Lithospheric flexure, uplift, and landscape evolution in south-central England
The high level river gravels in Oxfordshire (the Northern Drift Group), which range in age from Early Pleistocene to around 450 ka, contain pebbles that were derived from a source area to the north near Birmingham. The pebbles could not have been transported across the Upper Triassic and Lower Juras...
| Format: | Journal article |
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| Published: |
Geological Society Publishing House
2000
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