Swiss Journal of Geosciences

Table 1 δ¹⁸O and/or δ¹³C values obtained from the different whole rocks (pebbles) and their veins (quartz and calcite)

From: Sediment provenance during Alpine orogeny: fluid inclusions and stable isotopes on quartz–calcite veins from detritic pebbles

Sample	Whole rock			Vein
Sample	Pebble petrology	δ¹⁸O (‰ relative to SMOW)	δ¹³C (‰ relative to PDB)	Host mineral	δ¹⁸O (‰ relative to SMOW)	δ¹³C (‰ relative to PDB)
SL1a	Basalt	17		Qtz	22.8
				Cal	20.7	−2.01
SL2b	Sandy limestone	22.8	−4	Cal	27.3	−1.14
SL2c	Dolomitic sandstone	20.6		Qtz	23.3
SL2g	Dolomitic sandstone	22.4	1.2	Qtz	23.5
SL2h	Dolomitic sandy limestone	22.7		Cal	25.7	2.05
SL2i	Sandy limestone	24.3	1.4	Qtz	26.3
				Cal	24.5	1.35
SL3b	Dolomitic sandstone	21.5		Qtz	24.7
SL5a	Micaceous sandstone	20		Cal	25.3	1.69
SL3e	Cement of conglomerates			Cal	20	−1.7
Standard	Carrare	29.14	2.1

The δ¹⁸O values have been measured on the silicate part of the whole rock and on quartz and calcite minerals of the veins, while the δ¹³C values have been measured on the carbonate fraction of the whole rocks (when possible) and on calcite minerals of the veins

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