AgeSpectraAnalyst: A MATLAB based package to model zircon age distributions in silicic magmatic systems. [PDF]
Tavazzani L +6 more
europepmc +1 more source
The nature and polygenetic origin of orbicular granodiorite in the Lower Castle Creek pluton, northern Sierra Nevada batholith, California [PDF]
Arthur G. Sylvester
openalex +1 more source
Pan-African alkali granites and syenites of Kerala as imprints of taphrogenic magmatism in the South Indian shield [PDF]
Granite and syenite plutons with alkaline affinities ranging in age from 550 to 750 Ma sporadically puncture the Precambrian granulites of the Kerala region.
Drury, S. A., Iyer, S. S., Santosh, M.
core +1 more source
The making of pure quartzose sand in continental interiors: Paraná River (Brazil and Argentina)
ABSTRACT As part of a comprehensive project on sedimentary processes in South America, this study focuses on sediment generation in the intracratonic Paraná Basin and monitors the evolution of sand composition along the Paraná River from central Brazil to the Río de la Plata estuary in Argentina.
Eduardo Garzanti +5 more
wiley +1 more source
Diapirs of crystal-rich slurry explain granite emplacement temperature and duration. [PDF]
Copley A, Weller O, Bain H.
europepmc +1 more source
Establishing Genetic Relationships between the Takidani Pluton and Two Large Silicic Eruptions in the Northern Japan Alps [PDF]
Eva Hartung +4 more
openalex +1 more source
Dating C/S Structures in Syntectonic Granites by In Situ Rb‐Sr Analyses on Muscovite
ABSTRACT The interplay of crystallisation, deformation and fluid–rock interactions makes deciphering geochronological information complex in syntectonic granites. In this study, we apply in situ Rb‐Sr analyses to selected samples from the Questembert Variscan syntectonic granite in Western France, which was emplaced along the South Armorican Shear Zone
Philippe Boulvais, Romain Tartèse
wiley +1 more source
Synsedimentary deformation and thrusting on the eatern margin of the Barberton Greenstone belt, Swaziland [PDF]
Mapping on the eastern margin of the 3.6 to 3.3 Ga Barberton Greenstone Belt NW Swaziland has revealed a tectonic complex which is more than 5 km thick. The area consists of fault bound units made up of three lithological associations. Some of these were
Lamb, S. H.
core +1 more source

