Abstract
The bypass margins in the Apennines were created on the escarpments of large normal faults, which broke up a large, continuous platform into a group of small, isolated platform remnants. The marginal escarpments of these platforms are characterized by a series of deep grooves that were cut into the escarpment by the subaqueous erosive action of bypassing sediment swept off the tops of the platforms and deposited in the basins. -from Authors
Original language | English (US) |
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Pages (from-to) | 565-568 |
Number of pages | 4 |
Journal | Geology |
Volume | 13 |
Issue number | 8 |
DOIs | |
State | Published - Jan 1 1985 |
All Science Journal Classification (ASJC) codes
- Geology