Revealing the Mineralogical and Petrographic Signs of Fluid-Related Processes in the Kelebia Basement Area (Szeged Basin, S Hungary): A Case Study of Alpine Prograde Metamorphism in a Permo-Triassic Succession

Table 1

Sample descriptions.

Location	Formation	Borehole (core number)	Sample code	Depth (m)	Type
Kel field	Permian red beds (underlain by the ignimbrites)	Kel–14 (#3)	ÁGK–244, no. 153	905.0	Thin sections and core chip
	Gyűrűfű Rhyolite (Permian ignimbrites)	Kel–7 (#6)	ÁGK–230, no. 24	869.5 and 870.2	Thin sections
		Kel–7 (#7)	ÁGK–231, no. 142	877.5	Thin sections and core chip
		Kel–7 (#8)	ÁGK–232	900.0	Thin section and core chip
		Kel–11 (#5)	ÁGK–240, no. 150	863.0	Thin sections
		Kel–12 (#1)	ÁGK–242, no. 151	836.0	Thin section
		Kel–14 (#4)	ÁGK–245	928.0	—
		Kel–22 (#10)	ÁGK–251, no. 158	823.0	Thin section
		Kel–22 (#12)	ÁGK–252	828.0	Thin section
		Kel–22 (#18)	ÁGK–253, no. 160	843.0	Thin section
		Kel–22 (#23)	ÁGK–254, no. 161	860.5	Thin sections
		Kel–23 (#3)	ÁGK–1866	833.0	Thin section
	Korpád Sandstone (overlain by the ignimbrites)	Kel–12 (#3)	ÁGK–243, no. 152	871.5	Thin sections
Ás–É field	Lower Miocene conglomerate (Triassic pebbles)	Ás–É–4 (#3)		1,963	Thin sections
		Ás–É–9 (#2)		2,045	Thin sections
Móra field	Jakabhegy Sandstone (Lower Triassic)	Móra–1 (#17)	M–1/17/1A, M–1/17/2	2,306	Thin sections and core chip