Quantification of free gas in the Kumano fore‐arc basin detected from borehole physical properties: IODP NanTroSEIZE drilling Site C0009
Identifieur interne : 006343 ( Main/Exploration ); précédent : 006342; suivant : 006344Quantification of free gas in the Kumano fore‐arc basin detected from borehole physical properties: IODP NanTroSEIZE drilling Site C0009
Auteurs : Mai-Linh Doan [France] ; Marianne Conin [France] ; Pierre Henry [France] ; Thomas Wiersberg [Allemagne] ; David Boutt [États-Unis] ; David Buchs [Australie] ; Demian Saffer [États-Unis] ; Lisa C. Mcneill [Royaume-Uni] ; Deniz Cukur [Corée du Sud] ; Weiren Lin [Japon]Source :
- Geochemistry, Geophysics, Geosystems [ 1525-2027 ] ; 2011-01.
Descripteurs français
- Wicri :
- topic : Géochimie, Géophysique.
English descriptors
- KwdEn :
- Basin, Borehole, Brie, Brie equation, Brie equations, Brie model, Brie theory, Bulk modulus, Cambridge univ, Cation, Cation exchange capacity, Chemical properties, Clay mineralogy, Clay minerals, Clay porosities, College station, Core data, Core matrix, Core samples, Cuttings samples, Density data, Effective porosity, Effective porosity data, Effective pressure, Fluid phase, Geochemistry, Geochemistry geophysics geosystems, Geophysics, Geosystems, Global inversion, Good agreement, Grain properties, Hydrate, Hydrated minerals, Iiia, Iiib, Intergranular pores, Inversion, Iodp, Iodp nantroseize drilling site, Iodp site, Kinoshita, Kumano, Kumano basin, Kumano basin figure, Lithodensity, Local inversion, Logging data, Matrix, Matrix parameters, Matrix properties, Mbsf, Modulus, Nankai, Nankai accretionary wedge, Nankai trough seismogenic zone experiment, Nantroseize, Nantroseize stage, Nearby site, Nearest receiver, Ocean drill, Oceanic drilling program, Organic carbon, Organic matter, Pore, Pore spaces, Porosity, Porous material, Porous media, Porous medium, Resistivity, Resistivity logs, Saffer, Saturation, Sediment, Seismic, Seismic surface, Silty mudstone, Solid grains, Sonic, Sonic data, Sonic properties, Sonic velocities, Sonic velocity, Total clay content, Total porosity, Unit iiia, Unit iiib, Units iiib, Water content, Water saturation, Wave data, Wave velocities, Wave velocity, Wave velocity measurements, Yellow diamonds.
- Teeft :
- Basin, Borehole, Brie, Brie equation, Brie equations, Brie model, Brie theory, Bulk modulus, Cambridge univ, Cation, Cation exchange capacity, Chemical properties, Clay mineralogy, Clay minerals, Clay porosities, College station, Core data, Core matrix, Core samples, Cuttings samples, Density data, Effective porosity, Effective porosity data, Effective pressure, Fluid phase, Geochemistry, Geochemistry geophysics geosystems, Geophysics, Geosystems, Global inversion, Good agreement, Grain properties, Hydrate, Hydrated minerals, Iiia, Iiib, Intergranular pores, Inversion, Iodp, Iodp nantroseize drilling site, Iodp site, Kinoshita, Kumano, Kumano basin, Kumano basin figure, Lithodensity, Local inversion, Logging data, Matrix, Matrix parameters, Matrix properties, Mbsf, Modulus, Nankai, Nankai accretionary wedge, Nankai trough seismogenic zone experiment, Nantroseize, Nantroseize stage, Nearby site, Nearest receiver, Ocean drill, Oceanic drilling program, Organic carbon, Organic matter, Pore, Pore spaces, Porosity, Porous material, Porous media, Porous medium, Resistivity, Resistivity logs, Saffer, Saturation, Sediment, Seismic, Seismic surface, Silty mudstone, Solid grains, Sonic, Sonic data, Sonic properties, Sonic velocities, Sonic velocity, Total clay content, Total porosity, Unit iiia, Unit iiib, Units iiib, Water content, Water saturation, Wave data, Wave velocities, Wave velocity, Wave velocity measurements, Yellow diamonds.
