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NARROW
GeoRef Subject
-
all geography including DSDP/ODP Sites and Legs
-
Africa
-
Southern Africa
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Namibia
-
Tsumeb Namibia (1)
-
-
South Africa
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Bushveld Complex (4)
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Merensky Reef (2)
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North-West Province South Africa (1)
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Transvaal region (2)
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West Africa
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Nigeria (1)
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Antarctica
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Antarctic Peninsula (1)
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Arctic Ocean
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Norwegian Sea
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Voring Basin (1)
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Voring Plateau (1)
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Arctic region
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Greenland
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East Greenland (1)
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Skaergaard Intrusion (1)
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Svalbard
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Spitsbergen (2)
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Arran (2)
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Asia
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Far East
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China
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Indian Peninsula
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Middle East
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Cyprus
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Yakutia Russian Federation (1)
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Atlantic Ocean
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Northeast Atlantic (4)
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Atlantic Ocean Islands
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Faeroe Islands (5)
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Atlantic region (5)
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Australasia
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Australia
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Caledonides (7)
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Commonwealth of Independent States
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Europe
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Islay (16)
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Jura Island (2)
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Mull Island (35)
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Hebrides
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Jura Island (2)
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Raasay (10)
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Rhum (52)
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Highland region Scotland
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Ardnamurchan (4)
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Caithness Scotland (1)
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Inverness-shire Scotland
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Isle of Skye (118)
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Raasay (10)
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Rhum (52)
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Sutherland Scotland
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Moine thrust zone (6)
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Scottish Highlands (6)
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Northern Ireland
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Jack Hills (1)
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North America
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Canadian Shield
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North Sea region (1)
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Oceania
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Polynesia
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Hawaii
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Raton Basin (1)
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South America
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Brazil
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United States
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Hawaii
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New York
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Wyoming
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elements, isotopes
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carbon
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C-14 (5)
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chemical ratios (2)
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fluorine (1)
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hydrogen
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deuterium (1)
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isotope ratios (21)
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isotopes
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C-14 (5)
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Pb-206/Pb-204 (1)
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Pb-207/Pb-204 (1)
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stable isotopes
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Nd-144/Nd-143 (3)
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O-18/O-16 (13)
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Pb-207/Pb-204 (1)
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Pb-208/Pb-204 (1)
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S-34/S-32 (3)
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Sr-87/Sr-86 (11)
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metals
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alkaline earth metals
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Sr/Ca (2)
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magnesium
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Mg/Ca (1)
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strontium
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Rb-87/Sr-86 (1)
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Sr/Ca (2)
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Sr-87/Sr-86 (11)
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chromium (1)
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iron (2)
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lead
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Pb-206/Pb-204 (1)
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Pb-207/Pb-204 (1)
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Pb-208/Pb-204 (1)
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platinum ores (4)
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rare earths
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Nd-144/Nd-143 (3)
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terbium (1)
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ytterbium (1)
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zirconium (2)
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noble gases
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helium
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He-4/He-3 (1)
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oxygen
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O-18/O-16 (13)
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sulfur
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S-34/S-32 (3)
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fossils
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Chordata
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Vertebrata
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Pisces (2)
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Tetrapoda
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Mammalia
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Reptilia
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Saurischia
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Theropoda
