Effects of Diagenetic Alterations on Hydrocarbon Reservoirs and Water Aquifers
Reservoir quality (porosity and permeability) and heterogeneity in carbonate and siliciclastic hydrocarbon reservoirs and groundwater aquifers are significantly constrained by diagenetic processes, such as biological, chemical, biochemical, and mechanical changes, that occur in sediments subsequent...
में बचाया:
| स्वरूप: | Online |
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| भाषा: | अंग्रेज़ी |
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MDPI - Multidisciplinary Digital Publishing Institute
2022
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| ऑनलाइन पहुंच: | ONIX_20221117_9783036555461_51 |
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| _version_ | 1869515764456751104 |
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| collection | Directory of Open Access Books |
| description | Reservoir quality (porosity and permeability) and heterogeneity in carbonate and siliciclastic hydrocarbon reservoirs and groundwater aquifers are significantly constrained by diagenetic processes, such as biological, chemical, biochemical, and mechanical changes, that occur in sediments subsequent to deposition and prior to low-grade metamorphism. Diagenesis, which has a variable but overall important impact on reservoir quality evolution, is controlled by several inter-related parameters. These parameters include the depositional composition of the sediments, depositional facies, sequence stratigraphy, pore water chemistry, burial history and tectonic setting of the basin, and paleoclimatic conditions.Carbonate and siliciclastic sediments often undergo multiple stages of diagenesis, which are related to complex patterns of burial-thermal history (subsidence and uplift) that are controlled by the tectonic evolution of the basin. Tectonic evolution of the basin is controlled by the position of the basin with respect to the type and activity along the plate boundaries. The episodes of burial and uplift may result in profound modifications in the pressure–temperature regimes and in the extent of mineral–water interaction, and hence in various phases of compaction, as well as mineral dissolution, recrystallization, transformation, and cementation. Diagenesis impacts reservoir quality in the following ways: (i) destruction by mechanical compaction and extensive cementation, (ii) preservation by prevention of mechanical and chemical compaction, or (iii) generation by dissolution of labile framework grains and intergranular cements. |
| format | Online |
| id | doab-20.500.12854ir-93794 |
| institution | Directory of Open Access Books |
| language | eng |
| publishDate | 2022 |
| publishDateRange | 2022 |
| publishDateSort | 2022 |
| publisher | MDPI - Multidisciplinary Digital Publishing Institute |
| publisherStr | MDPI - Multidisciplinary Digital Publishing Institute |
| record_format | ojs |
| spelling | doab-20.500.12854ir-937942024-03-28T03:31:30Z Effects of Diagenetic Alterations on Hydrocarbon Reservoirs and Water Aquifers Mansurbeg, Howri quartz cement oxygen isotopes silica sources tight sandstones Sichuan Basin drusy dolomite dolomitization cementation hot basinal fluids fluid flow Paleozoic Huron Domain origin of diagenetic fluids strontium isotope-laser ablation ICP-MS upper jurassic carbonate rocks ZTFB NE-Iraq hydrothermal fluids cold meteoric waters Upper Cretaceous carbonate rocks U-Pb geochronology fluid inclusion microthermometry n/a thema EDItEUR::G Reference, Information and Interdisciplinary subjects::GP Research and information: general thema EDItEUR::R Earth Sciences, Geography, Environment, Planning Reservoir quality (porosity and permeability) and heterogeneity in carbonate and siliciclastic hydrocarbon reservoirs and groundwater aquifers are significantly constrained by diagenetic processes, such as biological, chemical, biochemical, and mechanical changes, that occur in sediments subsequent to deposition and prior to low-grade metamorphism. Diagenesis, which has a variable but overall important impact on reservoir quality evolution, is controlled by several inter-related parameters. These