Abstract
The Kumano fore‐arc basin overlies the Nankai accretionary prism, formed by the subduction of the Philippine Sea Plate beneath the Eurasian plate offshore the Kii Peninsula, SW Honshu, Japan. Seismic surveys and boreholes within the framework of the Nankai Trough Seismogenic Zone Experiment (NanTroSEIZE) project show evidence of gas hydrates and free gas within the basin. Here we use high‐quality borehole sonic data from Integrated Oceanic Drilling Program (IODP) Site C0009 to quantify the free gas distribution in the landward part of the basin. The Brie theory is used to quantify gas content from sonic logs, which are calibrated from laboratory measurements on drill cores. First, we show that the sonic data are mainly sensitive to the fluid phase filling the intergranular pores (effective porosity), rather than to the total porosity that includes water bound to clay minerals. We then compare the effective porosity to lithodensity‐derived porosity that acts as a proxy for total porosity. The combination of these two data sets also allows assessment of clay mineralogy of the sediments. Second, we compute free gas saturation and find a gas‐rich interval that is restricted to a lithological unit characterized by a high abundance of wood fragments and lignite. This unit, at the base of the fore‐arc basin, is a hydrocarbon source that should be taken into account in models explaining gas distribution and the formation of the bottom‐simulating reflector within the Kumano fore‐arc basin.
Url:
DOI: 10.1029/2010GC003284
Affiliations:
- Allemagne, Australie, Corée du Sud, France, Japon, Royaume-Uni, États-Unis
- Auvergne-Rhône-Alpes, Brandebourg, Massachusetts, Pennsylvanie, Provence-Alpes-Côte d'Azur, Rhône-Alpes
- Aix en Provence, Amherst (Massachusetts), Grenoble, Potsdam, University Park (Pennsylvanie)
- Université Joseph Fourier, Université d'État de Pennsylvanie, Université du Massachusetts à Amherst
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Science,, MA, 01003, Amherst</wicri:regionArea><orgName type="university">Université du Massachusetts à Amherst</orgName><placeName><settlement type="city">Amherst (Massachusetts)</settlement><region type="state">Massachusetts</region></placeName></affiliation></author><author><name sortKey="Buchs, David" sort="Buchs, David" uniqKey="Buchs D" first="David" last="Buchs">David Buchs</name><affiliation wicri:level="1"><country xml:lang="fr">Australie</country><wicri:regionArea>Research School of Earth Sciences, The Australian National University, 61 Mills Road, Building J1,, 0200, Canberra, ACT</wicri:regionArea><wicri:noRegion>ACT</wicri:noRegion></affiliation></author><author><name sortKey="Saffer, Demian" sort="Saffer, Demian" uniqKey="Saffer D" first="Demian" last="Saffer">Demian Saffer</name><affiliation wicri:level="4"><country xml:lang="fr">États-Unis</country><wicri:regionArea>Geosciences, Pennsylvania State University, PA, 16802, 310 Deike Building, University 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Mcneill</name><affiliation wicri:level="1"><country xml:lang="fr">Royaume-Uni</country><wicri:regionArea>National Oceanography Centre, Southampton, University of Southampton, European Way,, SO14 3ZH, Southampton</wicri:regionArea><wicri:noRegion>Southampton</wicri:noRegion></affiliation></author><author><name sortKey="Cukur, Deniz" sort="Cukur, Deniz" uniqKey="Cukur D" first="Deniz" last="Cukur">Deniz Cukur</name><affiliation wicri:level="1"><country xml:lang="fr">Corée du Sud</country><wicri:regionArea>Department of Energy Resources Engineering, Pukyong National University, 599‐1, Daeyeon 3‐Dong, Nam‐Gu,, 608‐737, Busan</wicri:regionArea><wicri:noRegion>Busan</wicri:noRegion></affiliation></author><author><name sortKey="Lin, Weiren" sort="Lin, Weiren" uniqKey="Lin W" first="Weiren" last="Lin">Weiren Lin</name><affiliation wicri:level="1"><country xml:lang="fr">Japon</country><wicri:regionArea>Kochi Institute for Core Sample Research, JAMSTEC, Monobe‐otsu 200,, 783‐8502, Nankoku</wicri:regionArea><wicri:noRegion>Nankoku</wicri:noRegion></affiliation></author></analytic><monogr></monogr><series><title level="j" type="main">Geochemistry, Geophysics, Geosystems</title><title level="j" type="alt">GEOCHEMISTRY, GEOPHYSICS, GEOSYSTEMS</title><idno type="ISSN">1525-2027</idno><idno type="eISSN">1525-2027</idno><imprint><biblScope unit="vol">12</biblScope><biblScope unit="issue">1</biblScope><biblScope unit="page-count">12</biblScope><date type="published" when="2011-01">2011-01</date></imprint><idno type="ISSN">1525-2027</idno></series></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">1525-2027</idno></seriesStmt></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Basin</term><term>Borehole</term><term>Brie</term><term>Brie