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hydrogen
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porphyry (2)
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volcanic rocks
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tuff (3)
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impact statements (1)
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inclusions
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fluid inclusions (9)
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Indian Ocean
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industrial minerals (14)
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interplanetary space (1)
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intrusions (30)
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Invertebrata
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Echinodermata
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isostasy (1)
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isotopes
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radioactive isotopes
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K-40 (1)
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Th-232 (1)
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U-238 (1)
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stable isotopes
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C-13/C-12 (7)
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D/H (2)
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deuterium (1)
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He-3 (1)
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O-18/O-16 (6)
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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-206 (1)
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S-34/S-32 (4)
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Sr-87/Sr-86 (2)
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kaolin deposits (2)
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land use (19)
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Malay Archipelago
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mantle (13)
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maps (19)
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Mediterranean region
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Mediterranean Sea
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Mesozoic
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Cretaceous
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Lower Cretaceous
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Aptian (1)
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Upper Cretaceous
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K-T boundary (1)
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Jurassic
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Upper Jurassic (2)
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Triassic
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Montney Formation (1)
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metal ores
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base metals (10)
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chromite ores (3)
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IOCG deposits (1)
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metals
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actinides
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thorium
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Th-232 (1)
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uranium
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U-234 (1)
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U-238 (1)
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alkali metals
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cesium (2)
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potassium
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K-40 (1)
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alkaline earth metals
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calcium (1)
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strontium
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Sr-87/Sr-86 (2)
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aluminum (1)
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iron
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lead
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Pb-206/Pb-204 (1)
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manganese (1)
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platinum group
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platinum ores (7)
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metamorphic rocks
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marbles
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metamorphism (19)
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Mexico
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mineral deposits, genesis (112)
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Moon (5)
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nitrogen (1)
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noble gases
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helium
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radon (1)
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nodules (4)
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nonmetal deposits (7)
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nonmetals (7)
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North America
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Appalachians
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Basin and Range Province
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ocean basins (1)
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Ocean Drilling Program
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ocean floors (15)
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Oceania
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Pacific Coast (1)
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West Pacific
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Pacific region
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paleoclimatology (4)
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Paleozoic
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Bedford Shale (1)
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Cambrian
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Kanmantoo Group (1)
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Lower Cambrian
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Shady Dolomite (1)
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Carboniferous
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Lower Carboniferous
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Dinantian (2)
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Mississippian
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Boone Formation (1)
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Lower Mississippian
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Pocono Formation (1)
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Tournaisian (1)
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Middle Mississippian
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Visean (1)
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Sunbury Shale (1)
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Pennsylvanian
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Conemaugh Group (1)
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Monongahela Group (1)
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Upper Carboniferous (3)
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Devonian
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Dunkard Group (1)
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Ordovician
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Permian
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Upper Permian (1)
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Sauk Sequence (1)
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Silurian
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upper Paleozoic
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Antrim Shale (1)
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paragenesis (14)
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petrology (22)
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Plantae
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Spermatophyta
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Myrtaceae
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Gymnospermae
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Coniferales
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Pinus (1)
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plate tectonics (22)
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Precambrian
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Central Rand Group (1)
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upper Precambrian
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Proterozoic
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Neoproterozoic
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Vendian (1)
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Paleoproterozoic (8)
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reclamation (4)
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reefs (6)
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coal
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South America
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sulfur
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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
mineral resources
Delineating the Lithotectonic Domains in the Eastern Ghats Mobile Belt: Implication for the Regional Exploration of the Metasediment Hosted Graphite and Manganese Ore Horizons
Mineralogy and Paragenesis of the Boundary Zone Zn-Pb ± Ag Deposit, Yukon, Canada
The Geology, Geochemistry, and Mineralogy of the Moa Bay Ni Laterite Mining District, Cuba
The Magino Gold Deposit, Ontario, Canada: An Overprinted Archean Intrusion-Related Gold Deposit
Fractures and faults across intrusion-induced forced folds: a georesource perspective
Abstract Intruding magma can create space by uplift and elastic bending of the overburden, which locally fractures the deforming volume and produces flat-topped or dome-like forced folds. Here, I map such fracture networks and quantify their geometry and connectivity across a range of natural and modelled intrusion-induced forced folds. I show that there is a positive relationship between forced fold length and amplitude, and all fracture networks comprise traces, with variable lengths and orientations, that are more intense and denser where fold curvature is greatest. Fracture length populations are typically best described by power-law distributions, but some fit better to log-normal or exponential distributions. Connectivity of fracture networks is low and generally increases with folding, but resurfacing by eruptive products can disrupt this trend. My work supports previous analyses of forced folds and fractures, suggesting that we can use the fracture characteristics of exposed forced folds to predict that of buried forced folds. Due to their geometry and fracture network, intrusion-induced forced folds make ideal fluid traps. As these forced folds are common in many volcanic settings and sedimentary basins, we should consider their potential as exploration targets for water, magmatic-related mineral and metal deposits, and particularly CO 2 storage.
Structural Defects of Heavy Rare Earth Element Minerals in Granite Accelerate Their Decomposition and Facilitate Mineralization During Weathering
SOME CHARACTERISTICS AND CAUSES OF CHANGES IN THE RATE OF DISCOVERY OF NEW MINERALS SINCE 1800
Zircon and Whole-Rock Trace Element Indicators of Magmatic Hydration State and Oxidation State Discriminate Copper Ore-Forming from Barren Arc Magmas
Practical applications of quality assurance and quality control in mineral exploration, resource estimation and mining programmes: a review of recommended international practices
Deep resistivity geophysics of the San Juan–Silverton caldera complex, San Juan County, Colorado (USA)
‘Practically useful, scientifically important, and to the honour of the country’: geological maps and services provided by the Geological Survey of Norway these past 165 years
Abstract Geological maps document knowledge of considerable value (economic, cultural and aesthetic) for societies, enterprises and people in general. Knowledge illustrated in geological maps also helps us to foresee how landscape interventions and climate change may affect our living ground and make us vulnerable to geohazards. The present paper presents an overview of geological mapping carried out by the Geological Survey of Norway since 1858 while also focusing on mapping activities and products produced in the present millennium. Key issues to consider are how we are moving into the digital world, how we use geological mapping to follow up on national agendas like Green Shift and Blue Growth and how national agreements and cooperation help us to make geological and other geographic information available to everyone through open access web portals and services.