4. ● Diligent petrographic analysis and point-counting of terrigenous
sands and sandstones demonstrated that the dominant
framework grain types are quartz, feldspar and lithic fragments
(QFL).
● Today, the popular classification schemes incorporate these
three components in triangular QFL plots , originally constructed
by R.H.Dott and later modified by Pettijohn, Potter and Siever, .
8. Arkose with K-feldspar (pinkish-
orangish) and quartz (gray)
grains
Arkose is generally formed from the
weathering of feldspar-rich igneous
or metamorphic, most commonly
granitic, rocks, which are primarily
composed of quartz and feldspar
12. Sample Point
Count
Composition at 300 points is identified. The relative abundance of framework grains
to matrix determines whether the rock is an arenite, a wacke, or a mudstone. The
framework composition is normalized to determine type of arenite or wacke.