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Coelurosauria
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Ichthyosauria
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Synapsida (1)
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ichnofossils
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Invertebrata
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Mandibulata
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Ostracoda
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Podocopida
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Echinodermata
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Crinozoa
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Mollusca
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Bivalvia (3)
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Cephalopoda
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Ammonoidea
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Ammonites (1)
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Coleoidea
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Belemnitidae (2)
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Gastropoda (1)
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Protista
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Foraminifera (3)
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microfossils (17)
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Plantae
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Chlorophyta
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Spermatophyta
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thallophytes (2)
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tracks (6)
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geochronology methods
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thermochronology (2)
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geologic age
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Cenozoic
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Quaternary
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lower Holocene (1)
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Pleistocene
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upper Pleistocene
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Devensian
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upper Devensian (5)
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Weichselian
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Loch Lomond Stade (1)
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upper Weichselian
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Younger Dryas (4)
-
-
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-
-
-
Tertiary
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Neogene
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Miocene
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Topopah Spring Member (1)
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Pliocene
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Cimmerian (1)
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Paleogene
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Eocene
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lower Eocene (2)
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middle Eocene (1)
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Oligocene (2)
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Paleocene
-
lower Paleocene
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K-T boundary (3)
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Paleocene-Eocene Thermal Maximum (1)
-
-
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Dalradian (9)
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Mesozoic
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Cretaceous
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Lower Cretaceous (2)
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Upper Cretaceous
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K-T boundary (3)
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Santonian (1)
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Jurassic
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Lower Jurassic
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Toarcian (1)
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upper Liassic (1)
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Middle Jurassic
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Upper Jurassic
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lower Kimmeridgian (1)
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Oxfordian (3)
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Sundance Formation (1)
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Triassic
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Upper Triassic (2)
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Paleozoic
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Cambrian
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Old Red Sandstone (1)
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Sauk Sequence (1)
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Phanerozoic (2)
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Precambrian
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Lewisian Complex (4)
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upper Precambrian
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Proterozoic
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Mesoproterozoic
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Neoproterozoic
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Moinian (2)
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Torridonian (13)
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Paleoproterozoic (2)
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igneous rocks
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igneous rocks
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feldspathoid rocks (1)
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plutonic rocks
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troctolite (5)
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felsite (5)
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lamprophyres (1)
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ultramafics
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peridotites (10)
-
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volcanic rocks
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basalts
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alkali basalts
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columnar basalt (1)
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glasses
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pyroclastics
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welded tuff (2)
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rhyodacites (5)
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-
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ophiolite (1)
-
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metamorphic rocks
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metamorphic rocks
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amphibolites (1)
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gneisses (6)
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marbles (2)
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metaigneous rocks
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metagabbro (1)
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metasedimentary rocks
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metasomatic rocks
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skarn (5)
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ophiolite (1)
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meteorites
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minerals
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alloys
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borates
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sakhaite (1)
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carbonates
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calcite (4)
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dolomite (1)
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magnesian calcite (1)
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sakhaite (1)
-
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K-bentonite (1)
