significance
Abstract The carbon isotope δ13C value of dispersed organic matter in the Upper Triassic sediments in the Ordos basin is (−24.5 to −26.6) × $ 10^{−3} $ with the carbon being derived from C3-like pleustons. The paleoclimate of the Late Triassic, especially during the deposition of the Chang 7 member,...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Yang, Minghui [verfasserIn] |
|---|
| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2008 |
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| Anmerkung: |
© China University of Petroleum 2008 |
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| Übergeordnetes Werk: |
Enthalten in: Petroleum science - Beijing, 2007, 5(2008), 1 vom: Feb., Seite 20-23 |
|---|---|
| Übergeordnetes Werk: |
volume:5 ; year:2008 ; number:1 ; month:02 ; pages:20-23 |
| Links: |
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| DOI / URN: |
10.1007/s12182-008-0003-7 |
|---|
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SPR025576402 |
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| 245 | 1 | 4 | |a The Chang 7 member of the upper Triassic in the southwest Ordos Basin: Carbon isotope studay of dispersed organic matter and its paleoclimate significance |
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| 520 | |a Abstract The carbon isotope δ13C value of dispersed organic matter in the Upper Triassic sediments in the Ordos basin is (−24.5 to −26.6) × $ 10^{−3} $ with the carbon being derived from C3-like pleustons. The paleoclimate of the Late Triassic, especially during the deposition of the Chang 7 member, was characterized by a hot and humid climate. It underwent four small climate cycles from humid and warm to humid and hot. | ||
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| 700 | 1 | |a Tang, Xuan |4 aut | |
| 700 | 1 | |a Zheng, Xiaofeng |4 aut | |
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10.1007/s12182-008-0003-7 doi (DE-627)SPR025576402 (SPR)s12182-008-0003-7-e DE-627 ger DE-627 rakwb eng Yang, Minghui verfasserin aut The Chang 7 member of the upper Triassic in the southwest Ordos Basin: Carbon isotope studay of dispersed organic matter and its paleoclimate significance 2008 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © China University of Petroleum 2008 Abstract The carbon isotope δ13C value of dispersed organic matter in the Upper Triassic sediments in the Ordos basin is (−24.5 to −26.6) × $ 10^{−3} $ with the carbon being derived from C3-like pleustons. The paleoclimate of the Late Triassic, especially during the deposition of the Chang 7 member, was characterized by a hot and humid climate. It underwent four small climate cycles from humid and warm to humid and hot. Liu, Chiyang aut Tang, Xuan aut Zheng, Xiaofeng aut Enthalten in Petroleum science Beijing, 2007 5(2008), 1 vom: Feb., Seite 20-23 (DE-627)565518909 (DE-600)2424436-3 1995-8226 nnns volume:5 year:2008 number:1 month:02 pages:20-23 https://dx.doi.org/10.1007/s12182-008-0003-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_20 GBV_ILN_31 GBV_ILN_40 GBV_ILN_60 GBV_ILN_63 GBV_ILN_65 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_110 GBV_ILN_120 GBV_ILN_150 GBV_ILN_161 GBV_ILN_213 GBV_ILN_230 GBV_ILN_293 GBV_ILN_370 GBV_ILN_374 GBV_ILN_702 GBV_ILN_2027 GBV_ILN_2190 GBV_ILN_2700 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 AR 5 2008 1 02 20-23 |
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10.1007/s12182-008-0003-7 doi (DE-627)SPR025576402 (SPR)s12182-008-0003-7-e DE-627 ger DE-627 rakwb eng Yang, Minghui verfasserin aut The Chang 7 member of the upper Triassic in the southwest Ordos Basin: Carbon isotope studay of dispersed organic matter and its paleoclimate significance 2008 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © China University of Petroleum 2008 Abstract The carbon isotope δ13C value of dispersed organic matter in the Upper Triassic sediments in the Ordos basin is (−24.5 to −26.6) × $ 10^{−3} $ with the carbon being derived from C3-like