Organic geochemical signatures of source rocks and oil-source correlation in the Papuan Basin, Papua New Guinea
The Papuan Basin is the largest petroliferous basin in Papua New Guinea (PNG), where developed several sets of potential source rocks (SRs). The Jurassic SRs are clay-rich shales, whose organic matter (OM, mainly type Ⅱ2-Ⅲ) is predominantly derived from terrestrial higher plants deposited in a more...
Ausführliche Beschreibung
Autor*in: |
Xu, Min [verfasserIn] |
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E-Artikel |
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Sprache: |
Englisch |
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2022transfer abstract |
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Übergeordnetes Werk: |
Enthalten in: Iterated Gilbert mosaics - Baccelli, Francois ELSEVIER, 2019, Amsterdam [u.a.] |
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Übergeordnetes Werk: |
volume:210 ; year:2022 ; pages:0 |
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DOI / URN: |
10.1016/j.petrol.2021.109972 |
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ELV056641583 |
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520 | |a The Papuan Basin is the largest petroliferous basin in Papua New Guinea (PNG), where developed several sets of potential source rocks (SRs). The Jurassic SRs are clay-rich shales, whose organic matter (OM, mainly type Ⅱ2-Ⅲ) is predominantly derived from terrestrial higher plants deposited in a more oxic environment with relatively high maturity (0.35% 2, the mild dominance of C29 ααα 20 R sterane and the absence of oleanane ± lupane. Type C2 oils can be clearly distinguished from Type C3 by C19/(C19 + C23) tricyclic terpane <0.5, while the latter ones have higher abundances of oleanane ± lupine and diahopanes as well as C24 tetracyclic/C23 tricyclic terpane ratios. Type C2-3 oils are originated from calcareous SRs that deposited in Late Cretaceous or younger age. | ||
520 | |a The Papuan Basin is the largest petroliferous basin in Papua New Guinea (PNG), where developed several sets of potential source rocks (SRs). The Jurassic SRs are clay-rich shales, whose organic matter (OM, mainly type Ⅱ2-Ⅲ) is predominantly derived from terrestrial higher plants deposited in a more oxic environment with relatively high maturity (0.35% 2, the mild dominance of C29 ααα 20 R sterane and the absence of oleanane ± lupane. Type C2 oils can be clearly distinguished from Type C3 by C19/(C19 + C23) tricyclic terpane <0.5, while the latter ones have higher abundances of oleanane ± lupine and diahopanes as well as C24 tetracyclic/C23 tricyclic terpane ratios. Type C2-3 oils are originated from calcareous SRs that deposited in Late Cretaceous or younger age. | ||
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10.1016/j.petrol.2021.109972 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001658.pica (DE-627)ELV056641583 (ELSEVIER)S0920-4105(21)01586-2 DE-627 ger DE-627 rakwb eng 510 VZ 31.70 bkl Xu, Min verfasserin aut Organic geochemical signatures of source rocks and oil-source correlation in the Papuan Basin, Papua New Guinea 2022transfer abstract nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier The Papuan Basin is the largest petroliferous basin in Papua New Guinea (PNG), where developed several sets of potential source rocks (SRs). The Jurassic SRs are clay-rich shales, whose organic matter (OM, mainly type Ⅱ2-Ⅲ) is predominantly derived from terrestrial higher plants deposited in a more oxic environment with relatively high maturity (0.35% 2, the mild dominance of C29 ααα 20 R sterane and the absence of oleanane ± lupane. Type C2 oils can be clearly distinguished from Type C3 by C19/(C19 + C23) tricyclic terpane <0.5, while the latter ones have higher abundances of oleanane ± lupine and diahopanes as well as C24 tetracyclic/C23 tricyclic terpane ratios. Type C2-3 oils are originated from calcareous SRs that deposited in Late Cretaceous or younger age. The Papuan Basin is the largest petroliferous basin in Papua New Guinea (PNG), where developed several sets of potential source rocks (SRs). The Jurassic SRs are clay-rich shales, whose organic matter (OM, mainly type Ⅱ2-Ⅲ) is predominantly derived from terrestrial higher plants deposited in a more oxic environment with relatively high maturity (0.35% 2, the mild dominance of C29 ααα 20 R sterane and the absence of oleanane ± lupane. Type C2 oils can be clearly distinguished from Type C3 by C19/(C19 + C23) tricyclic terpane <0.5, while the latter ones have higher abundances of oleanane ± lupine and diahopanes as well as C24 tetracyclic/C23 tricyclic terpane ratios. Type C2-3 oils are originated from calcareous SRs that deposited in Late Cretaceous or younger age. Source rocks Elsevier Oil-source rock correlation Elsevier Organic geochemistry Elsevier The papuan basin Elsevier Genetic oil families Elsevier Hou, Dujie oth Lin, Xiaoyun oth Liu, Jian oth Ding, Wenjing oth Xie, Rui oth Enthalten in Elsevier Science Baccelli, Francois ELSEVIER Iterated Gilbert mosaics 2019 Amsterdam [u.a.] (DE-627)ELV008094314 volume:210 year:2022 pages:0 https://doi.org/10.1016/j.petrol.2021.109972 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OPC-MAT 31.70 Wahrscheinlichkeitsrechnung VZ AR 210 2022 0 |
