Published April 22, 2022
| Version v1
Dataset
Open
Mid-Miocene to recent tectonic evolution of the Punta Stilo Swell (Calabrian Arc, southern Italy): an effect of Calabrian Arc migration.
Authors/Creators
- 1. National Institute of Oceanography and Experimental Geophysics - OGS
- 2. University of Calabria
Description
An approach consisting of seismics, wells, bathymetrics and literature information provides a better understanding of the origin of an unknown submerged morphological high, the so-called Punta Stilo Swell (S Italy). The Punta Stilo Swell is the expression of alternating phases between contractional, extensional and extetnsional/transpressional tectonics occurred since late Messinian onwards, linked to the Calabrian Arc kinematics
Files
Figura bat 3 con terra.tif
Files
(694.8 kB)
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md5:5c1573ebe92155a02a6d12420da5fc6d
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394 Bytes | Download |
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md5:580d1492774e250e448578f483ff556a
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37 Bytes | Download |
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289.3 kB | Preview Download |