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  2. Calc-alkaline magma series - Wikipedia

    en.wikipedia.org/wiki/Calc-alkaline_magma_series

    The calc-alkaline magma series is one of two main subdivisions of the subalkaline magma series, the other subalkaline magma series being the tholeiitic series. A magma series is a series of compositions that describes the evolution of a mafic magma, which is high in magnesium and iron and produces basalt or gabbro, as it fractionally crystallizes to become a felsic magma, which is low in ...

  3. Alkaline magma series - Wikipedia

    en.wikipedia.org/wiki/Alkaline_magma_series

    Rocks in the alkaline magma series are distinguished from rocks in the subalkaline tholeiitic and calc-alkaline magma series by their high content of alkali metal oxides (K 2 O plus Na 2 O) relative to silica (SiO 2). They are distinct from the rare peralkaline magmas, which have excess alkali oxides relative to alumina (Na 2 O + K 2 O > Al 2 O 3).

  4. Igneous differentiation - Wikipedia

    en.wikipedia.org/wiki/Igneous_differentiation

    Normative mineralogy – Calculation of the composition of a rock; Alkaline magma series – Series of alkaline magmas produced by igneous differentiation; Calc-alkaline magma series – Subdivision of the subalkaline magma series; Tholeiitic magma series – Series of sub-alkaline magmas

  5. Category:Calc-alkaline rocks - Wikipedia

    en.wikipedia.org/wiki/Category:Calc-alkaline_rocks

    Pages in category "Calc-alkaline rocks" The following 2 pages are in this category, out of 2 total. This list may not reflect recent changes. C.

  6. Dacite - Wikipedia

    en.wikipedia.org/wiki/Dacite

    Dacite (/ ˈ d eɪ s aɪ t /) is a volcanic rock formed by rapid solidification of lava that is high in silica and low in alkali metal oxides. It has a fine-grained ( aphanitic ) to porphyritic texture and is intermediate in composition between andesite and rhyolite .

  7. Igneous rock - Wikipedia

    en.wikipedia.org/wiki/Igneous_rock

    Andesite and basaltic andesite are the most abundant volcanic rock in island arc which is indicative of the calc-alkaline magmas. Some island arcs have distributed volcanic series as can be seen in the Japanese island arc system where the volcanic rocks change from tholeiite—calc-alkalinealkaline with increasing distance from the trench ...

  8. Normative mineralogy - Wikipedia

    en.wikipedia.org/wiki/Normative_mineralogy

    Normative mineralogy is an estimate of the mineralogy of the rock. It usually differs from the visually observable mineralogy, at least as much as the types of mineral species, especially amongst the ferromagnesian minerals and feldspars, where it is possible to have many solid solution series of minerals, or minerals with similar Fe and Mg ratios substituting, especially with water (e.g ...

  9. Volcanic arc - Wikipedia

    en.wikipedia.org/wiki/Volcanic_arc

    In the rock record, volcanic arcs can be recognized from their thick sequences of volcaniclastic rock (formed by explosive volcanism) interbedded with greywackes and mudstones and by their calc-alkaline composition. In more ancient rocks that have experienced metamorphism and alteration of their composition (metasomatism), calc-alkaline rocks ...

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