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