| 1. | Orogenic belts can form during the assembly of continents and supercontinents.
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| 2. | The assembly of a supercontinent would have to show intercratonic orogenic belts.
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| 3. | Foliation is common in rocks affected by the regional orogenic belts ).
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| 4. | Sarmatia is made up of several once-independent Archaean orogenic belts.
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| 5. | In a Alpine, Carpathian, and Dinaride orogenic belts.
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| 6. | Intercratonic orogenic belts are characteristic of ocean basin closure.
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| 7. | However, interpretation of orogenic belts can be difficult.
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| 8. | Thrust faults occur in the foreland basin which occur marginal to orogenic belts.
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| 9. | These include intracontinental orogenic belts may also produce phonolites.
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| 10. | Intracratonic orogenic belts occur as thrust belts and do not contain any oceanic material.
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