equation</term><term>Brie equations</term><term>Brie model</term><term>Brie theory</term><term>Bulk modulus</term><term>Cambridge univ</term><term>Cation</term><term>Cation exchange capacity</term><term>Chemical properties</term><term>Clay mineralogy</term><term>Clay minerals</term><term>Clay porosities</term><term>College station</term><term>Core data</term><term>Core matrix</term><term>Core samples</term><term>Cuttings samples</term><term>Density data</term><term>Effective porosity</term><term>Effective porosity data</term><term>Effective pressure</term><term>Fluid phase</term><term>Geochemistry</term><term>Geochemistry geophysics geosystems</term><term>Geophysics</term><term>Geosystems</term><term>Global inversion</term><term>Good agreement</term><term>Grain properties</term><term>Hydrate</term><term>Hydrated minerals</term><term>Iiia</term><term>Iiib</term><term>Intergranular pores</term><term>Inversion</term><term>Iodp</term><term>Iodp nantroseize drilling site</term><term>Iodp site</term><term>Kinoshita</term><term>Kumano</term><term>Kumano basin</term><term>Kumano basin figure</term><term>Lithodensity</term><term>Local inversion</term><term>Logging data</term><term>Matrix</term><term>Matrix parameters</term><term>Matrix properties</term><term>Mbsf</term><term>Modulus</term><term>Nankai</term><term>Nankai accretionary wedge</term><term>Nankai trough seismogenic zone experiment</term><term>Nantroseize</term><term>Nantroseize stage</term><term>Nearby site</term><term>Nearest receiver</term><term>Ocean drill</term><term>Oceanic drilling program</term><term>Organic carbon</term><term>Organic matter</term><term>Pore</term><term>Pore spaces</term><term>Porosity</term><term>Porous material</term><term>Porous media</term><term>Porous medium</term><term>Resistivity</term><term>Resistivity logs</term><term>Saffer</term><term>Saturation</term><term>Sediment</term><term>Seismic</term><term>Seismic surface</term><term>Silty mudstone</term><term>Solid grains</term><term>Sonic</term><term>Sonic data</term><term>Sonic properties</term><term>Sonic velocities</term><term>Sonic velocity</term><term>Total clay content</term><term>Total porosity</term><term>Unit iiia</term><term>Unit iiib</term><term>Units iiib</term><term>Water content</term><term>Water saturation</term><term>Wave data</term><term>Wave velocities</term><term>Wave velocity</term><term>Wave velocity measurements</term><term>Yellow diamonds</term></keywords><keywords scheme="Teeft" xml:lang="en"><term>Basin</term><term>Borehole</term><term>Brie</term><term>Brie equation</term><term>Brie equations</term><term>Brie model</term><term>Brie theory</term><term>Bulk modulus</term><term>Cambridge univ</term><term>Cation</term><term>Cation exchange capacity</term><term>Chemical properties</term><term>Clay mineralogy</term><term>Clay minerals</term><term>Clay porosities</term><term>College station</term><term>Core data</term><term>Core matrix</term><term>Core samples</term><term>Cuttings samples</term><term>Density data</term><term>Effective porosity</term><term>Effective porosity data</term><term>Effective pressure</term><term>Fluid phase</term><term>Geochemistry</term><term>Geochemistry geophysics geosystems</term><term>Geophysics</term><term>Geosystems</term><term>Global inversion</term><term>Good agreement</term><term>Grain properties</term><term>Hydrate</term><term>Hydrated minerals</term><term>Iiia</term><term>Iiib</term><term>Intergranular pores</term><term>Inversion</term><term>Iodp</term><term>Iodp nantroseize drilling site</term><term>Iodp site</term><term>Kinoshita</term><term>Kumano</term><term>Kumano basin</term><term>Kumano basin figure</term><term>Lithodensity</term><term>Local inversion</term><term>Logging data</term><term>Matrix</term><term>Matrix parameters</term><term>Matrix properties</term><term>Mbsf</term><term>Modulus</term><term>Nankai</term><term>Nankai accretionary wedge</term><term>Nankai trough seismogenic zone experiment</term><term>Nantroseize</term><term>Nantroseize stage</term><term>Nearby site</term><term>Nearest receiver</term><term>Ocean drill</term><term>Oceanic drilling program</term><term>Organic carbon</term><term>Organic matter</term><term>Pore</term><term>Pore spaces</term><term>Porosity</term><term>Porous material</term><term>Porous media</term><term>Porous medium</term><term>Resistivity</term><term>Resistivity logs</term><term>Saffer</term><term>Saturation</term><term>Sediment</term><term>Seismic</term><term>Seismic surface</term><term>Silty mudstone</term><term>Solid grains</term><term>Sonic</term><term>Sonic data</term><term>Sonic properties</term><term>Sonic