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Further subdivision of both arenites and wackes into three specific sandstone families is based on the relative proportions of three major framework grain types: quartz (Q), feldspar (F), and rock fragments (R for rock fragment, or L for lithic fragment).
Statistical data show that the content of lithic fragment is positive correlation to ACR.
Feldspar and lithic fragment are the main dissolution minerals in the Xujiahe Formation.
Secondary pores are intragranular and intergranular dissolution pores created by the dissolution of feldspars and lithic fragment.
We observe that the An and Fe/(Fe + Mg) values of the Plag#1 lithic fragment do not overlap with that of any lithologic component.
Samples were subsequently polished with 0.3-μm alumina powder to remove the carbon coating and warmed to ~100 °C for ~1 min to soften the CrystalBond© adhesive for removal of each lithic fragment.
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Transported till reflects a similar divergent flow pattern based on dispersal geometries for multiple indicators (e.g., heavy minerals and lithic fragments), which are aligned with the dominant and latest ice flow direction.
A large portion of the matrix in ancient wackes must therefore be secondary, derived either from the disaggregation of feldspar and fine-grained lithic fragments like shale, phyllite, and volcanic rocks or from the postdepositional infiltration of clay- and silt-size clasts from overlying beds.
The aggregate is composed of lithic fragments and monocrystalline grains.
40Ar/39Ar ages of individual plagioclase-rich lithic fragments.
Lithic fragments include volcanic and country rocks (Fig. 3c, d).
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