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Of reservoir characterization studies in the Fullerton Clear Fork reservoir / Stephen C. Ruppel -- Facies and sequence stratigraphy : critical tools for reservoir framework definition, Fullerton Clear Fork reservoir, Texas / Stephen C. Ruppel and Rebecca R. Harrington -- Integration of rock fabrics and stratigraphy for petrophysical quantification of reservoir framework / Rebecca R. Harrington and F. Jerry Lucia -- Developing a wireline-log database and a basis for determining reservoir porosity / Jeffrey A. Kane and James W. Jennings, Jr. -- Calculation of permeability and initial water saturations from wireline logs in a mature carbonate reservoir / F. Jerry Lucia and Jeffrey A. Kane -- Construction and analysis of three-dimensional seismic porosity inversion models / Hongliu Zeng -- Reservoir modeling and simulation of the Fullerton Clear Fork reservoir, Andrews County, Texas / Fred P. Wang and F. Jerry Lucia -- CD-ROM material: Appendix 1 (Plates / Stephen C. Ruppel) ; Appendix 2 (Core analysis data / Stephen C. Ruppel) ; Appendix 3 (Core slab photographs / Stephen C. Ruppel) ; Appendix 4 (Photomicrographs / Stephen C. Ruppel)
Carbonate reservoirs --- Carbonate reservoirs --- Petroleum --- Geology --- Geology --- Geology, Stratigraphic --- Hydrocarbon reservoirs --- Oil reservoir engineering --- Sedimentary basins --- Géologie --- Réservoirs carbonatés --- Pétrole --- Geology --- Development. --- Recherche --- Géologie. --- Yeso Formation (N.M. and Tex.) --- Permian Basin (Tex. and N.M.)
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Dating and geochemical analyses of detrital minerals (mainly zircons) combined with traditional methods, such as heavy minerals and sandstone modes, are a powerful tool in paleogeographic and paleotectonic research and industrial applications.
Research & information: general --- detrital zircon U-Pb geochronology --- bulk geochemistry --- provenance --- tectonic setting --- West Bogeda Shan --- U-Pb geochronology --- detrital zircon --- source-to-sink --- provenance analysis --- mixing model --- sediment budgeting --- east China seas --- Pennsylvanian --- Sino-Korean Block --- detrital zircons --- U–Pb ages --- subduction zones --- U–Pb dating --- sandstone petrography --- peripheral bulge --- tectonics --- zircon U-Pb ages --- muscovite 40Ar/39Ar ages --- sediment provenance --- Yangtze River --- detrital-zircon age spectrum --- Ereendavaa terrane --- Mongol-Okhotsk orogenic belt --- opening of the Mongol-Okhotsk ocean --- northeastern Mongolia --- Lu-Hf isotopes --- early Miocene --- Yinggehai-Song Hong Basin --- South China Sea --- stratigraphic thicknesses --- net sand to gross thickness ratio --- conglomerate percentage --- heavy mineral analysis --- detrital zircon U‒Pb geochronology --- Intermontane basin --- Mongolia --- laser ablation U-Pb dating --- Hafnium isotope-ratio --- terrane definition --- paleotectonic reconstruction --- Western Andes --- Miocene --- Silante Formation --- Ecuador --- compositional heterogeneity --- major element --- nonmarine basin --- gejiu basalts --- zircon U–Pb dating --- geochemistry --- Sr–Nd–Pb isotope --- petrogenesis --- Cameroon --- Meiganga --- gold placer --- trace element --- geochronology --- Archean-Proterozoic origins --- zircon crystal morphology --- zircon textures --- zircon trace elements --- alteration of zircon --- REE in zircon --- rare metal granites --- Li-F granites --- Western Hercynian Meseta --- Permian basin --- Tiddas Souk Es-Sebt des ait ikko volcanic basin --- U–Pb geochronology --- mineralogy --- petrology --- n/a --- U-Pb ages --- U-Pb dating --- zircon U-Pb dating --- Sr-Nd-Pb isotope
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Dating and geochemical analyses of detrital minerals (mainly zircons) combined with traditional methods, such as heavy minerals and sandstone modes, are a powerful tool in paleogeographic and paleotectonic research and industrial applications.
