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"Chapters examine Columbia River Basalt Group stratigraphy, update the nomenclature, revise basalt ages, and update the volume of basalt and areal extent of flows; discuss current ideas on the petrogenesis for the Columbia River Basalt Group; and address the tectonic and structural development of the Columbia River Flood Basalt province"--
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"Gathers together papers focused on understanding oceanic large igneous provinces from their origin and evolution to environmental impacts. Research presented has made extensive use of dredge samples and cores collected by scientific ocean drilling. Samples from terrestrial sequences are also integrated into understanding global environmental consequences of oceanic LIPs"--
Igneous rocks. --- Volcanism. --- Flood basalts. --- Magmatism. --- Petrology.
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Stratigraphic correlation --- Paleomagnetism --- Flood basalts --- Idaho --- United States
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552.3 --- Flood basalts --- Volcanism --- Volcanicity --- Vulcanism --- Geodynamics --- Volcanology --- Flood volcanism --- Plateau basalts --- Basalt --- Lava flows --- Magmatic rocks. Igneous rocks --- 552.3 Magmatic rocks. Igneous rocks
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Rock deformation --- Geology, Stratigraphic --- Flood basalts --- Geology, Structural --- From 570 million to 2 billion years ago --- Lake Superior Region.
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Geology --- Mines and mineral resources --- Ore deposits --- Lava flows --- Volcanic ash, tuff, etc. --- Flood basalts --- Rhyolite --- Nevada.
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This book describes the microbiota of the intertrappean beds in the Chhindwara District, Madhya Pradesh, India. In this work, special emphasis is placed on the microbiota from the Late Cretaceous-Early Palaeocene transition of the central Narmada River region. Recently, the intertrappean beds of the Eastern Deccan Volcanic Province (one of the subprovinces of the Deccan Volcanic Province) have received considerable attention, which resulted in the addition of some significant biotic assemblages to the existing record from the Dindori-Chhindwara area of the province. The biotic assemblages include charophytes, ostracods, foraminiferans, fishes, frogs, lizards, turtles, crocodiles, and mammals. In spite of the recent discoveries, the known fossil record of the Late Cretaceous-Early Palaeocene biota of India is not sufficient and thus does not permit us to speculate on the possible impact of environmental changes triggered by the Deccan volcanic lava flows on the contemporary biota and to precisely document their palaeoecologic, palaeoenvironmental and palaeobiogeographic implications. The recent biotic reports from the intertrappean beds exposed in the Chhindwara region of the Eastern Deccan Volcanic Province clearly indicate that these beds have a vast potential in terms of fossil content, which could reveal new and dissimilar biotic remains when compared to the Western Deccan Volcanic Province. The record of diverse accumulations of freshwater charophytes, brackish to freshwater ostracods, and planktic foraminiferal and fish assemblages from the intertrappean beds of Jhilmili and adjacent areas of Early Danian (P1a) age and lying just north of Chhindwara town and in the heart of peninsular India has intriguing implications for defining the age limits of the basaltic flows. The occurrence of non-marine taxa, for example, algae, molluscs, and vertebrates, associated with brackish water ostracods in the nearby Singpur and Mohgaon Kalan localities of the Chhindwara region, has also raised concerns about the sedimentary environments of these intertrappean beds. The new finds (presented in this book) prove useful for the better understanding of the palaeoecology and palaeoenvironment of the biota and also throw light on various paleobiogeographic models proposed for the northward drifting Indian plate. The microbiotic assemblages of the intertrappean beds of the eastern Deccan volcanic province at District Chhindwara, Madhya Pradesh are documented in this book. The microbiota of the central Narmada River region, the charophytes, ostracods, planktic foraminifera, and fishes, receive special attention in this study.
Deccan traps. --- Microorganisms --- Micropaleontology. --- Micropaleontology --- Paleontology --- Germs --- Micro-organisms --- Microbes --- Microscopic organisms --- Organisms --- Microbiology --- Deccan basalts --- Deccan flood basalts --- Traps, Deccan --- Flood basalts --- Paleoecology. --- Paleontology. --- Bioinformatics. --- Archaeology. --- Earth sciences. --- Computational and Systems Biology. --- Earth Sciences. --- Geosciences --- Environmental sciences --- Physical sciences --- Archeology --- Anthropology --- Auxiliary sciences of history --- History --- Antiquities --- Bio-informatics --- Biological informatics --- Biology --- Information science --- Computational biology --- Systems biology --- Fossilogy --- Fossilology --- Palaeontology --- Paleontology, Zoological --- Paleozoology --- Historical geology --- Zoology --- Fossils --- Prehistoric animals in motion pictures --- Palaeoecology --- Ecology --- Paleobiology --- Data processing
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552.3 --- Flood basalts --- -Volcanism --- -Geology, Structural --- -Geotectonics --- Structural geology --- Tectonics (Geology) --- Physical geology --- Volcanicity --- Vulcanism --- Geodynamics --- Volcanology --- Flood volcanism --- Plateau basalts --- Basalt --- Lava flows --- Magmatic rocks. Igneous rocks --- -Magmatic rocks. Igneous rocks --- 552.3 Magmatic rocks. Igneous rocks --- -552.3 Magmatic rocks. Igneous rocks --- Geotectonics --- Geology, Structural --- Volcanism
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This unique book presents hundreds of spectacular photographs of large-scale to small-scale field geological features of flood basalt volcanism from around the world. Major flood basalt provinces covered in this book include the British Palaeogene, Central Atlantic Magmatic Province, Columbia River, Deccan, East Greenland, Emeishan, Ethiopian, Ferrar-Karoo-Tasmania, Iceland, Indo-Madagascar, Paraná, Siberian, West Greenland, and others. Intermediate- to small-sized flood basalts (such as Saudi Arabia and South Caucasus) are also included. Different chapters of the book illustrate varied features of flood basalts, including landscapes, lava flow morphology and stacking, structures formed during lava flow transport, inflation and degassing, structures produced during lava solidification, subaqueous volcanism and volcanosedimentary associations, explosive volcanism, intrusions, igneous processes and magmatic diversity, tectonic deformation, secondary mineralization, and weathering and erosion. This book will be valuable for a large audience: specialists studying flood basalt volcanology, petrology, geochemistry, geochronology, geophysics, and environmental impact and mass extinction links; nonspecialists who want to know more about flood basalts; field geologists (such as those working in geological surveys); students of volcanology and igneous petrology, and even people employed in the industry, such as those working on flood basalt-hosted groundwater or petroleum reservoirs.