parameters include the depositional composition of the sediments, depositional facies, sequence stratigraphy, pore water chemistry, burial history and tectonic setting of the basin, and paleoclimatic conditions.Carbonate and siliciclastic sediments often undergo multiple stages of diagenesis, which are related to complex patterns of burial-thermal history (subsidence and uplift) that are controlled by the tectonic evolution of the basin. Tectonic evolution of the basin is controlled by the position of the basin with respect to the type and activity along the plate boundaries. The episodes of burial and uplift may result in profound modifications in the pressure–temperature regimes and in the extent of mineral–water interaction, and hence in various phases of compaction, as well as mineral dissolution, recrystallization, transformation, and cementation. Diagenesis impacts reservoir quality in the following ways: (i) destruction by mechanical compaction and extensive cementation, (ii) preservation by prevention of mechanical and chemical compaction, or (iii) generation by dissolution of labile framework grains and intergranular cements. 2022-11-17T16:25:03Z 2022-11-17T16:25:03Z 2022 book ONIX_20221117_9783036555461_51 9783036555461 9783036555454 https://directory.doabooks.org/handle/20.500.12854/93794 eng image/jpeg Attribution 4.0 International https://mdpi.com/books/pdfview/book/6223 https://mdpi.com/books/pdfview/book/6223 MDPI - Multidisciplinary Digital Publishing Institute 10.3390/books978-3-0365-5546-1 10.3390/books978-3-0365-5546-1 46cabcaa-dd94-4bfe-87b4-55023c1b36d0 9783036555461 9783036555454 134 Basel open access |
| spellingShingle | quartz cement oxygen isotopes silica sources tight sandstones Sichuan Basin drusy dolomite dolomitization cementation hot basinal fluids fluid flow Paleozoic Huron Domain origin of diagenetic fluids strontium isotope-laser ablation ICP-MS upper jurassic carbonate rocks ZTFB NE-Iraq hydrothermal fluids cold meteoric waters Upper Cretaceous carbonate rocks U-Pb geochronology fluid inclusion microthermometry n/a thema EDItEUR::G Reference, Information and Interdisciplinary subjects::GP Research and information: general thema EDItEUR::R Earth Sciences, Geography, Environment, Planning Effects of Diagenetic Alterations on Hydrocarbon Reservoirs and Water Aquifers |
| title | Effects of Diagenetic Alterations on Hydrocarbon Reservoirs and Water Aquifers |
| title_full | Effects of Diagenetic Alterations on Hydrocarbon Reservoirs and Water Aquifers |
| title_fullStr | Effects of Diagenetic Alterations on Hydrocarbon Reservoirs and Water Aquifers |
| title_full_unstemmed | Effects of Diagenetic Alterations on Hydrocarbon Reservoirs and Water Aquifers |
| title_short | Effects of Diagenetic Alterations on Hydrocarbon Reservoirs and Water Aquifers |
| title_sort | effects of diagenetic alterations on hydrocarbon reservoirs and water aquifers |
| topic | quartz cement oxygen isotopes silica sources tight sandstones Sichuan Basin drusy dolomite dolomitization cementation hot basinal fluids fluid flow Paleozoic Huron Domain origin of diagenetic fluids strontium isotope-laser ablation ICP-MS upper jurassic carbonate rocks ZTFB NE-Iraq hydrothermal fluids cold meteoric waters Upper Cretaceous carbonate rocks U-Pb geochronology fluid inclusion microthermometry n/a thema EDItEUR::G Reference, Information and Interdisciplinary subjects::GP Research and information: general thema EDItEUR::R Earth Sciences, Geography, Environment, Planning |
| topic_facet | quartz cement oxygen isotopes silica sources tight sandstones Sichuan Basin drusy dolomite dolomitization cementation hot basinal fluids fluid flow Paleozoic Huron Domain origin of diagenetic fluids strontium isotope-laser ablation ICP-MS upper jurassic carbonate rocks ZTFB NE-Iraq hydrothermal fluids cold meteoric waters Upper Cretaceous carbonate rocks U-Pb geochronology fluid inclusion microthermometry n/a thema EDItEUR::G Reference, Information and Interdisciplinary subjects::GP Research and information: general thema EDItEUR::R Earth Sciences, Geography, Environment, Planning |
| url | ONIX_20221117_9783036555461_51 |