spelling |
10.1016/j.petrol.2021.109972 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001658.pica (DE-627)ELV056641583 (ELSEVIER)S0920-4105(21)01586-2 DE-627 ger DE-627 rakwb eng 510 VZ 31.70 bkl Xu, Min verfasserin aut Organic geochemical signatures of source rocks and oil-source correlation in the Papuan Basin, Papua New Guinea 2022transfer abstract nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier The Papuan Basin is the largest petroliferous basin in Papua New Guinea (PNG), where developed several sets of potential source rocks (SRs). The Jurassic SRs are clay-rich shales, whose organic matter (OM, mainly type Ⅱ2-Ⅲ) is predominantly derived from terrestrial higher plants deposited in a more oxic environment with relatively high maturity (0.35% 2, the mild dominance of C29 ααα 20 R sterane and the absence of oleanane ± lupane. Type C2 oils can be clearly distinguished from Type C3 by C19/(C19 + C23) tricyclic terpane <0.5, while the latter ones have higher abundances of oleanane ± lupine and diahopanes as well as C24 tetracyclic/C23 tricyclic terpane ratios. Type C2-3 oils are originated from calcareous SRs that deposited in Late Cretaceous or younger age. The Papuan Basin is the largest petroliferous basin in Papua New Guinea (PNG), where developed several sets of potential source rocks (SRs). The Jurassic SRs are clay-rich shales, whose organic matter (OM, mainly type Ⅱ2-Ⅲ) is predominantly derived from terrestrial higher plants deposited in a more oxic environment with relatively high maturity (0.35% 2, the mild dominance of C29 ααα 20 R sterane and the absence of oleanane ± lupane. Type C2 oils can be clearly distinguished from Type C3 by C19/(C19 + C23) tricyclic terpane <0.5, while the latter ones have higher abundances of oleanane ± lupine and diahopanes as well as C24 tetracyclic/C23 tricyclic terpane ratios. Type C2-3 oils are originated from calcareous SRs that deposited in Late Cretaceous or younger age. Source rocks Elsevier Oil-source rock correlation Elsevier Organic geochemistry Elsevier The papuan basin Elsevier Genetic oil families Elsevier Hou, Dujie oth Lin, Xiaoyun oth Liu, Jian oth Ding, Wenjing oth Xie, Rui oth Enthalten in Elsevier Science Baccelli, Francois ELSEVIER Iterated Gilbert mosaics 2019 Amsterdam [u.a.] (DE-627)ELV008094314 volume:210 year:2022 pages:0 https://doi.org/10.1016/j.petrol.2021.109972 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OPC-MAT 31.70 Wahrscheinlichkeitsrechnung VZ AR 210 2022 0 |
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10.1016/j.petrol.2021.109972 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001658.pica (DE-627)ELV056641583 (ELSEVIER)S0920-4105(21)01586-2 DE-627 ger DE-627 rakwb eng 510 VZ 31.70 bkl Xu, Min verfasserin aut Organic geochemical signatures of source rocks and oil-source correlation in the Papuan Basin, Papua New Guinea 2022transfer abstract nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier The Papuan Basin is the largest petroliferous basin in Papua New Guinea (PNG), where developed several sets of potential source rocks (SRs). The Jurassic SRs are clay-rich shales, whose organic matter (OM, mainly type Ⅱ2-Ⅲ) is predominantly derived from terrestrial higher plants deposited in a more oxic environment with relatively high maturity (0.35% 2, the mild dominance of C29 ααα 20 R sterane and the absence of oleanane ± lupane. Type C2 oils can be clearly distinguished from Type C3 by C19/(C19 + C23) tricyclic terpane <0.5, while the latter ones have higher abundances of oleanane ± lupine and diahopanes as well as C24 tetracyclic/C23 tricyclic terpane ratios. Type C2-3 oils are originated from calcareous SRs that deposited in Late Cretaceous or younger age. The Papuan Basin is the largest petroliferous basin in Papua New Guinea (PNG), where developed several sets of potential source rocks (SRs). The Jurassic SRs are clay-rich shales, whose organic matter (OM, mainly type Ⅱ2-Ⅲ) is predominantly derived from terrestrial higher plants deposited in a more oxic environment with relatively high maturity (0.35% 2, the mild dominance of C29 ααα 20 R sterane and the absence of oleanane ± lupane. Type C2 