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
Gespeichert in:
| Autor*in: |
Xu, Min [verfasserIn] |
|---|
| Format: |
E-Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2022transfer abstract |
|---|
| Schlagwörter: |
|---|
| Übergeordnetes Werk: |
Enthalten in: Iterated Gilbert mosaics - Baccelli, Francois ELSEVIER, 2019, Amsterdam [u.a.] |
|---|---|
| Übergeordnetes Werk: |
volume:210 ; year:2022 ; pages:0 |
| Links: |
|---|
| DOI / URN: |
10.1016/j.petrol.2021.109972 |
|---|
| Katalog-ID: |
ELV056641583 |
|---|
| LEADER | 01000caa a22002652 4500 | ||
|---|---|---|---|
| 001 | ELV056641583 | ||
| 003 | DE-627 | ||
| 005 | 20230626043713.0 | ||
| 007 | cr uuu---uuuuu | ||
| 008 | 220205s2022 xx |||||o 00| ||eng c | ||
| 024 | 7 | |a 10.1016/j.petrol.2021.109972 |2 doi | |
| 028 | 5 | 2 | |a /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001658.pica |
| 035 | |a (DE-627)ELV056641583 | ||
| 035 | |a (ELSEVIER)S0920-4105(21)01586-2 | ||
| 040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
| 041 | |a eng | ||
| 082 | 0 | 4 | |a 510 |q VZ |
| 084 | |a 31.70 |2 bkl | ||
| 100 | 1 | |a Xu, Min |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a Organic geochemical signatures of source rocks and oil-source correlation in the Papuan Basin, Papua New Guinea |
| 264 | 1 | |c 2022transfer abstract | |
| 336 | |a nicht spezifiziert |b zzz |2 rdacontent | ||
| 337 | |a nicht spezifiziert |b z |2 rdamedia | ||
| 338 | |a nicht spezifiziert |b zu |2 rdacarrier | ||
| 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. | ||
| 650 | 7 | |a Source rocks |2 Elsevier | |
| 650 | 7 | |a Oil-source rock correlation |2 Elsevier | |
| 650 | 7 | |a Organic geochemistry |2 Elsevier | |
| 650 | 7 | |a The papuan basin |2 Elsevier | |
| 650 | 7 | |a Genetic oil families |2 Elsevier | |
| 700 | 1 | |a Hou, Dujie |4 oth | |
| 700 | 1 | |a Lin, Xiaoyun |4 oth | |
| 700 | 1 | |a Liu, Jian |4 oth | |
| 700 | 1 | |a Ding, Wenjing |4 oth | |
| 700 | 1 | |a Xie, Rui |4 oth | |
| 773 | 0 | 8 | |i Enthalten in |n Elsevier Science |a Baccelli, Francois ELSEVIER |t Iterated Gilbert mosaics |d 2019 |g Amsterdam [u.a.] |w (DE-627)ELV008094314 |
| 773 | 1 | 8 | |g volume:210 |g year:2022 |g pages:0 |
| 856 | 4 | 0 | |u https://doi.org/10.1016/j.petrol.2021.109972 |3 Volltext |
| 912 | |a GBV_USEFLAG_U | ||
| 912 | |a GBV_ELV | ||
| 912 | |a SYSFLAG_U | ||
| 912 | |a SSG-OPC-MAT | ||
| 936 | b | k | |a 31.70 |j Wahrscheinlichkeitsrechnung |q VZ |
| 951 | |a AR | ||
| 952 | |d 210 |j 2022 |h 0 | ||
| author_variant |
m x mx |
|---|---|
| matchkey_str |
xuminhoudujielinxiaoyunliujiandingwenjin:2022----:raigohmclintrsforeokadisuccreainnh |
| hierarchy_sort_str |
2022transfer abstract |
| bklnumber |
31.70 |
| publishDate |
2022 |
| allfields |
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 |
| allfields_unstemmed |
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 |
| allfieldsGer |
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 |
| allfieldsSound |
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 |
| language |
English |
| source |
Enthalten in Iterated Gilbert mosaics Amsterdam [u.a.] volume:210 year:2022 pages:0 |
| sourceStr |
Enthalten in Iterated Gilbert mosaics Amsterdam [u.a.] volume:210 year:2022 pages:0 |
| format_phy_str_mv |
Article |
| bklname |
Wahrscheinlichkeitsrechnung |
| institution |
findex.gbv.de |
| topic_facet |
Source rocks Oil-source rock correlation Organic geochemistry The papuan basin Genetic oil families |
| dewey-raw |
510 |
| isfreeaccess_bool |
false |
| container_title |
Iterated Gilbert mosaics |
| authorswithroles_txt_mv |
Xu, Min @@aut@@ Hou, Dujie @@oth@@ Lin, Xiaoyun @@oth@@ Liu, Jian @@oth@@ Ding, Wenjing @@oth@@ Xie, Rui @@oth@@ |
| publishDateDaySort_date |
2022-01-01T00:00:00Z |
| hierarchy_top_id |
ELV008094314 |
| dewey-sort |
3510 |
| id |
ELV056641583 |
| language_de |
englisch |
| fullrecord |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">ELV056641583</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230626043713.