Contrasting intensity of aragonite dissolution and dolomite cementation in glacial versus interglacial intervals of a subtropical carbonate succession
- Location
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Deutsche Nationalbibliothek Frankfurt am Main
- Extent
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Online-Ressource
- Language
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Englisch
- Bibliographic citation
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In: Sedimentology : journal of the International Association of Sedimentologists(69), H. 5, S.2131-2150 - ISSN 0037-0746
In: Wiley, Oxford [u.a.]
- Event
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Veröffentlichung
- (where)
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Kiel
- (who)
-
Universitätsbibliothek Kiel
- (when)
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2022
- Creator
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Reuning, Lars
Deik, Hanaa
Petrick, Benjamin
Auer, Gerald
Takayanagi, Hideko
Iryu, Yasufumi
Courtillat, Margot
Bassetti, Maria‐Angela
- Contributor
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Tosca, Nicholas
- URN
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urn:nbn:de:gbv:8:3-2024-00542-8
- Rights
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Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Last update
-
14.08.2025, 10:45 AM CEST
Data provider
This object is provided by:
Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.
Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.
Associated
- Reuning, Lars
- Deik, Hanaa
- Petrick, Benjamin
- Auer, Gerald
- Takayanagi, Hideko
- Iryu, Yasufumi
- Courtillat, Margot
- Bassetti, Maria‐Angela
- Tosca, Nicholas
- Universitätsbibliothek Kiel
Time of origin
- 2022
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Paleoceanographic and climatic teleconnections between the subarctic and subtropical North Atlantic during the last interglacial (MIS 5e)
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Contrasting intensity of aragonite dissolution and dolomitecementation in glacial versus interglacial intervals of asubtropical carbonate succession
5.8 Dolomite
Direct nanoscale observations of the coupled dissolution of calcite and dolomite and the precipitation of gypsum
Beiträge zur Chemie der Dolomite
Einiges über Kalksteine und Dolomite
Paleoceanographic and climatic teleconnections between the subarctic and subtropical North Atlantic during the last interglacial (MIS 5e)
Fibrous dolomite formation at a Miocene methane seep may reflect Neoproterozoic aragonite-dolomite sea conditions
The effect of dolomite amendment on soil organic carbon mineralization is determined by the dolomite size
South Tyrol and Venetian or Dolomite Alps
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