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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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Kenya (1)
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Mozambique (1)
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Madagascar
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Antananarivo Madagascar (1)
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North Africa
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Morocco (1)
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Southern Africa
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South Africa (1)
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Antarctica
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Arctic region
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Asia
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Oman (1)
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Central Asia
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Kazakhstan
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Far East
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China
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Indonesia
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Java
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Japan
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Oita Japan
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Middle East
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Iran (1)
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Sri Lanka (1)
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Atlantic Ocean
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Canada
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Cascade Range (3)
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Central America
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Commonwealth of Independent States
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Kazakhstan
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Russian Federation
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Kamchatka Peninsula
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Murmansk Russian Federation
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Russian Pacific region (3)
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Sakhalin Russian Federation
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Craters of the Moon (1)
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East Pacific Ocean Islands
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Hawaii
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Europe
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Mexico
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Oceania
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Hawaii
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Tonga (1)
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Old Faithful Geyser (1)
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Pacific Ocean
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United States
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Arizona
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Atlantic Coastal Plain
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Kern County California
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Mono Craters (3)
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Southern California (1)
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Hawaii
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Idaho (1)
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Minnesota
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Mojave Desert (2)
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Montana
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New Mexico
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fluorine (7)
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hydrogen
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incompatible elements (2)
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isotope ratios (21)
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isotopes
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tritium (3)
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stable isotopes
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Ar-40/Ar-36 (1)
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C-13/C-12 (2)
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Cl-37/Cl-35 (1)
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D/H (9)
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deuterium (6)
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He-4/He-3 (2)
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O-17/O-16 (1)
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O-18/O-16 (14)
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S-34/S-32 (1)
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Sr-87/Sr-86 (1)
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large-ion lithophile elements (1)
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metals
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actinides
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thorium (1)
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alkaline earth metals
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strontium
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aluminum (2)
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nitrogen (4)
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noble gases
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argon
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helium
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oxygen
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O-17/O-16 (1)
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sulfur
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trace metals (1)
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fossils
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Reptilia
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dinosaurs
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Synapsida
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Invertebrata
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microfossils
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geochronology methods
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geologic age
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Cenozoic
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Quaternary
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upper Holocene (1)
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Pleistocene
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upper Pleistocene (1)
-
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Tertiary
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Paleogene
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Eocene
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lower Eocene (1)
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Oligocene
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Fish Canyon Tuff (1)
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Paleocene
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lower Paleocene
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K-T boundary (1)
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upper Cenozoic (1)
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Laurentide ice sheet (1)
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Mesozoic
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Cretaceous
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Clearwater Formation (2)
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Upper Cretaceous
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Jurassic
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Triassic
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Paleozoic
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lower Paleozoic (1)
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Precambrian
-
upper Precambrian
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Proterozoic
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Neoproterozoic (1)
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igneous rocks
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kimberlite (3)
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plutonic rocks
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granodiorites
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pegmatite (3)
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porphyry (1)
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volcanic rocks
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andesites (3)
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basalts
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alkali basalts
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flood basalts (1)
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basanite (3)
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glasses
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obsidian (3)
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nephelinite (1)
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phonolites (5)
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pyroclastics
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pumice (2)
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tuff (5)
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rhyolites (10)
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tephrite (1)
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trachytes (3)
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volcanic ash (1)
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metamorphic rocks
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eclogite (1)
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granulites (2)
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metasedimentary rocks
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metasomatic rocks
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greisen (1)
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migmatites
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schists
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-
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meteorites
-
meteorites
-
stony meteorites
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achondrites
-
Martian meteorites
-
SNC Meteorites
-
chassignite
-
Chassigny Meteorite (1)
-
-
-
-
-
-
-
-
minerals
-
carbonates
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bastnaesite (1)
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calcite (3)
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dolomite (1)
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magnesite (1)
-
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halides
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chlorides
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halite (1)
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fluorides
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fluorite (2)
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zinnwaldite (1)
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iodides (1)
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minerals (7)
-
molybdates
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powellite (1)
-
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native elements
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diamond (2)
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oxides
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aluminum oxides (1)
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anatase (1)
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hematite (1)
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hydroxides (1)
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iron oxides (1)
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magnetite (5)
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niobates
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pyrochlore (1)
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pseudobrookite (1)
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rutile (2)
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titanium oxides (1)
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phosphates
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apatite (8)
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fluorapatite (1)
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silicates
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asbestos (1)
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chain silicates
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amphibole group
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carpholite (1)
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pyroxene group
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clinopyroxene
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orthopyroxene
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framework silicates
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feldspar group
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alkali feldspar
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K-feldspar (2)
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sanidine (3)
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plagioclase
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anorthite (2)
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leucite (1)
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nepheline group
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silica minerals
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opal (2)
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quartz (12)
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sodalite group
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nosean (1)
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zeolite group
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analcime (2)
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chabazite (1)
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natrolite (1)
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phillipsite (1)
-
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orthosilicates
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nesosilicates
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andalusite (1)
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garnet group
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grossular (1)
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kyanite (1)
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olivine group
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forsterite (1)
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olivine (9)
-
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water vapor
Significance of tridymite distribution during cooling and vapor-phase alteration of ignimbrites
Are Vapor-Like Fluids Viable Ore Fluids for Cu-Au-Mo Porphyry Ore Formation?
Constraints on deep, CO 2 -rich degassing at arc volcanoes from solubility experiments on hydrous basaltic andesite of Pavlof Volcano, Alaska Peninsula, at 300 to 1200 MPa
Temperature Reconstructions Using Speleothems
Triple Oxygen Isotope Systematics in the Hydrologic Cycle
Vapor-bubble growth in olivine-hosted melt inclusions
Metamorphic Fluids in Orogenic Settings
The hydrothermal system of Bagni San Filippo (Italy): fluids circulation and CO 2 degassing
Abstract The existing controversy regarding the climatic response to given changes in the geomagnetic field intensity (e.g. climate cooling or warming in periods of geomagnetic field strengthening) raises scepticism about the existence of any relationship between both variables. The main shortcomings of the recent understanding of the geomagnetic field–climate relationship are the expectations for: (i) its universal character over the globe; and (ii) the zonal homogeneity of this relationship. This paper offers a new conceptual framework aimed at resolving the existing controversy and explaining the mechanism for the appearance of geomagnetic footprints on climatic records. We show that particles trapped in the Earth's radiation belts are subject to geomagnetic lensing in the parts of their trajectories closest to the surface, being focused or defocused at different regions over the world. The irregularly distributed ionization, created in such a way near the tropopause, activates various ion–molecular reactionships which affect the atmospheric composition there. Thus, the regional changes in the ozone and water vapour are furthermore projected onto the surface temperature and pressure. Consequently, the geomagnetic field–climate relationship is not a rigid but, rather, a flexible one because it is mediated by the near-tropopause ionization, ozone and humidity, with each of them being subject to the other's influence.