2 edition of Olisthostromes and other delapsional deposits, and their occurrence in the region of Moratalla (Prov. of Murcia, Spain) found in the catalog.
Olisthostromes and other delapsional deposits, and their occurrence in the region of Moratalla (Prov. of Murcia, Spain)
Hoedemaeker, Ph. J.
Published
1973
by Rijksmuseum van Geologie en Mineralogie in Leiden
.
Written in English
Edition Notes
| Statement | [by] Ph. J. Hoedemaeker. |
| Series | Scripta geologica, no. 19, Scripta geologica ;, 19. |
| Classifications | |
|---|---|
| LC Classifications | QE283 .H6 |
| The Physical Object | |
| Pagination | 207 p. |
| Number of Pages | 207 |
| ID Numbers | |
| Open Library | OL5115893M |
| LC Control Number | 74188759 |
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Olisthostromes and other delapsional deposits, and their occurrence in the region of Moratalla (Prov. of Murcia, Spain). Leiden, Rijksmuseum van Geologie en Mineralogie, (OCoLC) Document Type: Book: All Authors / Contributors: Ph J Hoedemaker Olisthostromes and other delapsional deposits, and their occurrence in the region of Moratalla (Prov.
of Murcia, Spain) (Scripta geologica) by Ph. J Hoedemaker | 1 Jan ?k=geology+spain. Online shopping from a great selection at Books Store. Books Advanced Search Amazon Charts Best Sellers & more Top New Releases Deals in Books School Books Textbooks Books Outlet Children's Books Calendars & Diaries Advanced?k=geologica&rh=n Hoedemaeker, P., Olisthostromes and other delapsional deposits, and their occurrence in the region of Moratalla (Province of Murcia, Spain).
Scripta Geologica, Jednorowska, A., Zespoły małych otwornic w warstwach jednostki magurskiej rejonu P. HoedemaekerOlisthostromes and other delapsional deposits, and their occurrence in the region of Moratalla (Province of Murcia, Spain) Scripta Geologica, 19, Leiden (), p. Google Scholar Hoedemaeker PhJ () Olisthostromes and other delapsional deposits, and their occurrence in the region of Moratalla (Prov.
of Murcia, Spain). Scripta Geolog p Google Scholar Hottinger L, Caus E () Meandropsinidae, an ophtalmidid family of late Cretaceous K-strategist foraminifera endemic in the Pyrenean Gulf. Geol. :// Request PDF | Structure and organitation of the Porma mélange: progressive denudation of a submarine nappe toe by gravitational collapse.
| The Porma Mélange is a unit up to 1 km thick Request PDF | On Jan 1,J.L. Alonso and others published Structure and organization of the Porma mélange: progressive denudation of a submarine nappe toe by gravitational collapse. | Find Boulter, C.A. et al. - Provenance and geochemistry of sedimentary components in the Volcano-Sedimentary Complex, Iberian Pyrite Belt: discrimination between the sill–sediment-complex and volcanic-pile models.
- Journal of the Geological Society, Januaryv. p.illustr. Stapled extract, 4to. € 3, Bourcart, J. & G. Zbyszewski - La faune de Cacela en Algarve The Epiligurian deposits can be subdivided into different successions on the basis of the presence of olistostromes. Olistostromes are small bodies interbedded in Epiligurian successions of normal pelagic deposition.
Their dimensions are at most some hundreds of meters in length and to 20 m thick. ://.
