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Table 2 Composition of sandstones from the Wagrain basin

From: Formation of an intra-orogenic transtensional basin: the Neogene Wagrain basin in the Eastern Alps

Sample RS 12 RS 25 RS 26 RS 27 RS 28 RS 29 RS 30 RS 31 RS 32 RS 33 RS 34 RS 35
Qm 31.7 38.0 23.8 46.5 49.5 29.8 22.8 51.4 46.3 44.5 41.0 20.3
Qp 3.8 22.3 1.3 4.0 8.5 3.0 1.0 2 6.8 6.5 4.0 6.8
K 5.3 2.0 5.0 7.8 3.8 2 1.8 9.1 3.0 1.3 3.5 1.0
P 2.0 2.3 0.8 3.3 4.8 1.3 4 3.1 1.3 4.3 4.3 2.5
lithsed 2.0 0.5 0.5
lithmeta 0.8 5.0 23.8 3.8 5 5.3 9 1.7 3.8 5.3 2.0 24.0
lithvolc 0.3
Mus 16 15.3 14.8 8.0 7.5 24 24.5 13.7 13.5 16.5 16.5 17.8
Bio 6.2 2.0 12.8 2.0 5.8 5.3 18.3 1.7 6.8 7.3 4.0 11.3
Chl 2.0 1.8 0.8 0.3 1.8 6.5 3.5 3.7 2 3.0 2.8 1.8
Opaque 2.2 0.8 0.8 1.0 1.3 0.6 0.8 2.3 0.5
HMtransl 5.2 4.0 0.5 17.0 3.3 1.8 2.3 2.9 8.3 9.0 10.5 0.5
Cbm
Matrix 24.5 4.8 16.0 7.5 9.8 20.3 11.8 10.0 7.8 2.0 9.3 13.8
Sample no. RS 36 RS 37 RS 38 RS 39 RS 40 RS 42 RS 43 RS 44 RS 45 RS 46 RS 59  
Qm 33.8 31 41.8 41 29.5 43.2 44.9 43.5 39.8 29.8 34.3  
Qp 5.8 1.8 7.0 3.5 0.8 3.7 9.1 2.3 3.0 3.8 5.3  
K 1.5 0.8 2.8 3.3 0.8 4.67 2.6 4.3 1.0 2.8 2.3  
P 2.8 1.3 7.3 4.3 1.8 2.6 1.1 2.5 2.0 2.5 2.0  
lithsed  
lithmeta 16 2.8 5.3 3.3 3.8 5.7 6.0 3.0 3.4 0.8 10.3  
lithvolc 1.4 0.3  
Mus 15.3 32.3 14.5 20.5 24.5 18.3 15.1 14.8 9.8 27.3 17.5  
Bio 5.8 6.8 3.3 4.8 1.5 2.9 0.9 4.3 0.8 8.5 1.3  
Chl 2.8 2.3 4.0 1.3 1.5 2.6 4.9 3.5 7.8 3.0 1.3  
Opaque 0.5 2.5 0.5 0.5 1.8 1.7 0.6 0.5 0.8 0.8  
HMtransl 1.3 2.0 7.0 4.3 0.8 4.3 3.7 6.8 22.0 4.3 9.5  
Cbm 0.3  
Matrix 14.8 16.8 6.8 13.5 22.3 10.6 9.7 15.3 10.3 16.8 15.3  
  1. Q m monocrystalline quartz, Q p polycrystalline quartz, K K-feldspar, P plagioclase, lith sed lithic sedimentary, lith met lithic metamorphic, lith volc lithic volcanic, Mus white mica, Bio biotite, Chl chlorite, HM transl translucent heavy minerals, Cb m monocrystalline carbonate