AustralieFrV1, PascalFrancis, Corpus, bibRecord, 000F62

Normal faults and gas migration in an active plate boundary, southern Taranaki Basin, offshore New Zealand

Identifieur interne : 000F62 ( PascalFrancis/Corpus ); précédent : 000F61; suivant : 000F63

Normal faults and gas migration in an active plate boundary, southern Taranaki Basin, offshore New Zealand

Auteurs : Bradley R. Ilg ; Samuel Hemmings-Sykes ; Andrew Nicol ; Jan Baur ; Miko Fohrmann ; Rob Funnell ; Mike Milner

Source :

AAPG bulletin [ 0149-1423 ] ; 2012.

RBID : Pascal:12-0388867

Descripteurs français

Pascal (Inist)
- Faille normale, Migration, Limite plaque, Off shore, Ecoulement, Sismique 3D, Distribution spatiale, Epaisseur, Oligocène, Mudstone, Modèle, Hydrocarbure, Crétacé, Roche mère, Perméabilité, Densité, Fracture ouverte, Gaz naturel, Sismique réflexion, Formation Otaraoa, Bassin Taranaki, Nouvelle Zélande.

English descriptors

KwdEn :
- Cretaceous, New Zealand, Oligocene, Taranaki Basin, density, flow, hydrocarbons, migration, models, mudstone, natural gas, normal faults, offshore, open fractures, permeability, plate boundaries, seismic reflection, source rocks, spatial distribution, thickness, three-dimensional seismics.

Abstract

The function of normal faults in upsequence flow of gas has been examined using two-dimensional and three-dimensional seismic-reflection data from the southern Taranaki Basin, New Zealand. The spatial distributions of late-stage normal faults, gas chimneys, thickness of the Oligocene mudstone-rich seal (Otaraoa Formation), and modeled hydrocarbon expulsion volumes are compared. Gas chimneys are most common above Cretaceous source rocks modeled to have expelled hydrocarbons. Most (∼70%) of the observed gas chimneys follow, and/ or are rooted in, late-stage normal faults. These faults are the primary seal bypass mechanism for hydrocarbons, where they displace the seal (or intersect faults that displace the seal) and the seal is thick (e.g., more tan ∼340 m [∼1115 ft]). Active vertical gas flow through the seal commenced after the onset of faulting (∼3.6 Ma), whereas subseal lateral flow started significantly earlier at approximately 15 Ma and resulted in an early charge of structural highs. Gas flow up along faults in low-permeability mudstones (<1 md) is channelized with steep chimneys commonly occurring close to fault tips and relay ramps. In these cases, gas flow may be focused by the presence of high densities of open fractures locally elevating upsequence bulk permeabilities to approximately 1 to 400 md.

Notice en format standard (ISO 2709)

Pour connaître la documentation sur le format Inist Standard.

