Annotated Bibliographies of Mineral Deposits in Europe. by J. D. Ridge

By J. D. Ridge

This quantity offers bibliographic and textural details which provides a true knowing of the forty ore deposits in Western and West relevant Europe. every one deposit is brought through a specific bibliography directory crucial literature. this can be by means of a close dialogue overlaying geological features together with the placement, grade and tonnage of the ore produced including capability reserve, the stratigraphy and constitution of the rocks of the district, and the features and age of the ore physique. The booklet additionally encompasses a component of maps, pin-pointing an important mineral deposits in each one zone, making this paintings a worthwhile reference resource for all these operating within the fields of ore-deposit geology and exploration

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1 9 6 0 , T h e o r e c o n t r o l s of s o m e u r a n i u m v e i n d e p o s i t s in P o r t u g a l : J u n t a de E n e r g i a N u c l e a r ( P o r t u g a l ) , T e c h . P a p e r n o . 2 6 , 63 p . , 1 9 8 2 , G e o m o r p h o l o g y and u r a n i u m v e i n d e p o s i t s of t h e B e i r a r e g i o n of 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 t h a n P r o t e r o z o i c : T e c h . Comm. , Int. Atomic Energy Agency, Vienna, p.

G e o l . P o r t . , 1 9 7 1 , J a z i g o de p i r i t e de A l j u s t r e l - E s t u d i o da d i s t r i b u i c a o d o s t e o r e s em S, C u , Z n , Pb e A s n a s m a s s a s p i r i t o s a s : 1° C o n g . H i s p a n o - L u s o - A m e r i c a n o G e o l o g i a E c o n o m i c o , v. 4, p . , 1 9 7 1 - S u a de s c o b e r t a , s i t u a c a o a c t u a l e p o s s i b i 1 i d a d e s f u t u r a s : 1° C o n g . H i s p a n o - L u s o - A m e r i c a n o G e o l o g i a E c o n o m i c a , v.

Rocks on the northeast side of the Beja anticline are of no concern here. The materials that make up the Culm graywackes proper must have been derived from the erosion of Tournaisian (lower Mississippian) of the Beja geanticline, and the depth of erosion must have been quite sizeable, having been great enough to remove the rather thin Devonian beds once prsent in the geanticline.

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