By J. D. Ridge
This quantity offers bibliographic and textural info which provides a true knowing of the forty ore deposits in Western and West vital Europe. each one deposit is brought via a particular bibliography directory an important literature. this can be by means of a close dialogue protecting geological features together with the placement, grade and tonnage of the ore produced including power reserve, the stratigraphy and constitution of the rocks of the district, and the features and age of the ore physique. The publication additionally features a element of maps, pin-pointing crucial mineral deposits in every one quarter, making this paintings a necessary reference resource for all these operating within the fields of ore-deposit geology and exploration
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Extra info for Annotated Bibliographies of Mineral Deposits in Europe. Western and South Central Europe
984 P a g e l , M . , 1 9 8 2 , G r a n i t e s et g i s e m e n t s d ' u r a n i u m du P o r t u g a l , in V e i n - T y p e a n d S i m i l a r U r a n i u m D e p o s i t s in R o c k s Y o u n g e r t h a n P r o t e r o z o i c , in T e c h . C o m m . M e e t . , I n t . A t o m i c E n e r g y Agency, Vienna, p. 323-347 P o r t u g a l F e r r e i r a , M . a n d M a t o s D i a s , J. M . , 1 9 8 2 , U r a n i u m m i n e r a l i z a t i o n and e p i s y e n i t e s , a c a s e s t u d y in P o r t u g a l , in V e i n - T y p e and S i m i l a r U r a n i u m D e p o s i t s in R o c k s Y o u n g e r than P r o t e r o z o i c : T e c h .
They do think that the uranium would have been transported during remobilization as uranyl carbonate and that a drop in the pressure of p C 0 2 in the open vein structures would have resulted in the deposition of uranium as the oxide. Against this idea it can be argued that, as the carbonates at Urgeiriga are definitely later than the pitchblende, the transport of the uranium as an uranyl-carbonate complex may not be sound. From the very real possibility that not enough uranium could have been recovered from the alteration of the wall rock to sericite to have provided all the uranium in the vein pitchblende, it may be necessary to invoke (as has been done) hydrothermal solutions trapped at depth ever since the Hercynian introduction of the granites and released only on the rather drastic tectonic fracturing of Alpine time.
A n d o t h e r s , 1 9 8 3 , G e o c h e m i c a l i n d i c a t o r s of m a s s i v e s u l p h i d e m i n e r a l i z a t i o n in t h e I b e r i a n p y r i t e b e l t and t h e e a s t P o n t i c m e t a l l o t e c t : M i n e r a l D e p . , v. 1 8 , p . 3 8 7 - 3 9 8 ; d i s c . B e r n a r d , A . J. a r d S o l e r , E . , M i n e r a l D e p . , v. 2 0 , p . 66 P l i m e r , I. R. and C a r v a l h o , D . d e , 1 9 8 2 , T h e g e o c h e m i s t r y of h y d r o t h e r m a l a l t e r a t i o n at t h e S a l g a d i n h o c o p p e r d e p o s i t M i n e r a l .
Annotated Bibliographies of Mineral Deposits in Europe. Western and South Central Europe by J. D. Ridge