A01	`01`	`1`		`@0 0149-1423`
A02	`01`			`@0 AABUD2`
A03		`1`		`@0 AAPG bull.`
A05				`@2 96`
A06				`@2 9`
A08	`01`	`1`	`ENG`	`@1 Normal faults and gas migration in an active plate boundary, southern Taranaki Basin, offshore New Zealand`
A11	`01`	`1`		`@1 ILG (Bradley R.)`
A11	`02`	`1`		`@1 HEMMINGS-SYKES (Samuel)`
A11	`03`	`1`		`@1 NICOL (Andrew)`
A11	`04`	`1`		`@1 BAUR (Jan)`
A11	`05`	`1`		`@1 FOHRMANN (Miko)`
A11	`06`	`1`		`@1 FUNNELL (Rob)`
A11	`07`	`1`		`@1 MILNER (Mike)`
A14	`01`			`@1 New Zealand Petroleum and Minerals, Ministry of Economic Development, P.O. Box 1473 @2 Wellington @3 NZL @Z 1 aut.`
A14	`02`			`@1 ExxonMobil, 12 Riverside Quay, Southbank Victoria 3006 @2 Melbourne @3 AUS @Z 2 aut.`
A14	`03`			`@1 GNS Science, P.O. Box 30368 @2 Lower Hutt @3 NZL @Z 3 aut.`
A14	`04`			`@1 Total Exploration and Production, Scientific and Technical Center Jean Feger, Avenue Larribau @2 Pau @3 FRA @Z 4 aut.`
A14	`05`			`@1 CNS Science, P.O. Box 30368 @2 Lower Hutt @3 NZL @Z 5 aut. @Z 6 aut.`
A14	`06`			`@1 OMV, 10 Brandon Street @2 Wellington @3 NZL @Z 7 aut.`
A20				`@1 1733-1756`
A21				`@1 2012`
A23	`01`			`@0 ENG`
A43	`01`			`@1 INIST @2 3085 @5 354000508378720070`
A44				`@0 0000 @1 © 2012 INIST-CNRS. All rights reserved.`
A45				`@0 3 p.3/4`
A47	`01`	`1`		`@0 12-0388867`
A60				`@1 P`
A61				`@0 A`
A64	`01`	`1`		`@0 AAPG bulletin`
A66	`01`			`@0 USA`
C01	`01`		`ENG`	@0 The function of normal faults in upsequence flow of gas has been examined using two-dimensional and three-dimensional seismic-reflection data from the southern Taranaki Basin, New Zealand. The spatial distributions of late-stage normal faults, gas chimneys, thickness of the Oligocene mudstone-rich seal (Otaraoa Formation), and modeled hydrocarbon expulsion volumes are compared. Gas chimneys are most common above Cretaceous source rocks modeled to have expelled hydrocarbons. Most (∼70%) of the observed gas chimneys follow, and/ or are rooted in, late-stage normal faults. These faults are the primary seal bypass mechanism for hydrocarbons, where they displace the seal (or intersect faults that displace the seal) and the seal is thick (e.g., more tan ∼340 m [∼1115 ft]). Active vertical gas flow through the seal commenced after the onset of faulting (∼3.6 Ma), whereas subseal lateral flow started significantly earlier at approximately 15 Ma and resulted in an early charge of structural highs. Gas flow up along faults in low-permeability mudstones (<1 md) is channelized with steep chimneys commonly occurring close to fault tips and relay ramps. In these cases, gas flow may be focused by the presence of high densities of open fractures locally elevating upsequence bulk permeabilities to approximately 1 to 400 md.
C02	`01`	`2`		`@0 001E01G03`
C02	`02`	`2`		`@0 001E01I`
C02	`03`	`2`		`@0 001E01M04`
C02	`04`	`2`		`@0 223A03`
C02	`05`	`2`		`@0 224A`
C02	`06`	`2`		`@0 225B04`
C03	`01`	`2`	`FRE`	`@0 Faille normale @5 01`
C03	`01`	`2`	`ENG`	`@0 normal faults @5 01`
C03	`01`	`2`	`SPA`	`@0 Falla normal @5 01`
C03	`02`	`2`	`FRE`	`@0 Migration @5 02`
C03	`02`	`2`	`ENG`	`@0 migration @5 02`
C03	`02`	`2`	`SPA`	`@0 Migración @5 02`
C03	`03`	`2`	`FRE`	`@0 Limite plaque @5 03`
C03	`03`	`2`	`ENG`	`@0 plate boundaries @5 03`
C03	`03`	`2`	`SPA`	`@0 Límite placa @5 03`
C03	`04`	`2`	`FRE`	`@0 Off shore @5 04`
C03	`04`	`2`	`ENG`	`@0 offshore @5 04`
C03	`04`	`2`	`SPA`	`@0 Off shore @5 04`
C03	`05`	`2`	`FRE`	`@0 Ecoulement @5 05`
C03	`05`	`2`	`ENG`	`@0 flow @5 05`
C03	`06`	`2`	`FRE`	`@0 Sismique 3D @5 06`
C03	`06`	`2`	`ENG`	`@0 three-dimensional seismics @5 06`
C03	`06`	`2`	`SPA`	`@0 Sísmica 3D @5 06`
C03	`07`	`2`	`FRE`	`@0 Distribution spatiale @5 07`
C03	`07`	`2`	`ENG`	`@0 spatial distribution @5 07`
C03	`07`	`2`	`SPA`	`@0 Distribución espacial @5 07`
C03	`08`	`2`	`FRE`	`@0 Epaisseur @5 09`
C03	`08`	`2`	`ENG`	`@0 thickness @5 09`
C03	`08`	`2`	`SPA`	`@0 Espesor @5 09`
C03	`09`	`2`	`FRE`	`@0 Oligocène @2 NX @5 10`
C03	`09`	`2`	`ENG`	`@0 Oligocene @2 NX @5 10`
C03	`09`	`2`	`SPA`	`@0 Oligoceno @2 NX @5 10`
C03	`10`	`2`	`FRE`	`@0 Mudstone @2 NV @5 11`
C03	`10`	`2`	`ENG`	`@0 mudstone @2 NV @5 11`
C03	`11`	`2`	`FRE`	`@0 Modèle @5 12`
C03	`11`	`2`	`ENG`	`@0 models @5 12`
C03	`11`	`2`	`SPA`	`@0 Modelo @5 12`
C03	`12`	`2`	`FRE`	`@0 Hydrocarbure @5 13`
C03	`12`	`2`	`ENG`	`@0 hydrocarbons @5 13`
C03	`12`	`2`	`SPA`	`@0 Hidrocarburo @5 13`
C03	`13`	`2`	`FRE`	`@0 Crétacé @2 NX @5 14`
C03	`13`	`2`	`ENG`	`@0 Cretaceous @2 NX @5 14`
C03	`13`	`2`	`SPA`	`@0 Cretáceo @2 NX @5 14`
C03	`14`	`2`	`FRE`	`@0 Roche mère @5 15`
C03	`14`	`2`	`ENG`	`@0 source rocks @5 15`
C03	`14`	`2`	`SPA`	`@0 Roca madre @5 15`
C03	`15`	`2`	`FRE`	`@0 Perméabilité @5 16`
C03	`15`	`2`	`ENG`	`@0 permeability @5 16`
C03	`15`	`2`	`SPA`	`@0 Permeabilidad @5 16`
C03	`16`	`2`	`FRE`	`@0 Densité @5 17`
C03	`16`	`2`	`ENG`	`@0 density @5 17`
C03	`16`	`2`	`SPA`	`@0 Densidad @5 17`
C03	`17`	`2`	`FRE`	`@0 Fracture ouverte @5 18`
C03	`17`	`2`	`ENG`	`@0 open fractures @5 18`
C03	`17`	`2`	`SPA`	`@0 Fractura abierta @5 18`
C03	`18`	`2`	`FRE`	`@0 Gaz naturel @5 19`
C03	`18`	`2`	`ENG`	`@0 natural gas @5 19`
C03	`18`	`2`	`SPA`	`@0 Gas natural @5 19`
C03	`19`	`2`	`FRE`	`@0 Sismique réflexion @5 20`
C03	`19`	`2`	`ENG`	`@0 seismic reflection @5 20`
C03	`19`	`2`	`SPA`	`@0 Método reflexión sísmica @5 20`
C03	`20`	`2`	`FRE`	`@0 Formation Otaraoa @4 INC @5 52`
C03	`21`	`2`	`FRE`	`@0 Bassin Taranaki @2 NG @5 61`
C03	`21`	`2`	`ENG`	`@0 Taranaki Basin @2 NG @5 61`
C03	`22`	`2`	`FRE`	`@0 Nouvelle Zélande @2 NG @5 62`
C03	`22`	`2`	`ENG`	`@0 New Zealand @2 NG @5 62`
C03	`22`	`2`	`SPA`	`@0 Nueva Zelandia @2 NG @5 62`
C07	`01`	`2`	`FRE`	`@0 Paléogène @2 NX`
C07	`01`	`2`	`ENG`	`@0 Paleogene @2 NX`
C07	`01`	`2`	`SPA`	`@0 Paleógeno @2 NX`
C07	`02`	`2`	`FRE`	`@0 Tertiaire @2 NX`
C07	`02`	`2`	`ENG`	`@0 Tertiary @2 NX`
C07	`02`	`2`	`SPA`	`@0 Terciario @2 NX`
C07	`03`	`2`	`FRE`	`@0 Cénozoïque @2 NX`
C07	`03`	`2`	`ENG`	`@0 Cenozoic @2 NX`
C07	`03`	`2`	`SPA`	`@0 Cenozoico @2 NX`
C07	`04`	`2`	`FRE`	`@0 Phanérozoïque @2 NX`
C07	`04`	`2`	`ENG`	`@0 Phanerozoic @2 NX`
C07	`04`	`2`	`SPA`	`@0 Fanerozoico @2 NX`
C07	`05`	`2`	`FRE`	`@0 Roche clastique @2 NV`
C07	`05`	`2`	`ENG`	`@0 clastic rocks @2 NV`
C07	`05`	`2`	`SPA`	`@0 Roca clástica @2 NV`
C07	`06`	`2`	`FRE`	`@0 Roche sédimentaire @2 NV`
C07	`06`	`2`	`ENG`	`@0 sedimentary rocks @2 NV`
C07	`06`	`2`	`SPA`	`@0 Roca sedimentaria @2 NV`
C07	`07`	`2`	`FRE`	`@0 Mésozoïque @2 NX`
C07	`07`	`2`	`ENG`	`@0 Mesozoic @2 NX`
C07	`08`	`2`	`FRE`	`@0 Océan Pacifique Ouest @2 NG`
C07	`08`	`2`	`ENG`	`@0 West Pacific @2 NG`
C07	`09`	`2`	`FRE`	`@0 Océan Pacifique @2 564`
C07	`09`	`2`	`ENG`	`@0 Pacific Ocean @2 564`
C07	`09`	`2`	`SPA`	`@0 Océano Pacífico @2 564`
C07	`10`	`2`	`FRE`	`@0 Australasie`
C07	`10`	`2`	`ENG`	`@0 Australasia`
C07	`10`	`2`	`SPA`	`@0 Australasia`
N21				`@1 303`

