作者: Gautam Sen , Gautam Sen
DOI: 10.1007/978-3-642-38800-2_6
关键词: Igneous rock 、 Igneous textures 、 Magma chamber 、 Petrology 、 Nephelinite 、 Fractional crystallization (geology) 、 Geology 、 Geochemistry 、 Xenolith 、 Cumulate rock 、 Rock cycle
摘要: In the previous chapter we learned that magmas can vary considerably in chemical composition and hence their mineralogy. What are causes for such diversity? Is it possible all major magma types somehow genetically related? this focus on processes modify of magmas.