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. Lithic-arenite, Rounded to sub-angular weathered alkali feldspar and plagioclase. Rounded and weathered volcaniclasts displaying microlithic texture. Polycrystalline quartz grains. Monocrystalline and rounded to sub-rounded quartz grains. Microcrystalline lithic fragments. Epidote, chlorite, opaque minerals, zircon grains

. Feldsapthic-arenite, Well-sorted (ca. 0.1 mm in diameter), sub-rounded to sub-angular elements. Monocrystalline, weathered feldspar (alkali and plagioclase) grains, sub-rounded to sub-angular quartz grains. Lithic fragments of various origins (volcaniclasts, sedimentary rock fragments?) Opaque minerals

R. With-porphyritic-texture, Perthitic orthoclase (recrystallized after sanidine) phenocrysts. The groundmass contains crystallized area made up of quartz grains showing equilibrated texture and spherolites, also indicative of a crystallization of amorphous groundmass. Opaque minerals

. Lithic-arenite, Well sorted (ca. 0.2 mm in diameter) lithic fragments displaying microcrystalline and microgranular textures

. Monocrystalline, mainly angular but sometimes sub-rounded quartz grains. Rounded, slightly weathered alkaline feldspar and rare plagioclase grains White mica (muscovite) flakes, opaque minerals, chlorite and zircon grains

. Quartz-arenite, Well sorted, coarse (ca. 0.5 mm in diameter), sub-angular to sub-rounded quartz grains. Microgranular and microcrystalline, commonly sub-rounded, lithic fragments. White mica flakes underlining the stratification. Zircon grains displaying various shapes

S. Sedimentary, N. Volcaniclastic, and . Nzr, Probability of concordance ? 10%, decay constants errors included N Detection limits (%) Maximum depositional age DL1(pL=0.5) DL1(pL=0.95) DL3(pL=0.5) DL1(pL=0.95) Concordia age ± (2?) n MSWD Probability Song Da Basin Co Noi Formation