Uwe Ring
Biographic Data
| ID | 3527709 |
|---|---|
| NAME | Uwe Ring |
| GIVEN NAMES | Uwe |
| FAMILY NAME | Ring |
| SIGNATURE | RING U |
| AFFILIATIONS | Goethe University Frankfurt |
| ORCID | 0000-0003-3347-9284 |
| VERIFIED | Yes |
| TOTAL WORKS | 3 |
| TOTAL CITATIONS | 15 |
| WORKS AS AUTHOR | 3 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 1993 |
| LATEST PUBLICATION YEAR | 1995 |
| H-INDEX | 2 |
Sedimentology of the Malawi Rift
Shallow water, nearshore lake beds and fluviatile deposits exposed in the Karonga District (northern Malawi) are subdivided into several depositional units which are bounded by unconformities reflecting sedimentary breaks. Prior to the formation of a major perennial lake which also flooded the area studied, sedimentation was characterized by extensive fluviatile deposits mainly formed by reworked material of Jurassic red beds. Formation of a majo…
Geology of the Malawi Rift
Kinematic analysis of Neogene and Quaternary faults demonstrates that the direction of extension in the Malawi Rift rotated from east-northeast to southeast. Rift development commenced at about 8·6 Ma with normal faulting causing erosion and re-sedimentation of Mesozoic deposits and formation of half-grabens bounded by northwest-, north-, and northeast-striking normal faults. Continued normal faulting led to block faulting and basin subsidence wh…
Oldest Homo and Pliocene biogeography of the Malawi Rift
Sedimentology of the Malawi Rift
Shallow water, nearshore lake beds and fluviatile deposits exposed in the Karonga District (northern Malawi) are subdivided into several depositional units which are bounded by unconformities reflecting sedimentary breaks. Prior to the formation of a major perennial lake which also flooded the area studied, sedimentation was characterized by extensive fluviatile deposits mainly formed by reworked material of Jurassic red beds. Formation of a majo…
Geology of the Malawi Rift
Kinematic analysis of Neogene and Quaternary faults demonstrates that the direction of extension in the Malawi Rift rotated from east-northeast to southeast. Rift development commenced at about 8·6 Ma with normal faulting causing erosion and re-sedimentation of Mesozoic deposits and formation of half-grabens bounded by northwest-, north-, and northeast-striking normal faults. Continued normal faulting led to block faulting and basin subsidence wh…
Oldest Homo and Pliocene biogeography of the Malawi Rift
Sedimentology of the Malawi Rift
Shallow water, nearshore lake beds and fluviatile deposits exposed in the Karonga District (northern Malawi) are subdivided into several depositional units which are bounded by unconformities reflecting sedimentary breaks. Prior to the formation of a major perennial lake which also flooded the area studied, sedimentation was characterized by extensive fluviatile deposits mainly formed by reworked material of Jurassic red beds. Formation of a majo…
Geology of the Malawi Rift
Kinematic analysis of Neogene and Quaternary faults demonstrates that the direction of extension in the Malawi Rift rotated from east-northeast to southeast. Rift development commenced at about 8·6 Ma with normal faulting causing erosion and re-sedimentation of Mesozoic deposits and formation of half-grabens bounded by northwest-, north-, and northeast-striking normal faults. Continued normal faulting led to block faulting and basin subsidence wh…
Geology (3 works) · Paleontology (3 works) · Rift (3 works) · East African Rift (2 works) · Evolution and Paleontology Studies (2 works) · Geology (2 works) · Geomorphology (2 works) · Paleontology (2 works) · Pleistocene (2 works) · Pleistocene-Era Hominins and Archaeology (2 works)