García del Cura, M. Ángeles and Dabrio, Cristino J. and Ordóñez Delgado, Salvador (1996) Mineral resources of the Tertiary deposits of Spain. In Tertiary basins of Spain : the stratigraphic record of crustal kinematics / edited by Peter F. Friend and Cristino J. Dabrio. World and regional geology series . Cambridge University Press, Cambridge ; New York, pp. 26-40. ISBN 0521461715
Spain is the most self-sufficient country for minerals in the
EsU. A major proportion of these Spanish mineral resources has
been oblained from Tertiary material-. The main material
exploited in Tertiary basins have been: brown coal and lignites, potassium salts, sodium salts (sulphates and chlorides), diátomite,
sepiolite and other absorbent days, bentonites, celestine. pumíce and also dimension (building) stones and ceramícs, portland
cement and plaster raw materials.
Pb-Zn-Ag and gold alunite volcanogenic ores, related to Neogene
volcanism, besides Au-placers have been mined from Roman
times, Minor Cu and Mn occurrences are also reviewed.
The brown coal mines of Galician basins have provided all the
sígnificant productíon of Spain: more than 17 Mt. Low-quaility
Oligocene lignites in the eastern part of the Ebro Basin and Balearic
Islands are less important from tbe economic point of view. Other
occurrences are in the Guinzo de Limia. Guadix Baza. Granada
(Arenas del Rey) and Alcoy basins.
The Spanish Tertiary basins (continental and marine, (Oligocene-Miocene) are filled by thick evaporites in which are obtained
potassium salts and sodium salts (sulphates and chlorides). The
Montevives celestine mine is located in the evaporitic unit of the
Granada basin (Miocene), and provides all of the Spanish celestine
production. Spain is the world's third largest producer of celestine.
The Madríd basin and the minor Calatayud basín supply the
whole of Spanish sepiolitic production. The most important Spanish
attapulgite production is obtained from the El Cuervo mine (Sevilla
and Cádiz provinces). The genesis of the Cabo de Gata bentonite
deposits is thought to be by hydrothermal alteration and halmyrolsis
of Neogene volcanic roch. The Madrid basin bentonites and
'pink days' have been interpreted as an early diagenetic. even
edaphic Mg-rich, attapulgitization of illite clays. The most important
areas of ceramic c1ay production in Spain are localed in the
Guadalquivir basin (Bailen area) and the Madrid basin, (La Sagra
Alcalá de Henares).
The continental Neogene basin ofthe Hellin area supplies 90 % of Spanish diamote production.
|Item Type:||Book Section|
|Uncontrolled Keywords:||Spanish, Tertiary basins, Diatomite, Sepiolite, Bentonite, Celestine|
|Subjects:||Sciences > Geology > Stratigraphic geology|
Sciences > Geology > Mineralogy
|Deposited On:||24 Jun 2010 09:35|
|Last Modified:||24 Jun 2010 09:55|
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