Format Inist (serveur)

NO :	PASCAL 12-0388867 INIST
ET :	Normal faults and gas migration in an active plate boundary, southern Taranaki Basin, offshore New Zealand
AU :	ILG (Bradley R.); HEMMINGS-SYKES (Samuel); NICOL (Andrew); BAUR (Jan); FOHRMANN (Miko); FUNNELL (Rob); MILNER (Mike)
AF :	New Zealand Petroleum and Minerals, Ministry of Economic Development, P.O. Box 1473/Wellington/Nouvelle-Zélande (1 aut.); ExxonMobil, 12 Riverside Quay, Southbank Victoria 3006/Melbourne/Australie (2 aut.); GNS Science, P.O. Box 30368/Lower Hutt/Nouvelle-Zélande (3 aut.); Total Exploration and Production, Scientific and Technical Center Jean Feger, Avenue Larribau/Pau/France (4 aut.); CNS Science, P.O. Box 30368/Lower Hutt/Nouvelle-Zélande (5 aut., 6 aut.); OMV, 10 Brandon Street/Wellington/Nouvelle-Zélande (7 aut.)
DT :	Publication en série; Niveau analytique
SO :	AAPG bulletin; ISSN 0149-1423; Coden AABUD2; Etats-Unis; Da. 2012; Vol. 96; No. 9; Pp. 1733-1756; Bibl. 3 p.3/4
LA :	Anglais
EA :	The function of normal faults in upsequence flow of gas has been examined using two-dimensional and three-dimensional seismic-reflection data from the southern Taranaki Basin, New Zealand. The spatial distributions of late-stage normal faults, gas chimneys, thickness of the Oligocene mudstone-rich seal (Otaraoa Formation), and modeled hydrocarbon expulsion volumes are compared. Gas chimneys are most common above Cretaceous source rocks modeled to have expelled hydrocarbons. Most (∼70%) of the observed gas chimneys follow, and/ or are rooted in, late-stage normal faults. These faults are the primary seal bypass mechanism for hydrocarbons, where they displace the seal (or intersect faults that displace the seal) and the seal is thick (e.g., more tan ∼340 m [∼1115 ft]). Active vertical gas flow through the seal commenced after the onset of faulting (∼3.6 Ma), whereas subseal lateral flow started significantly earlier at approximately 15 Ma and resulted in an early charge of structural highs. Gas flow up along faults in low-permeability mudstones (<1 md) is channelized with steep chimneys commonly occurring close to fault tips and relay ramps. In these cases, gas flow may be focused by the presence of high densities of open fractures locally elevating upsequence bulk permeabilities to approximately 1 to 400 md.
CC :	001E01G03; 001E01I; 001E01M04; 223A03; 224A; 225B04
FD :	Faille normale; Migration; Limite plaque; Off shore; Ecoulement; Sismique 3D; Distribution spatiale; Epaisseur; Oligocène; Mudstone; Modèle; Hydrocarbure; Crétacé; Roche mère; Perméabilité; Densité; Fracture ouverte; Gaz naturel; Sismique réflexion; Formation Otaraoa; Bassin Taranaki; Nouvelle Zélande
FG :	Paléogène; Tertiaire; Cénozoïque; Phanérozoïque; Roche clastique; Roche sédimentaire; Mésozoïque; Océan Pacifique Ouest; Océan Pacifique; Australasie
ED :	normal faults; migration; plate boundaries; offshore; flow; three-dimensional seismics; spatial distribution; thickness; Oligocene; mudstone; models; hydrocarbons; Cretaceous; source rocks; permeability; density; open fractures; natural gas; seismic reflection; Taranaki Basin; New Zealand
EG :	Paleogene; Tertiary; Cenozoic; Phanerozoic; clastic rocks; sedimentary rocks; Mesozoic; West Pacific; Pacific Ocean; Australasia
SD :	Falla normal; Migración; Límite placa; Off shore; Sísmica 3D; Distribución espacial; Espesor; Oligoceno; Modelo; Hidrocarburo; Cretáceo; Roca madre; Permeabilidad; Densidad; Fractura abierta; Gas natural; Método reflexión sísmica; Nueva Zelandia
LO :	INIST-3085.354000508378720070
ID :	12-0388867

