Podrobnosti záznamu

    Causes of compositional diversity in a lobe of the Half Dome granodiorite, Tuolumne Batholith, Central Sierra Nevada, California
    Economos, Rita
    Erdmann, Saskia
    Memeti, Valbone
    Miller, Jonathan
    Paterson, Scott
    Žák, Jiří
Typ dokumentu
    článek v periodiku
Zdrojový dokument - seriál
    Earth and Environmental Science Transactions of the Royal Society of Edinburgh
    Roč. 100, č. 1-2
Výraz tezauru
Klíčové slovo
Abstrakt (anglicky)
   The causes of compositional diversity in the Tuolumne Batholith, whether source heterogeneity, magma mixing, or fractional crystallisation, is a matter of longstanding debate. This paper presents data from detailed mapping and a microstructural and major element, trace element and isotopic study of an elongate lobe of the Half Dome granodiorite that protrudes from the southern end of the batholith. The lobe it; normally zoned from quartz diorite along the outer margin to high-silica leucogranite in the core. Contacts are steep and gradational, except for the central leucogranite contact, which is locally sharp: magmatic fabrics overprint contacts.
    UK Praha, Přírodovědecká fakulta
Kód přispěvatele
    UK, PřF
Zdrojový formát
Datum importu
    8. 8. 2012