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">220205s2022 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1016/j.petrol.2021.109972</subfield><subfield code="2">doi</subfield></datafield><datafield tag="028" ind1="5" ind2="2"><subfield code="a">/cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001658.pica</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)ELV056641583</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(ELSEVIER)S0920-4105(21)01586-2</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">510</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">31.70</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Xu, Min</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Organic geochemical signatures of source rocks and oil-source correlation in the Papuan Basin, Papua New Guinea</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2022transfer abstract</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zzz</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">z</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zu</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="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.</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="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.</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Source rocks</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Oil-source rock correlation</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Organic geochemistry</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">The papuan basin</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Genetic oil families</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Hou, Dujie</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Lin, Xiaoyun</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Liu, Jian</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Ding, Wenjing</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Xie, Rui</subfield><subfield code="4">oth</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="n">Elsevier Science</subfield><subfield code="a">Baccelli, Francois ELSEVIER</subfield><subfield code="t">Iterated Gilbert mosaics</subfield><subfield code="d">2019</subfield><subfield code="g">Amsterdam [u.a.]</subfield><subfield code="w">(DE-627)ELV008094314</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:210</subfield><subfield code="g">year:2022</subfield><subfield code="g">pages:0</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doi.org/10.1016/j.petrol.2021.109972</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ELV</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-MAT</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">31.70</subfield><subfield code="j">Wahrscheinlichkeitsrechnung</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">210</subfield><subfield code="j">2022</subfield><subfield code="h">0</subfield></datafield></record></collection>
|
| author |
Xu, Min |
| spellingShingle |
Xu, Min ddc 510 bkl 31.70 Elsevier Source rocks Elsevier Oil-source rock correlation Elsevier Organic geochemistry Elsevier The papuan basin Elsevier Genetic oil families Organic geochemical signatures of source rocks and oil-source correlation in the Papuan Basin, Papua New Guinea |
| authorStr |
Xu, Min |
| ppnlink_with_tag_str_mv |
@@773@@(DE-627)ELV008094314 |
| format |
electronic Article |
| dewey-ones |
510 - Mathematics |
| delete_txt_mv |
keep |
| author_role |
aut |
| collection |
elsevier |
| remote_str |
true |
| illustrated |
Not Illustrated |
| topic_title |
510 VZ 31.70 bkl Organic geochemical signatures of source rocks and oil-source correlation in the Papuan Basin, Papua New Guinea Source rocks Elsevier Oil-source rock correlation Elsevier Organic geochemistry Elsevier The papuan basin Elsevier Genetic oil families Elsevier |
| topic |
ddc 510 bkl 31.70 Elsevier Source rocks Elsevier Oil-source rock correlation Elsevier Organic geochemistry Elsevier The papuan basin Elsevier Genetic oil families |
| topic_unstemmed |
ddc 510 bkl 31.70 Elsevier Source rocks Elsevier Oil-source rock correlation Elsevier Organic geochemistry Elsevier The papuan basin Elsevier Genetic oil families |
| topic_browse |
ddc 510 bkl 31.70 Elsevier Source rocks Elsevier Oil-source rock correlation Elsevier Organic geochemistry Elsevier The papuan basin Elsevier Genetic oil families |
| format_facet |
Elektronische Aufsätze Aufsätze Elektronische Ressource |
| format_main_str_mv |
Text Zeitschrift/Artikel |
| carriertype_str_mv |
zu |
| author2_variant |
d h dh x l xl j l jl w d wd r x rx |
| hierarchy_parent_title |
Iterated Gilbert mosaics |
| hierarchy_parent_id |
ELV008094314 |
| dewey-tens |
510 - Mathematics |
| hierarchy_top_title |
Iterated Gilbert mosaics |
| isfreeaccess_txt |
false |
| familylinks_str_mv |
(DE-627)ELV008094314 |
| title |
Organic geochemical signatures of source rocks and oil-source correlation in the Papuan Basin, Papua New Guinea |
| ctrlnum |
(DE-627)ELV056641583 (ELSEVIER)S0920-4105(21)01586-2 |
| title_full |
Organic geochemical signatures of source rocks and oil-source correlation in the Papuan Basin, Papua New Guinea |