Links to Exploration step

Pascal:12-0388867

Le document en format XML

<record><TEI><teiHeader><fileDesc><titleStmt><title xml:lang="en" level="a">Normal faults and gas migration in an active plate boundary, southern Taranaki Basin, offshore New Zealand</title>
<author><name sortKey="Ilg, Bradley R" sort="Ilg, Bradley R" uniqKey="Ilg B" first="Bradley R." last="Ilg">Bradley R. Ilg</name>
<affiliation><inist:fA14 i1="01"><s1>New Zealand Petroleum and Minerals, Ministry of Economic Development, P.O. Box 1473</s1>
<s2>Wellington</s2>
<s3>NZL</s3>
<sZ>1 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
<author><name sortKey="Hemmings Sykes, Samuel" sort="Hemmings Sykes, Samuel" uniqKey="Hemmings Sykes S" first="Samuel" last="Hemmings-Sykes">Samuel Hemmings-Sykes</name>
<affiliation><inist:fA14 i1="02"><s1>ExxonMobil, 12 Riverside Quay, Southbank Victoria 3006</s1>
<s2>Melbourne</s2>
<s3>AUS</s3>
<sZ>2 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
<author><name sortKey="Nicol, Andrew" sort="Nicol, Andrew" uniqKey="Nicol A" first="Andrew" last="Nicol">Andrew Nicol</name>
<affiliation><inist:fA14 i1="03"><s1>GNS Science, P.O. Box 30368</s1>
<s2>Lower Hutt</s2>
<s3>NZL</s3>
<sZ>3 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
<author><name sortKey="Baur, Jan" sort="Baur, Jan" uniqKey="Baur J" first="Jan" last="Baur">Jan Baur</name>
<affiliation><inist:fA14 i1="04"><s1>Total Exploration and Production, Scientific and Technical Center Jean Feger, Avenue Larribau</s1>
<s2>Pau</s2>
<s3>FRA</s3>
<sZ>4 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
<author><name sortKey="Fohrmann, Miko" sort="Fohrmann, Miko" uniqKey="Fohrmann M" first="Miko" last="Fohrmann">Miko Fohrmann</name>
<affiliation><inist:fA14 i1="05"><s1>CNS Science, P.O. Box 30368</s1>
<s2>Lower Hutt</s2>
<s3>NZL</s3>
<sZ>5 aut.</sZ>
<sZ>6 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
<author><name sortKey="Funnell, Rob" sort="Funnell, Rob" uniqKey="Funnell R" first="Rob" last="Funnell">Rob Funnell</name>
<affiliation><inist:fA14 i1="05"><s1>CNS Science, P.O. Box 30368</s1>
<s2>Lower Hutt</s2>
<s3>NZL</s3>
<sZ>5 aut.</sZ>
<sZ>6 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
<author><name sortKey="Milner, Mike" sort="Milner, Mike" uniqKey="Milner M" first="Mike" last="Milner">Mike Milner</name>
<affiliation><inist:fA14 i1="06"><s1>OMV, 10 Brandon Street</s1>
<s2>Wellington</s2>
<s3>NZL</s3>
<sZ>7 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
</titleStmt>
<publicationStmt><idno type="wicri:source">INIST</idno>
<idno type="inist">12-0388867</idno>
<date when="2012">2012</date>
<idno type="stanalyst">PASCAL 12-0388867 INIST</idno>
<idno type="RBID">Pascal:12-0388867</idno>
<idno type="wicri:Area/PascalFrancis/Corpus">000F62</idno>
</publicationStmt>
<sourceDesc><biblStruct><analytic><title xml:lang="en" level="a">Normal faults and gas migration in an active plate boundary, southern Taranaki Basin, offshore New Zealand</title>
<author><name sortKey="Ilg, Bradley R" sort="Ilg, Bradley R" uniqKey="Ilg B" first="Bradley R." last="Ilg">Bradley R. Ilg</name>
<affiliation><inist:fA14 i1="01"><s1>New Zealand Petroleum and Minerals, Ministry of Economic Development, P.O. Box 1473</s1>
<s2>Wellington</s2>
<s3>NZL</s3>
<sZ>1 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
<author><name sortKey="Hemmings Sykes, Samuel" sort="Hemmings Sykes, Samuel" uniqKey="Hemmings Sykes S" first="Samuel" last="Hemmings-Sykes">Samuel Hemmings-Sykes</name>
<affiliation><inist:fA14 i1="02"><s1>ExxonMobil, 12 Riverside Quay, Southbank Victoria 3006</s1>
<s2>Melbourne</s2>
<s3>AUS</s3>
<sZ>2 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
<author><name sortKey="Nicol, Andrew" sort="Nicol, Andrew" uniqKey="Nicol A" first="Andrew" last="Nicol">Andrew Nicol</name>
<affiliation><inist:fA14 i1="03"><s1>GNS Science, P.O. Box 30368</s1>
<s2>Lower Hutt</s2>
<s3>NZL</s3>
<sZ>3 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
<author><name sortKey="Baur, Jan" sort="Baur, Jan" uniqKey="Baur J" first="Jan" last="Baur">Jan Baur</name>
<affiliation><inist:fA14 i1="04"><s1>Total Exploration and Production, Scientific and Technical Center Jean Feger, Avenue Larribau</s1>
<s2>Pau</s2>
<s3>FRA</s3>
<sZ>4 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
<author><name sortKey="Fohrmann, Miko" sort="Fohrmann, Miko" uniqKey="Fohrmann M" first="Miko" last="Fohrmann">Miko Fohrmann</name>
<affiliation><inist:fA14 i1="05"><s1>CNS Science, P.O. Box 30368</s1>
<s2>Lower Hutt</s2>
<s3>NZL</s3>
<sZ>5 aut.</sZ>
<sZ>6 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
<author><name sortKey="Funnell, Rob" sort="Funnell, Rob" uniqKey="Funnell R" first="Rob" last="Funnell">Rob Funnell</name>
<affiliation><inist:fA14 i1="05"><s1>CNS Science, P.O. Box 30368</s1>
<s2>Lower Hutt</s2>
<s3>NZL</s3>
<sZ>5 aut.</sZ>
<sZ>6 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
<author><name sortKey="Milner, Mike" sort="Milner, Mike" uniqKey="Milner M" first="Mike" last="Milner">Mike Milner</name>
<affiliation><inist:fA14 i1="06"><s1>OMV, 10 Brandon Street</s1>
<s2>Wellington</s2>
<s3>NZL</s3>
<sZ>7 aut.</sZ>
</inist:fA14>
</affiliation>
</author>
</analytic>
<series><title level="j" type="main">AAPG bulletin</title>
<title level="j" type="abbreviated">AAPG bull.</title>
<idno type="ISSN">0149-1423</idno>
<imprint><date when="2012">2012</date>
</imprint>
</series>
</biblStruct>
</sourceDesc>
<seriesStmt><title level="j" type="main">AAPG bulletin</title>
<title level="j" type="abbreviated">AAPG bull.</title>
<idno type="ISSN">0149-1423</idno>
</seriesStmt>
</fileDesc>
<profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Cretaceous</term>
