Author(s):
Boski, T. 
; Wilamowski, A. ; Moura, Delminda ; Veiga-Pires, C.
Date: 2004
Persistent ID: http://hdl.handle.net/10400.1/2812
Origin: Sapientia - Universidade do Algarve
Document details
The material sources and processes during the infilling of estuaries in Algarve...
Description
The actual estuary that occupies the Boina-Arade paleovalley accommodated the Holocene sedimentary sequence whose thickness does not exceed 35 m in the deepest zones, as registered from geotechnical borehole data. We present here the results of partial analyses of two continuous cores which cross the Holocene sequence until the Pre-Quaternary substratum. In the P5 core (Boina river), the sedimentary column, which spans 20 m accumulated during ca 8500 years.
The actual estuary that occupies the Boina-Arade paleovalley accommodated the Holocene sedimentary sequence whose thickness does not exceed 35 m in the deepest zones, as registered from geotechnical borehole data. We present here the results of partial analyses of two continuous cores which cross the Holocene sequence until the Pre-Quaternary substratum. In the P5 core (Boina river), the sedimentary column, which spans 20 m accumulated during ca 8500 years.
Document Type
Conference Object
Language English
Language English
| Financiadores do RCAAP | |||||||
|
|
|
|
|
|
||