Podrobnosti záznamu

Předmětová skupina
    magmatický krb
Článek
    The Central Bohemian Plutonic Complex : A multi-generation intrusive complex with locally developed mafic-silicic layered magma chambers
    Characteristics of internal contacts in the Tuolumne Batholith, central Sierra Nevada, California (USA): Implications for episodic emplacement and physical processes in a continental arc magma chamber
    Eastern Margin of the Tuolumne Intrusive Suite (Sierra Nevada Batholith): Magmatic Fabrics, Internal Structures, Host Rocks Deformation and Emplacement Models in a Continental Island Arc Magma Chamber
    Four magmatic fabrics in the Tuolumne batholith, central Sierra Nevada, California (USA) : implications for interpreting fabric patterns in plutons and evolution of magma chambers in the upper crust
    Geochemical variations within the Upper Oligocene-Lower Miocene lava succession of Úhošť Hill (NE margin of Doupovské hory Mts., Czech Republic)
    Is stoping a volumetrically significant pluton emplacement process? : discussion
    Magma Chamber Construction during Crustal Thickening and Subsequent Exhumation: An Example of Interplay between Magmatic and Tectonic Processes from the Central Bohemian Batholith (Bohemian Massif)
    Magmatic erosion of the solidification front during reintrusion: the eastern margin of the Tuolumne batholith, Sierra Nevada, California
    Magmatic history of the Altenberg-Teplice caldera in the aspect of Th-U data
    Physical Processes Along Internal Boundaries in an Continental Arc Magma Chamber: Tuolumne Batholith, Central Sierra Nevada, California (USA)
    Plagioclase-mantled K-feldspar in the Carboniferous porphyritic microgranite of Altenberg-Frauenstein, Eastern Erzgebirge/Krušné Hory
    Quartz and feldspar zoning in the eastern Erzgebirge volcano-plutonic complex (Germany, Czech Republic): evidence of multiple magma mixing
    Quartz phenocrysts stratigraphy of the Teplice rhyolite a window into stratified magma chambers
    Succession of Lava Flows of Úhošť Hill in Relation to the History of Magma Reservoir
    Das "Underplatin-Modell", angewandt auf aktive Prozesse in der Unterkruste und im subkontinentalen Mantel unter dem westlichen Eger-Rift