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|Title: ||Synthesis of the Piacenzian onshore record between the Aveiro and Setubal parallels (Western portuguese margin)|
|Authors: ||Cunha, P. P.|
Barbosa, B. P.
Pena dos Reis, R.
Mondego and Lower Tagus basins
|Issue Date: ||25-Mar-2010|
|Abstract: ||Onshore, the Piacenzianof the Mondego and Lower Tagus Tertiary basins comprises siliciclastic sediments deposited in shallow
marine to continental environments. The outcrops of the deposits are relatively widespread in the Aveiro and Seuibal region. A
lithostratigraphic synthesis based on the correlation of geological sections, is presented for the two basins. In general, the Piacenzian
sediments display a regressive sucession. The Late Tortonian-Zanclean (?) confined drainage pattern changed at the beginning of
Piazencian, to fluvial systems draining to the Atlantic, and capturing the drainage of the inner parts of the Hesperic Meseta.
The Piacenzian sedimentary sequence post-dates one of the uprising phases during Neogene compression, recorded by a strong
regional unconformity. Some local active faulting - as in Lousa, Rio Maior and Senibal- Pinhal Novo - allowed the local thickening
of the sedimentary record. Later compressive tectonism continues to generate reverse faulting and diapiric reactivation, affecting those
sediments. Currently, the Piacenzian deposits culminates the marginal piedmonts, widely eroded by the Quaternary fluvial dissection.|
|Appears in Collections:||FCT: DCT - Ciências da Terra|
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