Please use this identifier to cite or link to this item:
http://hdl.handle.net/2445/34162
Full metadata record
DC Field | Value | Language |
---|---|---|
dc.contributor.author | Cabrera, Lluís | - |
dc.contributor.author | Hagemann, H.W. | - |
dc.contributor.author | Pickel, Walter | - |
dc.contributor.author | Sáez, Alberto | - |
dc.date.accessioned | 2013-03-08T18:26:19Z | - |
dc.date.available | 2013-03-08T18:26:19Z | - |
dc.date.issued | 1995 | - |
dc.identifier.issn | 0166-5162 | - |
dc.identifier.uri | http://hdl.handle.net/2445/34162 | - |
dc.description.abstract | Lignite deposits in the Cenozoic As Pontes strike-slip basin (northwestern Spain)were formed as a function of specific paleoclimatic conditions and tectonic evolution of the basin. | - |
dc.format.extent | 26 p. | - |
dc.format.mimetype | application/pdf | - |
dc.language.iso | eng | - |
dc.publisher | Elsevier B.V. | - |
dc.relation.ispartof | International Journal of Coal Geology, 1995, vol. 27, num. 2-4, p. 201-226 | - |
dc.rights | (c) Elsevier B.V., 1995 | - |
dc.source | Articles publicats en revistes (Dinàmica de la Terra i l'Oceà) | - |
dc.subject.classification | Jaciments minerals | - |
dc.subject.classification | Cenozoic | - |
dc.subject.classification | Espanya | - |
dc.subject.other | Mineral deposits | - |
dc.subject.other | Cenozoic | - |
dc.subject.other | Spain | - |
dc.title | The coal bearing Cenozoic As Pontes Basin (NW Spain): Geological influence on its coal's characteristics | - |
dc.type | info:eu-repo/semantics/article | - |
dc.type | info:eu-repo/semantics/acceptedVersion | - |
dc.identifier.idgrec | 082593 | - |
dc.date.updated | 2013-03-08T18:26:19Z | - |
dc.rights.accessRights | info:eu-repo/semantics/openAccess | - |
Appears in Collections: | Articles publicats en revistes (Dinàmica de la Terra i l'Oceà) |
Files in This Item:
File | Description | Size | Format | |
---|---|---|---|---|
082593.pdf | 2.07 MB | Adobe PDF | View/Open |
Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.