Late Pleistocene and Holocene coastal behaviour from 33° to 40° South, Argentine Republic
The coastal behaviour from 33° to 40°S, during two late Pleistocene and one Holocene (Postglacial) transgressions is analyzed. The transgressive episodes were developed in five morphostructural sectors of different tectonic character, at least for the pre-late Pleistocene times. The height of the Sa...
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1988
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| Acceso en línea: | https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_07490208_v4_n1_p59_Gonzalez http://hdl.handle.net/20.500.12110/paper_07490208_v4_n1_p59_Gonzalez |
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paper:paper_07490208_v4_n1_p59_Gonzalez |
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paper:paper_07490208_v4_n1_p59_Gonzalez2023-06-08T15:45:22Z Late Pleistocene and Holocene coastal behaviour from 33° to 40° South, Argentine Republic coastal behaviour crustal stability Holocene Late Pleistocene palaeo sea- level palaeo sea- levels Pleistocene (Late) postglacial transgression Sangamon subsidence transgression Argentina Argentina (fish) The coastal behaviour from 33° to 40°S, during two late Pleistocene and one Holocene (Postglacial) transgressions is analyzed. The transgressive episodes were developed in five morphostructural sectors of different tectonic character, at least for the pre-late Pleistocene times. The height of the Sangamon and Holocene deposits found by researches on the Brazilian coast were considered as indicating a relative crustal stability. Accordingly the height of the Sangamon (?), Mid-Wisconsin and Postglacial deposits recognized in the present work are correlated with the Brazilian deposits. -from Authors 1988 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_07490208_v4_n1_p59_Gonzalez http://hdl.handle.net/20.500.12110/paper_07490208_v4_n1_p59_Gonzalez |
| institution |
Universidad de Buenos Aires |
| institution_str |
I-28 |
| repository_str |
R-134 |
| collection |
Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) |
| topic |
coastal behaviour crustal stability Holocene Late Pleistocene palaeo sea- level palaeo sea- levels Pleistocene (Late) postglacial transgression Sangamon subsidence transgression Argentina Argentina (fish) |
| spellingShingle |
coastal behaviour crustal stability Holocene Late Pleistocene palaeo sea- level palaeo sea- levels Pleistocene (Late) postglacial transgression Sangamon subsidence transgression Argentina Argentina (fish) Late Pleistocene and Holocene coastal behaviour from 33° to 40° South, Argentine Republic |
| topic_facet |
coastal behaviour crustal stability Holocene Late Pleistocene palaeo sea- level palaeo sea- levels Pleistocene (Late) postglacial transgression Sangamon subsidence transgression Argentina Argentina (fish) |
| description |
The coastal behaviour from 33° to 40°S, during two late Pleistocene and one Holocene (Postglacial) transgressions is analyzed. The transgressive episodes were developed in five morphostructural sectors of different tectonic character, at least for the pre-late Pleistocene times. The height of the Sangamon and Holocene deposits found by researches on the Brazilian coast were considered as indicating a relative crustal stability. Accordingly the height of the Sangamon (?), Mid-Wisconsin and Postglacial deposits recognized in the present work are correlated with the Brazilian deposits. -from Authors |
| title |
Late Pleistocene and Holocene coastal behaviour from 33° to 40° South, Argentine Republic |
| title_short |
Late Pleistocene and Holocene coastal behaviour from 33° to 40° South, Argentine Republic |
| title_full |
Late Pleistocene and Holocene coastal behaviour from 33° to 40° South, Argentine Republic |
| title_fullStr |
Late Pleistocene and Holocene coastal behaviour from 33° to 40° South, Argentine Republic |
| title_full_unstemmed |
Late Pleistocene and Holocene coastal behaviour from 33° to 40° South, Argentine Republic |
| title_sort |
late pleistocene and holocene coastal behaviour from 33° to 40° south, argentine republic |
| publishDate |
1988 |
| url |
https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_07490208_v4_n1_p59_Gonzalez http://hdl.handle.net/20.500.12110/paper_07490208_v4_n1_p59_Gonzalez |
| _version_ |
1768545604481318912 |