<term>New Zealand</term>
<term>Oligocene</term>
<term>Taranaki Basin</term>
<term>density</term>
<term>flow</term>
<term>hydrocarbons</term>
<term>migration</term>
<term>models</term>
<term>mudstone</term>
<term>natural gas</term>
<term>normal faults</term>
<term>offshore</term>
<term>open fractures</term>
<term>permeability</term>
<term>plate boundaries</term>
<term>seismic reflection</term>
<term>source rocks</term>
<term>spatial distribution</term>
<term>thickness</term>
<term>three-dimensional seismics</term>
</keywords>
<keywords scheme="Pascal" xml:lang="fr"><term>Faille normale</term>
<term>Migration</term>
<term>Limite plaque</term>
<term>Off shore</term>
<term>Ecoulement</term>
<term>Sismique 3D</term>
<term>Distribution spatiale</term>
<term>Epaisseur</term>
<term>Oligocène</term>
<term>Mudstone</term>
<term>Modèle</term>
<term>Hydrocarbure</term>
<term>Crétacé</term>
<term>Roche mère</term>
<term>Perméabilité</term>
<term>Densité</term>
<term>Fracture ouverte</term>
<term>Gaz naturel</term>
<term>Sismique réflexion</term>
<term>Formation Otaraoa</term>
<term>Bassin Taranaki</term>
<term>Nouvelle Zélande</term>
</keywords>
</textClass>
</profileDesc>
</teiHeader>
<front><div type="abstract" xml:lang="en">The function of normal faults in upsequence flow of gas has been examined using two-dimensional and three-dimensional seismic-reflection data from the southern Taranaki Basin, New Zealand. The spatial distributions of late-stage normal faults, gas chimneys, thickness of the Oligocene mudstone-rich seal (Otaraoa Formation), and modeled hydrocarbon expulsion volumes are compared. Gas chimneys are most common above Cretaceous source rocks modeled to have expelled hydrocarbons. Most (∼70%) of the observed gas chimneys follow, and/ or are rooted in, late-stage normal faults. These faults are the primary seal bypass mechanism for hydrocarbons, where they displace the seal (or intersect faults that displace the seal) and the seal is thick (e.g., more tan ∼340 m [∼1115 ft]). Active vertical gas flow through the seal commenced after the onset of faulting (∼3.6 Ma), whereas subseal lateral flow started significantly earlier at approximately 15 Ma and resulted in an early charge of structural highs. Gas flow up along faults in low-permeability mudstones (<1 md) is channelized with steep chimneys commonly occurring close to fault tips and relay ramps. In these cases, gas flow may be focused by the presence of high densities of open fractures locally elevating upsequence bulk permeabilities to approximately 1 to 400 md.</div>
</front>
</TEI>
<inist><standard h6="B"><pA><fA01 i1="01" i2="1"><s0>0149-1423</s0>
</fA01>
<fA02 i1="01"><s0>AABUD2</s0>
</fA02>
<fA03 i2="1"><s0>AAPG bull.</s0>
</fA03>
<fA05><s2>96</s2>
</fA05>
<fA06><s2>9</s2>
</fA06>
<fA08 i1="01" i2="1" l="ENG"><s1>Normal faults and gas migration in an active plate boundary, southern Taranaki Basin, offshore New Zealand</s1>
</fA08>
<fA11 i1="01" i2="1"><s1>ILG (Bradley R.)</s1>
</fA11>
<fA11 i1="02" i2="1"><s1>HEMMINGS-SYKES (Samuel)</s1>
</fA11>
<fA11 i1="03" i2="1"><s1>NICOL (Andrew)</s1>
</fA11>
<fA11 i1="04" i2="1"><s1>BAUR (Jan)</s1>
</fA11>
<fA11 i1="05" i2="1"><s1>FOHRMANN (Miko)</s1>
</fA11>
<fA11 i1="06" i2="1"><s1>FUNNELL (Rob)</s1>
</fA11>
<fA11 i1="07" i2="1"><s1>MILNER (Mike)</s1>
</fA11>
<fA14 i1="01"><s1>New Zealand Petroleum and Minerals, Ministry of Economic Development, P.O. Box 1473</s1>
<s2>Wellington</s2>
<s3>NZL</s3>
<sZ>1 aut.</sZ>
</fA14>
<fA14 i1="02"><s1>ExxonMobil, 12 Riverside Quay, Southbank Victoria 3006</s1>
<s2>Melbourne</s2>
<s3>AUS</s3>
<sZ>2 aut.</sZ>
</fA14>
<fA14 i1="03"><s1>GNS Science, P.O. Box 30368</s1>
<s2>Lower Hutt</s2>
<s3>NZL</s3>
<sZ>3 aut.</sZ>
</fA14>
<fA14 i1="04"><s1>Total Exploration and Production, Scientific and Technical Center Jean Feger, Avenue Larribau</s1>
<s2>Pau</s2>
<s3>FRA</s3>
<sZ>4 aut.</sZ>
</fA14>
<fA14 i1="05"><s1>CNS Science, P.O. Box 30368</s1>
<s2>Lower Hutt</s2>
<s3>NZL</s3>
<sZ>5 aut.</sZ>
<sZ>6 aut.</sZ>
</fA14>
<fA14 i1="06"><s1>OMV, 10 Brandon Street</s1>
<s2>Wellington</s2>
<s3>NZL</s3>
<sZ>7 aut.</sZ>
</fA14>
<fA20><s1>1733-1756</s1>
</fA20>
<fA21><s1>2012</s1>
</fA21>
<fA23 i1="01"><s0>ENG</s0>
</fA23>
<fA43 i1="01"><s1>INIST</s1>
<s2>3085</s2>
<s5>354000508378720070</s5>
</fA43>
<fA44><s0>0000</s0>
<s1>© 2012 INIST-CNRS. All rights reserved.</s1>
</fA44>
<fA45><s0>3 p.3/4</s0>
</fA45>
<fA47 i1="01" i2="1"><s0>12-0388867</s0>
</fA47>
<fA60><s1>P</s1>
</fA60>
<fA61><s0>A</s0>
</fA61>
<fA64 i1="01" i2="1"><s0>AAPG bulletin</s0>
</fA64>
<fA66 i1="01"><s0>USA</s0>
</fA66>
<fC01 i1="01" l="ENG"><s0>The function of normal faults in upsequence flow of gas has been examined using two-dimensional and three-dimensional seismic-reflection data from the southern Taranaki Basin, New Zealand. The spatial distributions of late-stage normal faults, gas chimneys, thickness of the Oligocene mudstone-rich seal (Otaraoa Formation), and modeled hydrocarbon expulsion volumes are compared. Gas chimneys are most common above Cretaceous source rocks modeled to have expelled hydrocarbons. Most (∼70%) of the observed gas chimneys follow, and/ or are rooted in, late-stage normal faults. These faults are the primary seal bypass mechanism for hydrocarbons, where they displace the seal (or intersect faults that displace the seal) and the seal is thick (e.g., more tan ∼340 m [∼1115 ft]). Active vertical gas flow through the seal commenced after the onset of faulting (∼3.6 Ma), whereas subseal lateral flow started significantly earlier at approximately 15 Ma and resulted in an early charge of structural highs. Gas flow up along faults in low-permeability mudstones (<1 md) is channelized with steep chimneys commonly occurring close to fault tips and relay ramps. In these cases, gas flow may be focused by the presence of high densities of open fractures locally elevating upsequence bulk permeabilities to approximately 1 to 400 md.</s0>
