The Sedimentology of chalk
The Sedimentology of Chalk describes processes that caused the rhythmic, vertical variation in grain size, structures and authigenic mineral concentrations. Special attention is given to Late Cretaceous and Early Tertiary, subtropical, shallow marine, fine-grained, detrital bioclastic carbonates of...
Bewaard in:
| Hoofdauteur: | |
|---|---|
| Formaat: | Livre numérique |
| Taal: | Anglais |
| Gepubliceerd in: |
Berlin [etc.] :
Springer-Verlag : Springer e-books
[20..].
Cham : Springer Nature |
| Reeks: | Lecture notes in Earth sciences
54 |
| Onderwerpen: | |
| Online toegang: | Accès sur la plateforme de l'éditeur Accès sur la plateforme Istex Accès Université d'Orléans Accès INSA CVL |
| Opmerking: |
Archives Springer e-books (Licence nationale) Archives Springer e-books (Licence nationale) |
| Autres localisations: | Voir dans le Sudoc |
| Edition sous un autre format: | • The sedimentology of chalk, Hans Zijlstra, Berlin, Springer, 1995, 1 vol. (IX-194 p.), Lecture notes in earth sciences, 978-3-540-58948-8 • The Sedimentology of Chalk, Texte imprimé, 9783662197561 |
Inhoudsopgave:
- The geology of South Limburg in 1859
- Present-day views on chalk
- Early diagenesis of chalk
- Origin and growth of flint nodules
- The genesis of flint nodule layers
- The genesis of tempestite cycles
- The genesis of hardgrounds
- Genesis of the K/T section of stevns klint
- Self-organizing model for wavy bedform genesis.