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The chemical compositions of rocks are used to solve numerous geological problems, including crystallization history of igneous bodies such as granite or basalt, processes of formation of the sea floor, nature of chemical weathering in various climates, stratigraphic correlation of sedimentary and volcanic rocks, processes of ore generation, and many others. Most rocks are composed primarily of silicate minerals, and over 90% of the composition of most silicate rocks can be characterized by oxides of Si, Ti, Al, Fe, Mg, Ca, Na and K. Minor and trace elements present in rocks include practically every other element, many of which are especially useful for geochemical modelling of geological processes.