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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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Southern Africa
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Namibia
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Tsumeb Namibia (1)
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South Africa
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Merensky Reef (2)
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West Africa
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Raasay (10)
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Rhum (50)
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Outer Hebrides (3)
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Highland region Scotland
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oxygen
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illite (1)
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sulfides (4)
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Primary terms
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absolute age (13)
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Africa
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Southern Africa
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Namibia
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Tsumeb Namibia (1)
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South Africa
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Bushveld Complex (3)
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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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Arctic Ocean
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Arctic region
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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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Yakutia Russian Federation (1)
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Atlantic Ocean
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Faeroe-Shetland Basin (1)
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Atlantic Ocean Islands
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carbon
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organic carbon (2)
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Cenozoic
-
Quaternary
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Holocene (3)
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Pleistocene
-
upper Pleistocene
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Devensian
-
upper Devensian (2)
-
-
Weichselian
-
upper Weichselian
-
Younger Dryas (3)
-
-
-
-
-
-
Tertiary
-
Neogene
-
Miocene
-
Topopah Spring Member (1)
-
-
Pliocene
-
Cimmerian (1)
-
-
-
Paleogene
-
Eocene
-
lower Eocene (1)
-
-
Paleocene
-
lower Paleocene (1)
-
-
Paleocene-Eocene Thermal Maximum (1)
-
-
-
-
Chordata
-
Vertebrata
-
Pisces
-
Osteichthyes
-
Actinopterygii
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Teleostei (1)
-
-
-
-
Tetrapoda
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Reptilia
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Diapsida
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Archosauria
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Crocodilia (1)
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dinosaurs
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Ornithischia
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Stegosaurus (1)
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Saurischia
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Sauropoda (4)
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Theropoda
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Coelurosauria
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Tyrannosauridae (1)
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-
-
-
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Pterosauria (1)
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crystal growth (4)
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crystal structure (6)
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diagenesis (6)
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East Pacific Ocean Islands
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ecology (3)
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Europe
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Alps (1)
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Scotland
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Great Glen Fault (2)
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Hebrides
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Inner Hebrides
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Isle of Skye (109)
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Mull Island (4)
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Raasay (10)
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Rhum (50)
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-
Outer Hebrides (3)
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Highland region Scotland
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Caithness Scotland (1)
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Gairloch Scotland (1)
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Inverness-shire Scotland
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Isle of Skye (109)
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Raasay (10)
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Rhum (50)
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Sutherland Scotland
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Moine thrust zone (3)
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faults (18)
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How great is the Great Glen Fault?
Otoliths from the Lealt Shale Formation, Great Estuarine Group, Middle Jurassic (Bathonian), Inner Hebrides, Scotland
U−Pb geochronology and microstructural analysis of apatite within a Proterozoic crustal-scale shear zone, Outer Hebrides, NW Scotland
Debris flow at Luib on the A87 strategic road: Isle of Skye, Scotland
The impact of igneous intrusions on sedimentary host rocks: insights from field outcrop and subsurface data
A revision of the ‘coelophysoid-grade’ theropod specimen from the Lower Jurassic of the Isle of Skye (Scotland )
Concretionary cementation of a Scottish Middle Jurassic sandstone by hot, Paleocene fluids: a clumped isotope study
New postcranial remains from the Lealt Shale Formation of the Isle of Skye, Scotland, showcase hidden pterosaur diversity in the Middle Jurassic
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)
Geology and petroleum prospectivity of the Sea of Hebrides Basin and Minch Basin, offshore NW 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.
A VISIT TO LOUIS-ALBERT NECKER ON THE ISLE OF SKYE, 1852.
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.