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About GEO 321 LECTURE NOTES - Section - 6
1) Geosynclines are subsiding troughs where thick sequences of sediments are deposited and later compressed into mountain belts. They are divided into eugeosynclines and miogeosynclines based on sediment type and depth of deposition. 2) The document discusses the different tectonic plates that make up Africa, including several stable cratons and less stable terranes. Major rifting events starting in the Late Carboniferous separated the continents of Gondwana. 3) Key tectonic features of the African plate mentioned include the Central and West African Rift System, the West African Mobile Belt, and the Cape Mobile Belt.
Detailed Information
| Author: | ['Muhammad mubaraq'] |
|---|---|
| Publication Year: | 2022 |
| Pages: | 10 |
| Language: | English |
| Format: | |
| Price: | FREE |
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