velocities</term><term>Sonic velocity</term><term>Total clay content</term><term>Total porosity</term><term>Unit iiia</term><term>Unit iiib</term><term>Units iiib</term><term>Water content</term><term>Water saturation</term><term>Wave data</term><term>Wave velocities</term><term>Wave velocity</term><term>Wave velocity measurements</term><term>Yellow diamonds</term></keywords><keywords scheme="Wicri" type="topic" xml:lang="fr"><term>Géochimie</term><term>Géophysique</term></keywords></textClass></profileDesc></teiHeader><front><div type="abstract">The Kumano fore‐arc basin overlies the Nankai accretionary prism, formed by the subduction of the Philippine Sea Plate beneath the Eurasian plate offshore the Kii Peninsula, SW Honshu, Japan. Seismic surveys and boreholes within the framework of the Nankai Trough Seismogenic Zone Experiment (NanTroSEIZE) project show evidence of gas hydrates and free gas within the basin. Here we use high‐quality borehole sonic data from Integrated Oceanic Drilling Program (IODP) Site C0009 to quantify the free gas distribution in the landward part of the basin. The Brie theory is used to quantify gas content from sonic logs, which are calibrated from laboratory measurements on drill cores. First, we show that the sonic data are mainly sensitive to the fluid phase filling the intergranular pores (effective porosity), rather than to the total porosity that includes water bound to clay minerals. We then compare the effective porosity to lithodensity‐derived porosity that acts as a proxy for total porosity. The combination of these two data sets also allows assessment of clay mineralogy of the sediments. Second, we compute free gas saturation and find a gas‐rich interval that is restricted to a lithological unit characterized by a high abundance of wood fragments and lignite. This unit, at the base of the fore‐arc basin, is a hydrocarbon source that should be taken into account in models explaining gas distribution and the formation of the bottom‐simulating reflector within the Kumano fore‐arc basin.</div></front></TEI><affiliations><list><country><li>Allemagne</li><li>Australie</li><li>Corée du Sud</li><li>France</li><li>Japon</li><li>Royaume-Uni</li><li>États-Unis</li></country><region><li>Auvergne-Rhône-Alpes</li><li>Brandebourg</li><li>Massachusetts</li><li>Pennsylvanie</li><li>Provence-Alpes-Côte d'Azur</li><li>Rhône-Alpes</li></region><settlement><li>Aix en Provence</li><li>Amherst (Massachusetts)</li><li>Grenoble</li><li>Potsdam</li><li>University Park (Pennsylvanie)</li></settlement><orgName><li>Université Joseph Fourier</li><li>Université d'État de Pennsylvanie</li><li>Université du Massachusetts à Amherst</li></orgName></list><tree><country name="France"><noRegion><name sortKey="Doan, Mai Inh" sort="Doan, Mai Inh" uniqKey="Doan M" first="Mai-Linh" last="Doan">Mai-Linh Doan</name></noRegion><name sortKey="Conin, Marianne" sort="Conin, Marianne" uniqKey="Conin M" first="Marianne" last="Conin">Marianne Conin</name><name sortKey="Doan, Mai Inh" sort="Doan, Mai Inh" uniqKey="Doan M" first="Mai-Linh" last="Doan">Mai-Linh Doan</name><name sortKey="Doan, Mai Inh" sort="Doan, Mai Inh" uniqKey="Doan M" first="Mai-Linh" last="Doan">Mai-Linh Doan</name><name sortKey="Henry, Pierre" sort="Henry, Pierre" uniqKey="Henry P" first="Pierre" last="Henry">Pierre Henry</name></country><country name="Allemagne"><region name="Brandebourg"><name sortKey="Wiersberg, Thomas" sort="Wiersberg, Thomas" uniqKey="Wiersberg T" first="Thomas" last="Wiersberg">Thomas Wiersberg</name></region></country><country name="États-Unis"><region name="Massachusetts"><name sortKey="Boutt, David" sort="Boutt, David" uniqKey="Boutt D" first="David" last="Boutt">David Boutt</name></region><name sortKey="Saffer, Demian" sort="Saffer, Demian" uniqKey="Saffer D" first="Demian" last="Saffer">Demian Saffer</name></country><country name="Australie"><noRegion><name sortKey="Buchs, David" sort="Buchs, David" uniqKey="Buchs D" first="David" last="Buchs">David Buchs</name></noRegion></country><country name="Royaume-Uni"><noRegion><name sortKey="Mcneill, Lisa C" sort="Mcneill, Lisa C" uniqKey="Mcneill L" first="Lisa C." last="Mcneill">Lisa C. Mcneill</name></noRegion></country><country name="Corée du Sud"><noRegion><name sortKey="Cukur, Deniz" sort="Cukur, Deniz" uniqKey="Cukur D" first="Deniz" last="Cukur">Deniz Cukur</name></noRegion></country><country name="Japon"><noRegion><name sortKey="Lin, Weiren" sort="Lin, Weiren" uniqKey="Lin W" first="Weiren" last="Lin">Weiren Lin</name></noRegion></country></tree></affiliations></record>Pour manipuler ce document sous Unix (Dilib)
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