![ternary diagram feldspar ternary diagram feldspar](https://slidetodoc.com/presentation_image_h/7a8ee619b7c67d4f4f9097b314163837/image-11.jpg)
Some of the fields are assigned to 2 or 3 rock types, which are further distinguished by their mafic mineral content or plagioclase type ( calcic or sodic). They mostly have similar field divisions, so most volcanic rocks have a corresponding plutonic rock of equivalent mineralogy (for example, rhyolite and granite). There are 2 QAPF diagrams, one for coarse grained ( plutonic) or intrusive igneous rocks, one for fine grained ( volcanic) or extrusive igneous rocks. The QAPF diagram is divided into 15 basic fields that define ranges of mineral compositions for the different classes of rocks.
![ternary diagram feldspar ternary diagram feldspar](https://d32ogoqmya1dw8.cloudfront.net/images/research_education/equilibria/foanq532027.jpg)
The corners represent cases in which only one felsic component is present, effectively 100% of either quartz, alkali-feldspar, plagioclase or foid.īecause foids and quartz are mutually exclusive in an igneous rock, the QAPF classification is always based on a maximum of 3 components, either QAP or APF, and the compositions of the rocks are plotted in either the upper or lower triangle. Then, they interpret a K-Na-Ba triangle diagram by relating compositional data to the four feldspars. Students first verify the chemical formulas for the two new feldspars using the concept of charge balance. It is made of two ternary diagrams with the corners Q, A, P and F, A, P, adjoined to each other along their A-P edge. Part III involves working with barium-bearing feldspars including albite, orthoclase, hyalophane, and the pure Ba end member celsian. The composition of the rocks are plotted into a diamond-shaped coordinate system, the QAPF diagram, also known as Streckeisen diagram (named after the author of the original article). Within the QAPFM classification scheme proposed by the IUGS, rocks with less than 90 vol-% mafic minerals are classified by their content (in volume-%) of: In the next section we discuss the present state of knowledge on the geometry of the ternary feldspar system, and some of the problems of the attainment of equilibrium in natural systems.