| author_sort |
Xu, Min |
| journal |
Iterated Gilbert mosaics |
| journalStr |
Iterated Gilbert mosaics |
| lang_code |
eng |
| isOA_bool |
false |
| dewey-hundreds |
500 - Science |
| recordtype |
marc |
| publishDateSort |
2022 |
| contenttype_str_mv |
zzz |
| container_start_page |
0 |
| author_browse |
Xu, Min |
| container_volume |
210 |
| class |
510 VZ 31.70 bkl |
| format_se |
Elektronische Aufsätze |
| author-letter |
Xu, Min |
| doi_str_mv |
10.1016/j.petrol.2021.109972 |
| dewey-full |
510 |
| title_sort |
organic geochemical signatures of source rocks and oil-source correlation in the papuan basin, papua new guinea |
| title_auth |
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. |
| collection_details |
GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OPC-MAT |
| title_short |
Organic geochemical signatures of source rocks and oil-source correlation in the Papuan Basin, Papua New Guinea |
| url |
https://doi.org/10.1016/j.petrol.2021.109972 |
| remote_bool |
true |
| author2 |
Hou, Dujie Lin, Xiaoyun Liu, Jian Ding, Wenjing Xie, Rui |
| author2Str |
Hou, Dujie Lin, Xiaoyun Liu, Jian Ding, Wenjing Xie, Rui |
| ppnlink |
ELV008094314 |
| mediatype_str_mv |
z |
| isOA_txt |
false |
| hochschulschrift_bool |
false |
| author2_role |
oth oth oth oth oth |
| doi_str |
10.1016/j.petrol.2021.109972 |
| up_date |
2024-07-06T20:59:08.266Z |
| _version_ |
1803864819123617792 |
| fullrecord_marcxml |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">ELV056641583</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230626043713.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">220205s2022 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1016/j.petrol.2021.109972</subfield><subfield code="2">doi</subfield></datafield><datafield tag="028" ind1="5" ind2="2"><subfield code="a">/cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001658.pica</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)ELV056641583</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(ELSEVIER)S0920-4105(21)01586-2</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">510</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">31.70</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Xu, Min</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Organic geochemical signatures of source rocks and oil-source correlation in the Papuan Basin, Papua New Guinea</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2022transfer abstract</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zzz</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">z</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zu</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="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.</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="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.</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Source rocks</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Oil-source rock correlation</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Organic geochemistry</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">The papuan basin</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Genetic oil families</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Hou, Dujie</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Lin, Xiaoyun</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Liu, Jian</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Ding, Wenjing</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Xie, Rui</subfield><subfield code="4">oth</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="n">Elsevier Science</subfield><subfield code="a">Baccelli, Francois ELSEVIER</subfield><subfield code="t">Iterated Gilbert mosaics</subfield><subfield code="d">2019</subfield><subfield code="g">Amsterdam [u.a.]</subfield><subfield code="w">(DE-627)ELV008094314</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:210</subfield><subfield code="g">year:2022</subfield><subfield code="g">pages:0</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doi.org/10.1016/j.petrol.2021.109972</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ELV</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-MAT</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">31.70</subfield><subfield code="j">Wahrscheinlichkeitsrechnung</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">210</subfield><subfield code="j">2022</subfield><subfield code="h">0</subfield></datafield></record></collection>
|
| score |
7.4015017 |