oils can be clearly distinguished from Type C3 by C19/(C19 + C23) tricyclic terpane <0.5, while the latter ones have higher abundances of oleanane ± lupine and diahopanes as well as C24 tetracyclic/C23 tricyclic terpane ratios. Type C2-3 oils are originated from calcareous SRs that deposited in Late Cretaceous or younger age. Source rocks Elsevier Oil-source rock correlation Elsevier Organic geochemistry Elsevier The papuan basin Elsevier Genetic oil families Elsevier Hou, Dujie oth Lin, Xiaoyun oth Liu, Jian oth Ding, Wenjing oth Xie, Rui oth Enthalten in Elsevier Science Baccelli, Francois ELSEVIER Iterated Gilbert mosaics 2019 Amsterdam [u.a.] (DE-627)ELV008094314 volume:210 year:2022 pages:0 https://doi.org/10.1016/j.petrol.2021.109972 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OPC-MAT 31.70 Wahrscheinlichkeitsrechnung VZ AR 210 2022 0 |
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10.1016/j.petrol.2021.109972 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001658.pica (DE-627)ELV056641583 (ELSEVIER)S0920-4105(21)01586-2 DE-627 ger DE-627 rakwb eng 510 VZ 31.70 bkl Xu, Min verfasserin aut Organic geochemical signatures of source rocks and oil-source correlation in the Papuan Basin, Papua New Guinea 2022transfer abstract nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier The Papuan Basin is the largest petroliferous basin in Papua New Guinea (PNG), where developed several sets of potential source rocks (SRs). The Jurassic SRs are clay-rich shales, whose organic matter (OM, mainly type Ⅱ2-Ⅲ) is predominantly derived from terrestrial higher plants deposited in a more oxic environment with relatively high maturity (0.35% 2, the mild dominance of C29 ααα 20 R sterane and the absence of oleanane ± lupane. Type C2 oils can be clearly distinguished from Type C3 by C19/(C19 + C23) tricyclic terpane <0.5, while the latter ones have higher abundances of oleanane ± lupine and diahopanes as well as C24 tetracyclic/C23 tricyclic terpane ratios. Type C2-3 oils are originated from calcareous SRs that deposited in Late Cretaceous or younger age. The Papuan Basin is the largest petroliferous basin in Papua New Guinea (PNG), where developed several sets of potential source rocks (SRs). The Jurassic SRs are clay-rich shales, whose organic matter (OM, mainly type Ⅱ2-Ⅲ) is predominantly derived from terrestrial higher plants deposited in a more oxic environment with relatively high maturity (0.35% 2, the mild dominance of C29 ααα 20 R sterane and the absence of oleanane ± lupane. Type C2 oils can be clearly distinguished from Type C3 by C19/(C19 + C23) tricyclic terpane <0.5, while the latter ones have higher abundances of oleanane ± lupine and diahopanes as well as C24 tetracyclic/C23 tricyclic terpane ratios. Type C2-3 oils are originated from calcareous SRs that deposited in Late Cretaceous or younger age. Source rocks Elsevier Oil-source rock correlation Elsevier Organic geochemistry Elsevier The papuan basin Elsevier Genetic oil families Elsevier Hou, Dujie oth Lin, Xiaoyun oth Liu, Jian oth Ding, Wenjing oth Xie, Rui oth Enthalten in Elsevier Science Baccelli, Francois ELSEVIER Iterated Gilbert mosaics 2019 Amsterdam [u.a.] (DE-627)ELV008094314 volume:210 year:2022 pages:0 https://doi.org/10.1016/j.petrol.2021.109972 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OPC-MAT 31.70 Wahrscheinlichkeitsrechnung VZ AR 210 2022 0 |
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10.1016/j.petrol.2021.109972 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001658.pica (DE-627)ELV056641583 (ELSEVIER)S0920-4105(21)01586-2 DE-627 ger DE-627 rakwb eng 510 VZ 31.70 bkl Xu, Min verfasserin aut Organic geochemical signatures of source rocks and oil-source correlation in the Papuan Basin, Papua New Guinea 2022transfer abstract nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier The Papuan Basin is the largest petroliferous basin in Papua New Guinea (PNG), where developed several sets of potential source rocks (SRs). The Jurassic SRs are clay-rich shales, whose organic matter (OM, mainly type Ⅱ2-Ⅲ) is predominantly derived from terrestrial higher plants deposited in a more oxic environment with relatively high maturity (0.35% 2, the mild dominance of C29 ααα 20 R sterane and the absence of oleanane ± lupane. Type C2 oils can be clearly distinguished from Type C3 by C19/(C19 + C23) tricyclic terpane <0.5, while the latter ones have higher abundances of oleanane ± lupine and diahopanes as well as C24 tetracyclic/C23 tricyclic terpane ratios. Type C2-3 oils are originated from calcareous SRs that deposited in Late Cretaceous or younger age. The Papuan Basin is the largest petroliferous basin in Papua New Guinea (PNG), where developed several sets