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minerals (9)
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native elements (1)
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oxides
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baddeleyite (1)
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chrome spinel (2)
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hematite (2)
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spinel (2)
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-
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phosphates
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britholite (1)
-
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silicates
-
chain silicates
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amphibole group (2)
-
pyroxene group
-
clinopyroxene
-
augite (1)
-
-
-
tobermorite (1)
-
wollastonite group
-
wollastonite (3)
-
-
-
framework silicates
-
feldspar group
-
alkali feldspar
-
K-feldspar (1)
-
sanidine (1)
-
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plagioclase (6)
-
-
scapolite group
-
scapolite (1)
-
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silica minerals
-
quartz (1)
-
-
-
orthosilicates
-
nesosilicates
-
britholite group
-
britholite (1)
-
-
garnet group
-
grossular (1)
-
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harkerite (2)
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mullite (1)
-
olivine group
-
fayalite (1)
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forsterite (2)
-
olivine (6)
-
-
titanite group
-
titanite (1)
-
-
zircon group
-
zircon (4)
-
-
-
sorosilicates
-
epidote group
-
allanite (1)
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epidote (1)
-
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kilchoanite (1)
-
melilite group
-
melilite (1)
-
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vesuvianite (1)
-
-
-
sheet silicates
-
clay minerals
-
dickite (1)
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kaolinite (1)
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montmorillonite (1)
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saponite (2)
-
smectite (1)
-
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illite (1)
-
mica group
-
biotite (1)
-
phengite (1)
-
-
-
-
sulfates
-
anhydrite (1)
-
-
sulfides
-
pyrite (1)
-
-
-
Primary terms
-
absolute age (22)
-
Africa
-
Southern Africa
-
Namibia
-
Tsumeb Namibia (1)
-
-
South Africa
-
Bushveld Complex (4)
-
Merensky Reef (2)
-
North-West Province South Africa (1)
-
Transvaal region (2)
-
-
-
West Africa
-
Nigeria (1)
-
-
-
Antarctica
-
Antarctic Peninsula (1)
-
-
Arctic Ocean
-
Norwegian Sea
-
Voring Basin (1)
-
Voring Plateau (1)
-
-
-
Arctic region
-
Greenland
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East Greenland (1)
-
Skaergaard Intrusion (1)
-
-
Svalbard
-
Spitsbergen (2)
-
-
-
Asia
-
Buryat Russian Federation (1)
-
Far East
-
China
-
Dabie Mountains (1)
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Sulu Terrane (1)
-
-
-
Indian Peninsula
-
India (1)
-
-
Middle East
-
Cyprus
-
Troodos Massif (1)
-
-
-
Yakutia Russian Federation (1)
-
-
Atlantic Ocean
-
North Atlantic
-
Jeanne d'Arc Basin (1)
-
Northeast Atlantic (4)
-
-
-
Atlantic Ocean Islands
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Faeroe Islands (5)
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Shetland Islands (3)
-
-
Atlantic region (5)
-
Australasia
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Australia
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Northern Territory Australia (1)
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Western Australia (1)
-
-
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biogeography (1)
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biography (2)
-
boron (1)
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boron deposits (1)
-
Canada
-
Eastern Canada
-
Newfoundland and Labrador
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Newfoundland (1)
-
-
-
Muskox Intrusion (1)
-
Nunavut
-
Sverdrup Islands
-
Axel Heiberg Island (1)
-
-
-
Queen Elizabeth Islands
-
Sverdrup Islands
-
Axel Heiberg Island (1)
-
-
-
-
carbon
-
C-13/C-12 (8)
-
C-14 (5)
-
organic carbon (3)
-
-
Cenozoic
-
Quaternary
-
Holocene
-
lower Holocene (1)
-
-
Pleistocene
-
upper Pleistocene
-
Devensian
-
upper Devensian (5)
-
-
Weichselian
-
Loch Lomond Stade (1)
-
upper Weichselian
-
Younger Dryas (4)
-
-
-
-
-
-
Tertiary
-
Neogene
-
Miocene
-
Topopah Spring Member (1)
-
-
Pliocene
-
Cimmerian (1)
-
-
-
Paleogene
-
Eocene
-
lower Eocene (2)
-
middle Eocene (1)
-
-
Oligocene (2)
-
Paleocene
-
lower Paleocene
-
K-T boundary (3)
-
-
-
Paleocene-Eocene Thermal Maximum (1)
-
-
-
-
Chordata
-
Vertebrata
-
Pisces (2)
-
Tetrapoda
-
Mammalia
-
Docodonta (1)
-
-
Reptilia
-
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Inner Hebrides
Seawater signatures in the supracrustal Lewisian Complex, Scotland
Sintering as a key process in the textural evolution of chromitite seams in layered mafic-ultramafic intrusions
Reply to discussion on ‘Deglaciation and neotectonics in SE Raasay, Scottish Inner Hebrides’, by Smith et al. 2021 ( SJG , 57, 106–116)
Discussion on ‘Deglaciation and neotectonics in SE Raasay, Scottish Inner Hebrides’ by Smith et al. 2021 ( SJG , 57, 106–116)
A new stratigraphic framework for the early Neoproterozoic successions of Scotland
Deglaciation and neotectonics in SE Raasay, Scottish Inner Hebrides
Emplacement of the Little Minch Sill Complex, Sea of Hebrides Basin, NW Scotland
First and most northern occurrence of a thalattosuchian crocodylomorph from the Jurassic of the Isle of Skye, Scotland
Making oil from magma
Abstract Petroleum systems within rifted margin basins affected by volcanism continue to remain challenging for the exploration of hydrocarbons, most notably owing to the volume of intrusions that pose imaging, drilling and exploration problems. Typically, intrusions possess small thermal aureoles, but despite this, there is evidence that intrusions could none the less be responsible for the generation of commercial volumes of hydrocarbons. Here we shed new light on this petroleum systems challenge by integrating organic geochemical and Raman spectroscopic techniques to produce potential volumetric data for hydrocarbons generated as a result of igneous intrusion. The results indicate that, in areas with immature source rock intervals, it may be possible for intrusions to generate volumes of oil that would be capable of comfortably filling likely known oil reservoirs. This is a critical step forward in integrating several analytical techniques, indicating that under the right conditions there is the potential for hydrocarbon generation as a result of igneous intrusion.
Introduction to the thematic collection: Exploration Geochemistry at Exploration 17 October 21–25, 2017, Toronto
The effect of cooling rate on immiscible silicate liquid microstructure: an example from the Palaeogene dykes of Northeast England
A VISIT TO LOUIS-ALBERT NECKER ON THE ISLE OF SKYE, 1852.
Very large convergent multi-fluted glacigenic deposits in the NW Highlands, Scotland
New theropod dinosaur teeth from the Middle Jurassic of the Isle of Skye, Scotland
Response of Middle Jurassic shallow-marine environments to syn-depositional block tilting: Isles of Skye and Raasay, NW Scotland
Abstract Archibald Geikie’s (1835–1924) field research led to better understanding of geological relationships and, ultimately, Earth processes. We consider three pieces of research in Scotland, from his early work on Skye through to the execution and impact of his 1860 expedition to the NW Highlands with Murchison, returning to Skye to consider arguments with Judd on igneous relationships. We describe the field locations and place modern interpretations in their historical context. We discuss how methods and approaches for building interpretations in the field were modified and improved through debates. Reliance on a few ‘critical outcrops’ served to anchor interpretation at the expense of understanding more complex exposures. Similar bias appears to have arisen from using simple exploratory transects which were only mitigated by proper mapping approaches. Significant misunderstandings between protagonists appear to have arisen through the reliance of text description rather than diagrammatic illustrations. The vitriolic nature of debate seems to have anchored misinterpretations, obscured interpretational uncertainty and promoted false-reasoning by inhibiting inclusive scientific engagement.