Earth sciences. --- Geology. --- Mineralogy. --- Geophysics. --- Geomorphology. --- Environmental monitoring. --- Geoecology. --- Environmental geology. --- Earth Sciences. --- Geophysics/Geodesy. --- Geoecology/Natural Processes. --- Monitoring/Environmental Analysis. --- Flood basalts. --- Volcanism. --- Volcanicity --- Vulcanism --- Geodynamics --- Volcanology --- Flood volcanism --- Plateau basalts --- Basalt --- Lava flows --- Physical geography. --- Ecology. --- Physical geology --- Crystallography --- Minerals --- Balance of nature --- Biology --- Bionomics --- Ecological processes --- Ecological science --- Ecological sciences --- Environment --- Environmental biology --- Oecology --- Environmental sciences --- Population biology --- Geography --- Geognosy --- Geoscience --- Earth sciences --- Natural history --- Ecology --- Biomonitoring (Ecology) --- Ecological monitoring --- Environmental quality --- Monitoring, Environmental --- Applied ecology --- Environmental engineering --- Pollution --- Geoecology --- Environmental protection --- Geological physics --- Terrestrial physics --- Physics --- Geomorphic geology --- Physiography --- Physical geography --- Landforms --- Measurement --- Monitoring
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The rapid increasing of concentrations of anthropologically generated greenhouse gases (primarily CO2) in the atmosphere is responsible for global warming and ocean acidification. The International Panel on Climate Change (IPCC) indicates that carbon capture and storage (CCS) techniques are a necessary measure to reduce greenhouse gas emissions in the short-to-medium term. One of the technological solutions is the long-term storage of CO2 in appropriate geological formations, such as deep saline formations and depleted oil and gas reservoirs. Promising alternative options that guarantee the permanent capture of CO2, although on a smaller scale, are the in-situ and ex-situ fixation of CO2 in the form of inorganic carbonates via the carbonation of mafic and ultramafic rocks and of Mg/Ca-rich fly ash, iron and steel slags, cement waste, and mine tailings. According to this general framework, this Special Issue collects articles covering various aspects of recent scientific advances in the geological and mineralogical sequestration of CO2. In particular, it includes the assessment of the storage potential of candidate injection sites in Croatia, Greece, and Norway; numerical modelling of geochemical–mineralogical reactions and CO2 flow; studies of natural analogues providing information on the processes and the physical–chemical conditions characterizing serpentinite carbonation; and experimental investigations to better understand the effectiveness and mechanisms of geological and mineralogical CO2 sequestration.
Research & information: general --- Earth sciences, geography, environment, planning --- CO2 reservoir rock --- CO2 sealing capacity --- CO2 sequestration --- CO2 storage capacity --- CO2 storage ratio --- supercritical CO2 --- CO2 geological storage --- depleted gas fields --- deep saline aquifers --- Adriatic offshore --- Croatia --- CO2 geological sequestration --- unconsolidated sediments --- gas hydrates --- suitable methodology for mineral carbonation --- construction and demolition waste --- basalts --- carbonation --- CO2 storage --- hydrochemistry --- regional heat flow --- CO2 leakage --- cement --- well integrity --- leakage remediation --- TOUGHREACT --- reactive transport modelling --- CCS --- mineralization --- carbonatization --- mineral trapping --- mineral sequestration --- Johansen Formation --- North Sea --- sedimentary facies --- serpentinite --- X-ray diffraction --- rietveld refinement --- magnesium leaching --- thermal activation --- meta-serpentine --- heat activation optimization --- CO2 mineral sequestration --- hydromagnesite --- kerolite --- Cu mine --- Montecastelli --- underground microclimate --- replacement process --- low temperature carbonate precipitation --- Secondary Ion Mass Spectrometer --- seawater influx --- hydrothermal circulation --- ophicalcite --- CO2 reservoir rock --- CO2 sealing capacity --- CO2 sequestration --- CO2 storage capacity --- CO2 storage ratio --- supercritical CO2 --- CO2 geological storage --- depleted gas fields --- deep saline aquifers --- Adriatic offshore --- Croatia --- CO2 geological sequestration --- unconsolidated sediments --- gas hydrates --- suitable methodology for mineral carbonation --- construction and demolition waste --- basalts --- carbonation --- CO2 storage --- hydrochemistry --- regional heat flow --- CO2 leakage --- cement --- well integrity --- leakage remediation --- TOUGHREACT --- reactive transport modelling --- CCS --- mineralization --- carbonatization --- mineral trapping --- mineral sequestration --- Johansen Formation --- North Sea --- sedimentary facies --- serpentinite --- X-ray diffraction --- rietveld refinement --- magnesium leaching --- thermal activation --- meta-serpentine --- heat activation optimization --- CO2 mineral sequestration --- hydromagnesite --- kerolite --- Cu mine --- Montecastelli --- underground microclimate --- replacement process --- low temperature carbonate precipitation --- Secondary Ion Mass Spectrometer --- seawater influx --- hydrothermal circulation --- ophicalcite
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