pleustons. The paleoclimate of the Late Triassic, especially during the deposition of the Chang 7 member, was characterized by a hot and humid climate. It underwent four small climate cycles from humid and warm to humid and hot. Liu, Chiyang aut Tang, Xuan aut Zheng, Xiaofeng aut Enthalten in Petroleum science Beijing, 2007 5(2008), 1 vom: Feb., Seite 20-23 (DE-627)565518909 (DE-600)2424436-3 1995-8226 nnns volume:5 year:2008 number:1 month:02 pages:20-23 https://dx.doi.org/10.1007/s12182-008-0003-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_20 GBV_ILN_31 GBV_ILN_40 GBV_ILN_60 GBV_ILN_63 GBV_ILN_65 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_110 GBV_ILN_120 GBV_ILN_150 GBV_ILN_161 GBV_ILN_213 GBV_ILN_230 GBV_ILN_293 GBV_ILN_370 GBV_ILN_374 GBV_ILN_702 GBV_ILN_2027 GBV_ILN_2190 GBV_ILN_2700 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 AR 5 2008 1 02 20-23 |
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10.1007/s12182-008-0003-7 doi (DE-627)SPR025576402 (SPR)s12182-008-0003-7-e DE-627 ger DE-627 rakwb eng Yang, Minghui verfasserin aut The Chang 7 member of the upper Triassic in the southwest Ordos Basin: Carbon isotope studay of dispersed organic matter and its paleoclimate significance 2008 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © China University of Petroleum 2008 Abstract The carbon isotope δ13C value of dispersed organic matter in the Upper Triassic sediments in the Ordos basin is (−24.5 to −26.6) × $ 10^{−3} $ with the carbon being derived from C3-like pleustons. The paleoclimate of the Late Triassic, especially during the deposition of the Chang 7 member, was characterized by a hot and humid climate. It underwent four small climate cycles from humid and warm to humid and hot. Liu, Chiyang aut Tang, Xuan aut Zheng, Xiaofeng aut Enthalten in Petroleum science Beijing, 2007 5(2008), 1 vom: Feb., Seite 20-23 (DE-627)565518909 (DE-600)2424436-3 1995-8226 nnns volume:5 year:2008 number:1 month:02 pages:20-23 https://dx.doi.org/10.1007/s12182-008-0003-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_20 GBV_ILN_31 GBV_ILN_40 GBV_ILN_60 GBV_ILN_63 GBV_ILN_65 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_110 GBV_ILN_120 GBV_ILN_150 GBV_ILN_161 GBV_ILN_213 GBV_ILN_230 GBV_ILN_293 GBV_ILN_370 GBV_ILN_374 GBV_ILN_702 GBV_ILN_2027 GBV_ILN_2190 GBV_ILN_2700 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 AR 5 2008 1 02 20-23 |
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10.1007/s12182-008-0003-7 doi (DE-627)SPR025576402 (SPR)s12182-008-0003-7-e DE-627 ger DE-627 rakwb eng Yang, Minghui verfasserin aut The Chang 7 member of the upper Triassic in the southwest Ordos Basin: Carbon isotope studay of dispersed organic matter and its paleoclimate significance 2008 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © China University of Petroleum 2008 Abstract The carbon isotope δ13C value of dispersed organic matter in the Upper Triassic sediments in the Ordos basin is (−24.5 to −26.6) × $ 10^{−3} $ with the carbon being derived from C3-like pleustons. The paleoclimate of the Late Triassic, especially during the deposition of the Chang 7 member, was characterized by a hot and humid climate. It underwent four small climate cycles from humid and warm to humid and hot. Liu, Chiyang aut Tang, Xuan aut Zheng, Xiaofeng aut Enthalten in Petroleum science Beijing, 2007 5(2008), 1 vom: Feb., Seite 20-23 (DE-627)565518909 (DE-600)2424436-3 1995-8226 nnns volume:5 year:2008 number:1 month:02 pages:20-23 https://dx.doi.org/10.1007/s12182-008-0003-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_20 GBV_ILN_31 GBV_ILN_40 GBV_ILN_60 GBV_ILN_63 GBV_ILN_65 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_110 GBV_ILN_120 GBV_ILN_150 GBV_ILN_161 GBV_ILN_213 GBV_ILN_230 GBV_ILN_293 GBV_ILN_370 GBV_ILN_374 GBV_ILN_702 GBV_ILN_2027 GBV_ILN_2190 GBV_ILN_2700 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 AR 5 2008 1 02 20-23 |