detrital zircon U-Pb geochronology --- bulk geochemistry --- provenance --- tectonic setting --- West Bogeda Shan --- U-Pb geochronology --- detrital zircon --- source-to-sink --- provenance analysis --- mixing model --- sediment budgeting --- east China seas --- Pennsylvanian --- Sino-Korean Block --- detrital zircons --- U–Pb ages --- subduction zones --- U–Pb dating --- sandstone petrography --- peripheral bulge --- tectonics --- zircon U-Pb ages --- muscovite 40Ar/39Ar ages --- sediment provenance --- Yangtze River --- detrital-zircon age spectrum --- Ereendavaa terrane --- Mongol-Okhotsk orogenic belt --- opening of the Mongol-Okhotsk ocean --- northeastern Mongolia --- Lu-Hf isotopes --- early Miocene --- Yinggehai-Song Hong Basin --- South China Sea --- stratigraphic thicknesses --- net sand to gross thickness ratio --- conglomerate percentage --- heavy mineral analysis --- detrital zircon U‒Pb geochronology --- Intermontane basin --- Mongolia --- laser ablation U-Pb dating --- Hafnium isotope-ratio --- terrane definition --- paleotectonic reconstruction --- Western Andes --- Miocene --- Silante Formation --- Ecuador --- compositional heterogeneity --- major element --- nonmarine basin --- gejiu basalts --- zircon U–Pb dating --- geochemistry --- Sr–Nd–Pb isotope --- petrogenesis --- Cameroon --- Meiganga --- gold placer --- trace element --- geochronology --- Archean-Proterozoic origins --- zircon crystal morphology --- zircon textures --- zircon trace elements --- alteration of zircon --- REE in zircon --- rare metal granites --- Li-F granites --- Western Hercynian Meseta --- Permian basin --- Tiddas Souk Es-Sebt des ait ikko volcanic basin --- U–Pb geochronology --- mineralogy --- petrology --- n/a --- U-Pb ages --- U-Pb dating --- zircon U-Pb dating --- Sr-Nd-Pb isotope
Choose an application
Dating and geochemical analyses of detrital minerals (mainly zircons) combined with traditional methods, such as heavy minerals and sandstone modes, are a powerful tool in paleogeographic and paleotectonic research and industrial applications.
Research & information: general --- detrital zircon U-Pb geochronology --- bulk geochemistry --- provenance --- tectonic setting --- West Bogeda Shan --- U-Pb geochronology --- detrital zircon --- source-to-sink --- provenance analysis --- mixing model --- sediment budgeting --- east China seas --- Pennsylvanian --- Sino-Korean Block --- detrital zircons --- U-Pb ages --- subduction zones --- U-Pb dating --- sandstone petrography --- peripheral bulge --- tectonics --- zircon U-Pb ages --- muscovite 40Ar/39Ar ages --- sediment provenance --- Yangtze River --- detrital-zircon age spectrum --- Ereendavaa terrane --- Mongol-Okhotsk orogenic belt --- opening of the Mongol-Okhotsk ocean --- northeastern Mongolia --- Lu-Hf isotopes --- early Miocene --- Yinggehai-Song Hong Basin --- South China Sea --- stratigraphic thicknesses --- net sand to gross thickness ratio --- conglomerate percentage --- heavy mineral analysis --- detrital zircon U‒Pb geochronology --- Intermontane basin --- Mongolia --- laser ablation U-Pb dating --- Hafnium isotope-ratio --- terrane definition --- paleotectonic reconstruction --- Western Andes --- Miocene --- Silante Formation --- Ecuador --- compositional heterogeneity --- major element --- nonmarine basin --- gejiu basalts --- zircon U-Pb dating --- geochemistry --- Sr-Nd-Pb isotope --- petrogenesis --- Cameroon --- Meiganga --- gold placer --- trace element --- geochronology --- Archean-Proterozoic origins --- zircon crystal morphology --- zircon textures --- zircon trace elements --- alteration of zircon --- REE in zircon --- rare metal granites --- Li-F granites --- Western Hercynian Meseta --- Permian basin --- Tiddas Souk Es-Sebt des ait ikko volcanic basin --- mineralogy --- petrology
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