31. Xenoliths of granulite-facies metamorphic rock resemble those found in eastern Antarctica. 32. The Urgonian facies completely surrounds the Parentis Basin and persists into the Albian. 33. Special subduction related metamorphism to blueschist facies is known from the B�rka nappe. 34. The graptolite-bearing shales were later metamorphosed into lower amphibolite facies slates. 35. In many areas there is a frequent alternation of limestone and dolomite facies . 36. Depositional facies include the Uriconian and the Longmyndian sequences. 37. Passing from open-water the facies change to nearshore and alluvial deposits. 38. Around the lake margins, distinctive shoreline facies developed. 39. Oligocene clastic rocks can also act as reservoir rocks in distal fan facies . 40. The defomration associated with the orogeny can be seen in amphibolite facies metamorphism.