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10.1007/s12182-008-0003-7 doi (DE-627)SPR025576402 (SPR)s12182-008-0003-7-e DE-627 ger DE-627 rakwb eng Yang, Minghui verfasserin aut The Chang 7 member of the upper Triassic in the southwest Ordos Basin: Carbon isotope studay of dispersed organic matter and its paleoclimate significance 2008 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © China University of Petroleum 2008 Abstract The carbon isotope δ13C value of dispersed organic matter in the Upper Triassic sediments in the Ordos basin is (−24.5 to −26.6) × $ 10^{−3} $ with the carbon being derived from C3-like pleustons. The paleoclimate of the Late Triassic, especially during the deposition of the Chang 7 member, was characterized by a hot and humid climate. It underwent four small climate cycles from humid and warm to humid and hot. Liu, Chiyang aut Tang, Xuan aut Zheng, Xiaofeng aut Enthalten in Petroleum science Beijing, 2007 5(2008), 1 vom: Feb., Seite 20-23 (DE-627)565518909 (DE-600)2424436-3 1995-8226 nnns volume:5 year:2008 number:1 month:02 pages:20-23 https://dx.doi.org/10.1007/s12182-008-0003-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_20 GBV_ILN_31 GBV_ILN_40 GBV_ILN_60 GBV_ILN_63 GBV_ILN_65 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_110 GBV_ILN_120 GBV_ILN_150 GBV_ILN_161 GBV_ILN_213 GBV_ILN_230 GBV_ILN_293 GBV_ILN_370 GBV_ILN_374 GBV_ILN_702 GBV_ILN_2027 GBV_ILN_2190 GBV_ILN_2700 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 AR 5 2008 1 02 20-23 |
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Yang, Minghui Liu, Chiyang Tang, Xuan Zheng, Xiaofeng |
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Elektronische Aufsätze |
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Yang, Minghui |
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10.1007/s12182-008-0003-7 |
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chang 7 member of the upper triassic in the southwest ordos basin: carbon isotope studay of dispersed organic matter and its paleoclimate significance |
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The Chang 7 member of the upper Triassic in the southwest Ordos Basin: Carbon isotope studay of dispersed organic matter and its paleoclimate significance |
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Abstract The carbon isotope δ13C value of dispersed organic matter in the Upper Triassic sediments in the Ordos basin is (−24.5 to −26.6) × $ 10^{−3} $ with the carbon being derived from C3-like pleustons. The paleoclimate of the Late Triassic, especially during the deposition of the Chang 7 member, was characterized by a hot and humid climate. It underwent four small climate cycles from humid and warm to humid and hot. © China University of Petroleum 2008 |
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Abstract The carbon isotope δ13C value of dispersed organic matter in the Upper Triassic sediments in the Ordos basin is (−24.5 to −26.6) × $ 10^{−3} $ with the carbon being derived from C3-like pleustons. The paleoclimate of the Late Triassic, especially during the deposition of the Chang 7 member, was characterized by a hot and humid climate. It underwent four small climate cycles from humid and warm to humid and hot. © China University of Petroleum 2008 |
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Abstract The carbon isotope δ13C value of dispersed organic matter in the Upper Triassic sediments in the Ordos basin is (−24.5 to −26.6) × $ 10^{−3} $ with the carbon being derived from C3-like pleustons. The paleoclimate of the Late Triassic, especially during the deposition of the Chang 7 member, was characterized by a hot and humid climate. It underwent four small climate cycles from humid and warm to humid and hot. © China University of Petroleum 2008 |
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The Chang 7 member of the upper Triassic in the southwest Ordos Basin: Carbon isotope studay of dispersed organic matter and its paleoclimate significance |
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