Details
| Originalsprache | Englisch |
|---|---|
| Publikationsstatus | Veröffentlicht - 2009 |
| Extern publiziert | Ja |
| Veranstaltung | 4th North African/Mediterranean Petroleum and Geosciences Conference and Exhibition, Tunis 2009 - Tunis, Tunesien Dauer: 2 März 2009 → 4 März 2009 |
Konferenz
| Konferenz | 4th North African/Mediterranean Petroleum and Geosciences Conference and Exhibition, Tunis 2009 |
|---|---|
| Land/Gebiet | Tunesien |
| Ort | Tunis |
| Zeitraum | 2 März 2009 → 4 März 2009 |
Abstract
Well data from the Cambrian to Silurian succession of the Illizi Basin, Algeria, were interpreted to derive a depositional model and correlate the wells in a sequence stratigraphic framework. The succession contains thick glacimarine deposits of the Late Ordovician glaciation. The preglacial deposits show a retrogradational stacking pattern of terrestrial and shallow marine deposits. The synglacial succession is dominated by subaqueous fan deposits. Glacimarine depositional sequences were controlled by advance and retreat cycles of the glacier. Two glacial advance and retreat can be correlated across the study area. The postglacial succession was deposited on the shelf, infilling the residual glacial topography.
ASJC Scopus Sachgebiete
- Erdkunde und Planetologie (insg.)
- Geochemie und Petrologie
Ziele für nachhaltige Entwicklung
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2009. Beitrag in 4th North African/Mediterranean Petroleum and Geosciences Conference and Exhibition, Tunis 2009, Tunis, Tunesien.
Publikation: Konferenzbeitrag › Paper › Forschung › Peer-Review
}
TY - CONF
T1 - A sequence stratigraphic model for ordovician glacial deposits, Illizi Basin, Algeria
AU - Lang, J.
AU - Dixon, R. J.
AU - Le Heron, D. P.
AU - Winsemann, J.
PY - 2009
Y1 - 2009
N2 - Well data from the Cambrian to Silurian succession of the Illizi Basin, Algeria, were interpreted to derive a depositional model and correlate the wells in a sequence stratigraphic framework. The succession contains thick glacimarine deposits of the Late Ordovician glaciation. The preglacial deposits show a retrogradational stacking pattern of terrestrial and shallow marine deposits. The synglacial succession is dominated by subaqueous fan deposits. Glacimarine depositional sequences were controlled by advance and retreat cycles of the glacier. Two glacial advance and retreat can be correlated across the study area. The postglacial succession was deposited on the shelf, infilling the residual glacial topography.
AB - Well data from the Cambrian to Silurian succession of the Illizi Basin, Algeria, were interpreted to derive a depositional model and correlate the wells in a sequence stratigraphic framework. The succession contains thick glacimarine deposits of the Late Ordovician glaciation. The preglacial deposits show a retrogradational stacking pattern of terrestrial and shallow marine deposits. The synglacial succession is dominated by subaqueous fan deposits. Glacimarine depositional sequences were controlled by advance and retreat cycles of the glacier. Two glacial advance and retreat can be correlated across the study area. The postglacial succession was deposited on the shelf, infilling the residual glacial topography.
UR - http://www.scopus.com/inward/record.url?scp=84896914102&partnerID=8YFLogxK
M3 - Paper
T2 - 4th North African/Mediterranean Petroleum and Geosciences Conference and Exhibition, Tunis 2009
Y2 - 2 March 2009 through 4 March 2009
ER -