of potential source rocks (SRs). The Jurassic SRs are clay-rich shales, whose organic matter (OM, mainly type Ⅱ2-Ⅲ) is predominantly derived from terrestrial higher plants deposited in a more oxic environment with relatively high maturity (0.35% 2, the mild dominance of C29 ααα 20 R sterane and the absence of oleanane ± lupane. Type C2 oils can be clearly distinguished from Type C3 by C19/(C19 + C23) tricyclic terpane <0.5, while the latter ones have higher abundances of oleanane ± lupine and diahopanes as well as C24 tetracyclic/C23 tricyclic terpane ratios. Type C2-3 oils are originated from calcareous SRs that deposited in Late Cretaceous or younger age. Source rocks Elsevier Oil-source rock correlation Elsevier Organic geochemistry Elsevier The papuan basin Elsevier Genetic oil families Elsevier Hou, Dujie oth Lin, Xiaoyun oth Liu, Jian oth Ding, Wenjing oth Xie, Rui oth Enthalten in Elsevier Science Baccelli, Francois ELSEVIER Iterated Gilbert mosaics 2019 Amsterdam [u.a.] (DE-627)ELV008094314 volume:210 year:2022 pages:0 https://doi.org/10.1016/j.petrol.2021.109972 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OPC-MAT 31.70 Wahrscheinlichkeitsrechnung VZ AR 210 2022 0 |
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author |
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Organic geochemical signatures of source rocks and oil-source correlation in the Papuan Basin, Papua New Guinea |
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Organic geochemical signatures of source rocks and oil-source correlation in the Papuan Basin, Papua New Guinea |
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organic geochemical signatures of source rocks and oil-source correlation in the papuan basin, papua new guinea |
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Organic geochemical signatures of source rocks and oil-source correlation in the Papuan Basin, Papua New Guinea |
abstract |
The Papuan Basin is the largest petroliferous basin in Papua New Guinea (PNG), where developed several sets of potential source rocks (SRs). The Jurassic SRs are clay-rich shales, whose organic matter (OM, mainly type Ⅱ2-Ⅲ) is predominantly derived from terrestrial higher plants deposited in a more oxic environment with relatively high maturity (0.35% 2, the mild dominance of C29 ααα 20 R sterane and the absence of oleanane ± lupane. Type C2 oils can be clearly distinguished from Type C3 by C19/(C19 + C23) tricyclic terpane <0.5, while the latter ones have higher abundances of oleanane ± lupine and diahopanes as well as C24 tetracyclic/C23 tricyclic terpane ratios. Type C2-3 oils are originated from calcareous SRs that deposited in Late Cretaceous or younger age. |
abstractGer |
The Papuan Basin is the largest petroliferous basin in Papua New Guinea (PNG), where developed several sets of potential source rocks (SRs). The Jurassic SRs are clay-rich shales, whose organic matter (OM, mainly type Ⅱ2-Ⅲ) is predominantly derived from terrestrial higher plants deposited in a more oxic environment with relatively high maturity (0.35% 2, the mild dominance of C29 ααα 20 R sterane and the absence of oleanane ± lupane. Type C2 oils can be clearly distinguished from Type C3 by C19/(C19 + C23) tricyclic terpane <0.5, while the latter ones have higher abundances of oleanane ± lupine and diahopanes as well as C24 tetracyclic/C23 tricyclic terpane ratios. Type C2-3 oils are originated from calcareous SRs that deposited in Late Cretaceous or younger age. |
abstract_unstemmed |
The Papuan Basin is the largest petroliferous basin in Papua New Guinea (PNG), where developed several sets of potential source rocks (SRs). The Jurassic SRs are clay-rich shales, whose organic matter (OM, mainly type Ⅱ2-Ⅲ) is predominantly derived from terrestrial higher plants deposited in a more oxic environment with relatively high maturity (0.35% 2, the mild dominance of C29 ααα 20 R sterane and the absence of oleanane ± lupane. Type C2 oils can be clearly distinguished from Type C3 by C19/(C19 + C23) tricyclic terpane <0.5, while the latter ones have higher abundances of oleanane ± lupine and diahopanes as well as C24 tetracyclic/C23 tricyclic terpane ratios. Type C2-3 oils are originated from calcareous SRs that deposited in Late Cretaceous or younger age. |
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title_short |
Organic geochemical signatures of source rocks and oil-source correlation in the Papuan Basin, Papua New Guinea |
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https://doi.org/10.1016/j.petrol.2021.109972 |
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Hou, Dujie Lin, Xiaoyun Liu, Jian Ding, Wenjing Xie, Rui |
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