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Invertebrata
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Insecta (4)
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Trilobitomorpha
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Brachiopoda
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Articulata
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Inarticulata (2)
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Echinodermata
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Mytilus
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Cephalopoda
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Vermes
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Metazoa (8)
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Plantae
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Filicopsida
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Spermatophyta
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lower Paleogene (1)
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Oligocene (5)
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K-T boundary (4)
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Dalradian (2)
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Franciscan Complex (2)
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Lower Triassic
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Bunter
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Voltzia Sandstone (1)
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Permian-Triassic boundary (4)
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Thaynes Formation (1)
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Middle Triassic (1)
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Nicola Group (2)
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upper Mesozoic (2)
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Paleozoic
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Cambrian
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Carboniferous
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Pennsylvanian
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Minturn Formation (1)
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Upper Carboniferous
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Casper Formation (1)
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Old Red Sandstone (2)
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Popovich Formation (1)
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Upper Devonian
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Knox Group (1)
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lower Paleozoic
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middle Paleozoic (2)
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New Albany Shale (1)
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Upper Ordovician
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Ashgillian (3)
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Wufeng Formation (1)
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Permian
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Ecca Group (2)
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Lower Permian
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Qixia Formation (1)
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Lyons Sandstone (1)
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Permian-Triassic boundary (4)
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Sauk Sequence (1)
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Silurian
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Lockport Formation (1)
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Lower Silurian
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Tuscarora Formation (1)
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Middle Silurian (2)
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Niagaran (1)
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Tippecanoe Sequence (1)
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Dwyka Formation (1)
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Kaskaskia Sequence (1)
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Phanerozoic (880)
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Proterozoic
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Paleoproterozoic
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Sinian
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igneous rocks
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Tieschitz Meteorite (1)
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L chondrites (1)
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minerals
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alloys (1)
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carbonates
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halides
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K-bentonite (1)
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minerals (8)
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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
Phanerozoic
Cadmium isotope constraints on primary productivity and environmental perturbations across the Late Ordovician mass extinction Available to Purchase
Parental magma and mantle source compositions of chromitites in the Mesoarchean Nuggihalli greenstone belt, India: evidence for Archean subduction zone magmatism Available to Purchase
Subductability of continental lithosphere Available to Purchase
How does a soft collision orogen uplift and collapse? Insight from the eastern Central Asian Orogenic Belt Available to Purchase
Multicyclic Phanerozoic orogeny recorded in the Qaidam continent, northern Tibet: Implications for the tectonic evolution of the Tethyan orogenic system Available to Purchase
Phanerozoic emergence of global continental collision and onset of massive crustal eclogitization Available to Purchase
An evolutionary system of mineralogy, Part VIII: The evolution of metamorphic minerals Available to Purchase
Seawater sulfate dynamics and a new tipping point in the Earth system Available to Purchase
Scotland's geology: evolution, crustal structure and societal relevance Free
The Geological History of Water: From Earth’s Accretion to the Modern Deep Water Cycle Open Access
Hydrological phenomena related to elevation head on the Arabian Plate Available to Purchase
Structural interpretation of the basement beneath the Southern Desert of Iraq based on aeromagnetic data Available to Purchase
Insights into the Phanerozoic evolution of the São Francisco Craton based on detrital zircon thermochronology and U-Pb-Hf geochronology Available to Purchase
The Fractional MacroEvolution Model: a simple quantitative scaling macroevolution model Open Access
Modelling sulfate concentrations in the global ocean through Phanerozoic time Open Access
The history of palynology in Egypt Available to Purchase
Tracking cycles of Phanerozoic opening and closing of ocean basins using detrital rutile and zircon geochronology and geochemistry Open Access
Site classification scheme based on geological age and genesis for Xinjiang and the Capital Metropolitan areas of China Available to Purchase
Nature and origin of heterogeneities in the lithospheric mantle in the context of asthenospheric upwelling and mantle wedge zones: What do mantle xenoliths tell us? Open Access
The present contribution synthesizes the main petrographic, mineralogical and chemical features of mantle xenoliths uplifted by Phanerozoic lavas. The collections of mantle xenoliths consist predominantly of peridotites but minor pyroxenites are commonly associated. Two main petrogenetic processes are responsible for the features of mantle xenoliths: partial melting and circulation of melts/fluids and associated metasomatic and magmatic processes. Partial melting processes lead to the formation of residual pieces of upper mantle while two main types of mantle metasomatism could be recognized such as LILE enrichment, the first referring to asthenosphere upwelling settings (essentially mantle plumes, rifting zones and asthenosphere window zones) and the second to mantle wedge settings. The AUZ (asthenospheric upwelling zones) metasomatism is essentially related to the migration of more or less CO 2 -rich alkaline silicate melts and associated fluids while the MWZ (mantle wedge zones) metasomatism is associated with the activity of hydrated liquids (fluids) commonly SiO 2 -rich.