</fC01>
<fC02 i1="01" i2="2"><s0>001E01G03</s0>
</fC02>
<fC02 i1="02" i2="2"><s0>001E01I</s0>
</fC02>
<fC02 i1="03" i2="2"><s0>001E01M04</s0>
</fC02>
<fC02 i1="04" i2="2"><s0>223A03</s0>
</fC02>
<fC02 i1="05" i2="2"><s0>224A</s0>
</fC02>
<fC02 i1="06" i2="2"><s0>225B04</s0>
</fC02>
<fC03 i1="01" i2="2" l="FRE"><s0>Faille normale</s0>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="2" l="ENG"><s0>normal faults</s0>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="2" l="SPA"><s0>Falla normal</s0>
<s5>01</s5>
</fC03>
<fC03 i1="02" i2="2" l="FRE"><s0>Migration</s0>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="2" l="ENG"><s0>migration</s0>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="2" l="SPA"><s0>Migración</s0>
<s5>02</s5>
</fC03>
<fC03 i1="03" i2="2" l="FRE"><s0>Limite plaque</s0>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="2" l="ENG"><s0>plate boundaries</s0>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="2" l="SPA"><s0>Límite placa</s0>
<s5>03</s5>
</fC03>
<fC03 i1="04" i2="2" l="FRE"><s0>Off shore</s0>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="2" l="ENG"><s0>offshore</s0>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="2" l="SPA"><s0>Off shore</s0>
<s5>04</s5>
</fC03>
<fC03 i1="05" i2="2" l="FRE"><s0>Ecoulement</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="2" l="ENG"><s0>flow</s0>
<s5>05</s5>
</fC03>
<fC03 i1="06" i2="2" l="FRE"><s0>Sismique 3D</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="2" l="ENG"><s0>three-dimensional seismics</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="2" l="SPA"><s0>Sísmica 3D</s0>
<s5>06</s5>
</fC03>
<fC03 i1="07" i2="2" l="FRE"><s0>Distribution spatiale</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="2" l="ENG"><s0>spatial distribution</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="2" l="SPA"><s0>Distribución espacial</s0>
<s5>07</s5>
</fC03>
<fC03 i1="08" i2="2" l="FRE"><s0>Epaisseur</s0>
<s5>09</s5>
</fC03>
<fC03 i1="08" i2="2" l="ENG"><s0>thickness</s0>
<s5>09</s5>
</fC03>
<fC03 i1="08" i2="2" l="SPA"><s0>Espesor</s0>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="2" l="FRE"><s0>Oligocène</s0>
<s2>NX</s2>
<s5>10</s5>
</fC03>
<fC03 i1="09" i2="2" l="ENG"><s0>Oligocene</s0>
<s2>NX</s2>
<s5>10</s5>
</fC03>
<fC03 i1="09" i2="2" l="SPA"><s0>Oligoceno</s0>
<s2>NX</s2>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="2" l="FRE"><s0>Mudstone</s0>
<s2>NV</s2>
<s5>11</s5>
</fC03>
<fC03 i1="10" i2="2" l="ENG"><s0>mudstone</s0>
<s2>NV</s2>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="2" l="FRE"><s0>Modèle</s0>
<s5>12</s5>
</fC03>
<fC03 i1="11" i2="2" l="ENG"><s0>models</s0>
<s5>12</s5>
</fC03>
<fC03 i1="11" i2="2" l="SPA"><s0>Modelo</s0>
<s5>12</s5>
</fC03>
<fC03 i1="12" i2="2" l="FRE"><s0>Hydrocarbure</s0>
<s5>13</s5>
</fC03>
<fC03 i1="12" i2="2" l="ENG"><s0>hydrocarbons</s0>
<s5>13</s5>
</fC03>
<fC03 i1="12" i2="2" l="SPA"><s0>Hidrocarburo</s0>
<s5>13</s5>
</fC03>
<fC03 i1="13" i2="2" l="FRE"><s0>Crétacé</s0>
<s2>NX</s2>
<s5>14</s5>
</fC03>
<fC03 i1="13" i2="2" l="ENG"><s0>Cretaceous</s0>
<s2>NX</s2>
<s5>14</s5>
</fC03>
<fC03 i1="13" i2="2" l="SPA"><s0>Cretáceo</s0>
<s2>NX</s2>
<s5>14</s5>
</fC03>
<fC03 i1="14" i2="2" l="FRE"><s0>Roche mère</s0>
<s5>15</s5>
</fC03>
<fC03 i1="14" i2="2" l="ENG"><s0>source rocks</s0>
<s5>15</s5>
</fC03>
<fC03 i1="14" i2="2" l="SPA"><s0>Roca madre</s0>
<s5>15</s5>
</fC03>
<fC03 i1="15" i2="2" l="FRE"><s0>Perméabilité</s0>
<s5>16</s5>
</fC03>
<fC03 i1="15" i2="2" l="ENG"><s0>permeability</s0>
<s5>16</s5>
</fC03>
<fC03 i1="15" i2="2" l="SPA"><s0>Permeabilidad</s0>
<s5>16</s5>
</fC03>
<fC03 i1="16" i2="2" l="FRE"><s0>Densité</s0>
<s5>17</s5>
</fC03>
<fC03 i1="16" i2="2" l="ENG"><s0>density</s0>
<s5>17</s5>
</fC03>
<fC03 i1="16" i2="2" l="SPA"><s0>Densidad</s0>
<s5>17</s5>
</fC03>
<fC03 i1="17" i2="2" l="FRE"><s0>Fracture ouverte</s0>
<s5>18</s5>
</fC03>
<fC03 i1="17" i2="2" l="ENG"><s0>open fractures</s0>
<s5>18</s5>
</fC03>
<fC03 i1="17" i2="2" l="SPA"><s0>Fractura abierta</s0>
<s5>18</s5>
</fC03>
<fC03 i1="18" i2="2" l="FRE"><s0>Gaz naturel</s0>
<s5>19</s5>
</fC03>
<fC03 i1="18" i2="2" l="ENG"><s0>natural gas</s0>
<s5>19</s5>
</fC03>
<fC03 i1="18" i2="2" l="SPA"><s0>Gas natural</s0>
<s5>19</s5>
</fC03>
<fC03 i1="19" i2="2" l="FRE"><s0>Sismique réflexion</s0>
<s5>20</s5>
</fC03>
<fC03 i1="19" i2="2" l="ENG"><s0>seismic reflection</s0>
<s5>20</s5>
</fC03>
<fC03 i1="19" i2="2" l="SPA"><s0>Método reflexión sísmica</s0>
<s5>20</s5>
</fC03>
<fC03 i1="20" i2="2" l="FRE"><s0>Formation Otaraoa</s0>
<s4>INC</s4>
<s5>52</s5>
</fC03>
<fC03 i1="21" i2="2" l="FRE"><s0>Bassin Taranaki</s0>
<s2>NG</s2>
<s5>61</s5>
</fC03>
<fC03 i1="21" i2="2" l="ENG"><s0>Taranaki Basin</s0>
<s2>NG</s2>
<s5>61</s5>
</fC03>
<fC03 i1="22" i2="2" l="FRE"><s0>Nouvelle Zélande</s0>
<s2>NG</s2>
<s5>62</s5>
</fC03>
<fC03 i1="22" i2="2" l="ENG"><s0>New Zealand</s0>
<s2>NG</s2>
<s5>62</s5>
</fC03>
<fC03 i1="22" i2="2" l="SPA"><s0>Nueva Zelandia</s0>
<s2>NG</s2>
<s5>62</s5>
</fC03>
