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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Africa
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East Africa
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Ethiopia (1)
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Ethiopian Rift (1)
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Russian Federation
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sulfides (1)
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Primary terms
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Africa
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East Africa
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Ethiopia (1)
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Ethiopian Rift (1)
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Southern Africa
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Karoo Basin (2)
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Asia
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Far East
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China
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atmosphere (2)
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brines (1)
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carbon
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C-13/C-12 (2)
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organic carbon (2)
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Cenozoic
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Quaternary
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upper Quaternary (2)
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Tertiary
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Paleogene
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Eocene
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middle Eocene (1)
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Central America
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Nicaragua
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Masaya (1)
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crust (1)
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earthquakes (1)
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Europe
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Caucasus
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Northern Caucasus (1)
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Scythian Platform (1)
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Southern Europe
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Greece
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Greek Aegean Islands
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faults (1)
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igneous rocks
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plutonic rocks
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diabase (1)
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granites (1)
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volcanic rocks
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andesites (1)
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basalts
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dacites (1)
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rhyolites (1)
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inclusions
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intrusions (2)
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isotopes
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C-13/C-12 (2)
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O-18/O-16 (1)
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magmas (6)
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mantle (1)
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Mediterranean region
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Aegean Islands
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Greek Aegean Islands
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Cyclades
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Thera (1)
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Mesozoic
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Triassic
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Lower Triassic
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Permian-Triassic boundary (1)
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metal ores (1)
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metals
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iron (1)
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mercury (3)
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metamorphism (1)
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nitrogen (2)
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oxygen
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O-18/O-16 (1)
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paleoclimatology (1)
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Paleozoic
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Permian
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Ecca Group (1)
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Upper Permian
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Permian-Triassic boundary (1)
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palynomorphs (1)
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Plantae
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algae
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nannofossils (1)
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Precambrian
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remote sensing (1)
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sedimentary rocks (3)
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South America
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springs (1)
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thermal waters (1)
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rock formations
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sedimentary rocks
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sedimentary rocks (3)
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Mercury efficiently volatilized but not completely removed from sediments around igneous intrusions
Large Igneous Provinces and the Release of Thermogenic Volatiles from Sedimentary Basins
Experimentally derived F, Cl, and Br fluid/melt partitioning of intermediate to silicic melts in shallow magmatic systems
Deoxygenation and organic carbon sequestration in the Tethyan realm associated with the middle Eocene climatic optimum
Ecological disturbance in tropical peatlands prior to marine Permian-Triassic mass extinction
Santorini Volcano and its Plumbing System
Volcanic Sulfides and Outgassing
The magmatic and eruptive response of arc volcanoes to deglaciation: Insights from southern Chile
Structural controls on fluid pathways in an active rift system: A case study of the Aluto volcanic complex
Remote sensing of volcanoes and volcanic processes: Integrating Observation and Modelling – Introduction
Airborne thermal remote sensing of the Volcán de Colima (Mexico) lava dome from 2007 to 2010
Abstract We investigate high-resolution digital photographs and infrared images of the lava dome eruption at Volcán de Colima, from 2007 to 2010. Qualitative observations provide insight into active volcanic processes (e.g. rockfalls and fracturing) and show that, as the dome advances a substantial cooled talus apron develops, which stabilizes the structure. Progressive collapse of the talus apron as it reaches the crater rim corresponds with the development of a lava lobe, extruding hot lava from deeper within the dome. Quantitative dome surface temperature time-series show that the highest temperature hotspots migrate from the dome sides (250–380 °C) to the top (150–300 °C) and finally to the lava lobe (220–400 °C) as the structurally unstable areas expose fresh material. Net surface heat loss from the dome ranges from 5 to 30 MW, comparable to other dome forming systems. Heat budget calculations confirm that the lava dome retained a hot viscous core throughout the period 2007–2010. We propose that the mechanical stability of the Volcán de Colima dome arises from the shear strength of flanking talus which stabilizes the hot viscous core.
Abstract The Ozone Monitoring Instrument (OMI) is a satellite-based ultraviolet (UV) spectrometer with unprecedented sensitivity to atmospheric sulphur dioxide (SO 2 ) concentrations. Since late 2004, OMI has provided a high-quality SO 2 dataset with near-continuous daily global coverage. In this review, we discuss the principal applications of this dataset to volcano monitoring: (1) the detection and tracking of large eruption clouds, primarily for aviation hazard mitigation; and (2) the use of OMI data for long-term monitoring of volcanic degassing. This latter application is relatively novel, and despite showing some promise, requires further study into a number of key uncertainties. We discuss these uncertainties, and illustrate their potential impact on volcano monitoring with OMI through four new case studies. We also discuss potential future avenues of research using OMI data, with a particular emphasis on the need for greater integration between various monitoring strategies, instruments and datasets.