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Example text

Massive coral colonics. There is a small bioherm al Ihis level above the road. A porous, while biiimrcrite forms Ihe massive hed 11. Bed 12 is also massive, il is very resistant to erosion and forms the lidgeoii which Vorbourg chapel is built. pl. 11/151 included Ihis unit into his Vorbourg Member. Il is better to in­ terpret it to be the uppermost pall oil be St-I rsamic Formalion. corroded bedding plane al the lop of bed 12. Ihe base of the Vorbourg Member is marked hi bed 13 and the lop hi bed 24.

Bed I of this section is a massive hiomicrile with massive coral colonies. This is Ihe typical facies of the Grellingen Member (see below). Bed 2 is an oosparitic intercalation. This is the upper pari of the Grellingen Member. The Tiergarien 56 Member of the upper St-Ursanne Formation is an unbedded. almost pure oosparile (bed 4i with peloids at ihe lop (bed 5). 3 m. beds d to 9) crops out in the uppermost part of the cliff. These four beds are mierile wilh some very fine-grained detrital quam (ihin-seetion Gy 7438.

This is a lime mudstone with budseves that is probably a thrombohle. The stromatolitic limestone with rootlets of bed 26 is figured in GVGl (1992. fig. 13, PS Gy 4621). 6 Section RG 400 Corban JU, of marl. Fine-grained tied ilal t|tiail/ and -cklspai arc common, gorge northeast of La Providence (arm (pi. 48 and 5(1. Bed 50 is a quartz pelsparite thai is The section begins al Ihe end of Ihe road wilh Ihe Grellingen depicted in fig. 15. Oneoids occur in beds 43,44,81 and 88. Beds Member of the Sl-Ursanne Formation.

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