<fC07 i1="01" i2="2" l="FRE"><s0>Paléogène</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="01" i2="2" l="ENG"><s0>Paleogene</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="01" i2="2" l="SPA"><s0>Paleógeno</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="02" i2="2" l="FRE"><s0>Tertiaire</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="02" i2="2" l="ENG"><s0>Tertiary</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="02" i2="2" l="SPA"><s0>Terciario</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="03" i2="2" l="FRE"><s0>Cénozoïque</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="03" i2="2" l="ENG"><s0>Cenozoic</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="03" i2="2" l="SPA"><s0>Cenozoico</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="04" i2="2" l="FRE"><s0>Phanérozoïque</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="04" i2="2" l="ENG"><s0>Phanerozoic</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="04" i2="2" l="SPA"><s0>Fanerozoico</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="05" i2="2" l="FRE"><s0>Roche clastique</s0>
<s2>NV</s2>
</fC07>
<fC07 i1="05" i2="2" l="ENG"><s0>clastic rocks</s0>
<s2>NV</s2>
</fC07>
<fC07 i1="05" i2="2" l="SPA"><s0>Roca clástica</s0>
<s2>NV</s2>
</fC07>
<fC07 i1="06" i2="2" l="FRE"><s0>Roche sédimentaire</s0>
<s2>NV</s2>
</fC07>
<fC07 i1="06" i2="2" l="ENG"><s0>sedimentary rocks</s0>
<s2>NV</s2>
</fC07>
<fC07 i1="06" i2="2" l="SPA"><s0>Roca sedimentaria</s0>
<s2>NV</s2>
</fC07>
<fC07 i1="07" i2="2" l="FRE"><s0>Mésozoïque</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="07" i2="2" l="ENG"><s0>Mesozoic</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="08" i2="2" l="FRE"><s0>Océan Pacifique Ouest</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="08" i2="2" l="ENG"><s0>West Pacific</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="09" i2="2" l="FRE"><s0>Océan Pacifique</s0>
<s2>564</s2>
</fC07>
<fC07 i1="09" i2="2" l="ENG"><s0>Pacific Ocean</s0>
<s2>564</s2>
</fC07>
<fC07 i1="09" i2="2" l="SPA"><s0>Océano Pacífico</s0>
<s2>564</s2>
</fC07>
<fC07 i1="10" i2="2" l="FRE"><s0>Australasie</s0>
</fC07>
<fC07 i1="10" i2="2" l="ENG"><s0>Australasia</s0>
</fC07>
<fC07 i1="10" i2="2" l="SPA"><s0>Australasia</s0>
</fC07>
<fN21><s1>303</s1>
</fN21>
</pA>
</standard>
<server><NO>PASCAL 12-0388867 INIST</NO>
<ET>Normal faults and gas migration in an active plate boundary, southern Taranaki Basin, offshore New Zealand</ET>
<AU>ILG (Bradley R.); HEMMINGS-SYKES (Samuel); NICOL (Andrew); BAUR (Jan); FOHRMANN (Miko); FUNNELL (Rob); MILNER (Mike)</AU>
<AF>New Zealand Petroleum and Minerals, Ministry of Economic Development, P.O. Box 1473/Wellington/Nouvelle-Zélande (1 aut.); ExxonMobil, 12 Riverside Quay, Southbank Victoria 3006/Melbourne/Australie (2 aut.); GNS Science, P.O. Box 30368/Lower Hutt/Nouvelle-Zélande (3 aut.); Total Exploration and Production, Scientific and Technical Center Jean Feger, Avenue Larribau/Pau/France (4 aut.); CNS Science, P.O. Box 30368/Lower Hutt/Nouvelle-Zélande (5 aut., 6 aut.); OMV, 10 Brandon Street/Wellington/Nouvelle-Zélande (7 aut.)</AF>
<DT>Publication en série; Niveau analytique</DT>
<SO>AAPG bulletin; ISSN 0149-1423; Coden AABUD2; Etats-Unis; Da. 2012; Vol. 96; No. 9; Pp. 1733-1756; Bibl. 3 p.3/4</SO>
<LA>Anglais</LA>
<EA>The function of normal faults in upsequence flow of gas has been examined using two-dimensional and three-dimensional seismic-reflection data from the southern Taranaki Basin, New Zealand. The spatial distributions of late-stage normal faults, gas chimneys, thickness of the Oligocene mudstone-rich seal (Otaraoa Formation), and modeled hydrocarbon expulsion volumes are compared. Gas chimneys are most common above Cretaceous source rocks modeled to have expelled hydrocarbons. Most (∼70%) of the observed gas chimneys follow, and/ or are rooted in, late-stage normal faults. These faults are the primary seal bypass mechanism for hydrocarbons, where they displace the seal (or intersect faults that displace the seal) and the seal is thick (e.g., more tan ∼340 m [∼1115 ft]). Active vertical gas flow through the seal commenced after the onset of faulting (∼3.6 Ma), whereas subseal lateral flow started significantly earlier at approximately 15 Ma and resulted in an early charge of structural highs. Gas flow up along faults in low-permeability mudstones (<1 md) is channelized with steep chimneys commonly occurring close to fault tips and relay ramps. In these cases, gas flow may be focused by the presence of high densities of open fractures locally elevating upsequence bulk permeabilities to approximately 1 to 400 md.</EA>
<CC>001E01G03; 001E01I; 001E01M04; 223A03; 224A; 225B04</CC>
<FD>Faille normale; Migration; Limite plaque; Off shore; Ecoulement; Sismique 3D; Distribution spatiale; Epaisseur; Oligocène; Mudstone; Modèle; Hydrocarbure; Crétacé; Roche mère; Perméabilité; Densité; Fracture ouverte; Gaz naturel; Sismique réflexion; Formation Otaraoa; Bassin Taranaki; Nouvelle Zélande</FD>
<FG>Paléogène; Tertiaire; Cénozoïque; Phanérozoïque; Roche clastique; Roche sédimentaire; Mésozoïque; Océan Pacifique Ouest; Océan Pacifique; Australasie</FG>
<ED>normal faults; migration; plate boundaries; offshore; flow; three-dimensional seismics; spatial distribution; thickness; Oligocene; mudstone; models; hydrocarbons; Cretaceous; source rocks; permeability; density; open fractures; natural gas; seismic reflection; Taranaki Basin; New Zealand</ED>
<EG>Paleogene; Tertiary; Cenozoic; Phanerozoic; clastic rocks; sedimentary rocks; Mesozoic; West Pacific; Pacific Ocean; Australasia</EG>
<SD>Falla normal; Migración; Límite placa; Off shore; Sísmica 3D; Distribución espacial; Espesor; Oligoceno; Modelo; Hidrocarburo; Cretáceo; Roca madre; Permeabilidad; Densidad; Fractura abierta; Gas natural; Método reflexión sísmica; Nueva Zelandia</SD>
<LO>INIST-3085.354000508378720070</LO>
<ID>12-0388867</ID>
</server>
</inist>
</record>

Pour manipuler ce document sous Unix (Dilib)

EXPLOR_STEP=$WICRI_ROOT/Wicri/Asie/explor/AustralieFrV1/Data/PascalFrancis/Corpus

HfdSelect -h $EXPLOR_STEP/biblio.hfd -nk 000F62 | SxmlIndent | more

HfdSelect -h $EXPLOR_AREA/Data/PascalFrancis/Corpus/biblio.hfd -nk 000F62 | SxmlIndent | more

Pour mettre un lien sur cette page dans le réseau Wicri

{{Explor lien
   |wiki=    Wicri/Asie
   |area=    AustralieFrV1
   |flux=    PascalFrancis
   |étape=   Corpus
   |type=    RBID
   |clé=     Pascal:12-0388867
   |texte=   Normal faults and gas migration in an active plate boundary, southern Taranaki Basin, offshore New Zealand
}}

This area was generated with Dilib version V0.6.33.
Data generation: Tue Dec 5 10:43:12 2017. Site generation: Tue Mar 5 14:07:20 2024

	Serveur d'exploration sur les relations entre la France et l'Australie
	Attention, ce site est en cours de développement ! Attention, site généré par des moyens informatiques à partir de corpus bruts. Les informations ne sont donc pas validées.

Serveur d'exploration sur les relations entre la France et l'Australie

Normal faults and gas migration in an active plate boundary, southern Taranaki Basin, offshore New Zealand

Normal faults and gas migration in an active plate boundary, southern Taranaki Basin, offshore New Zealand

Source :

Descripteurs français

English descriptors

Abstract

Notice en format standard (ISO 2709)

Format Inist (serveur)

Links to Exploration step

Le document en format XML

Pour manipuler ce document sous Unix (Dilib)

Pour mettre un lien sur cette page dans le réseau Wicri