The "Kupferschiefer and Other Sediment-Hosted Deposits in Central Europe" field trip (22 May-1 June 1986), which focussed upon the stratiform copper shale (Kupferschiefer) deposits of West Germany and Poland, was a major success. Trip leaders effectively communicated the stratigraphy associated with these deposits, the sulphide zonation, and the controls of mineralization (particularly location with respect to hematitic alteration zones — "Rote Fäule" — and to paleotopography). Replacement textures by oxides and copper sulphides and cross-cutting relationships of ore zones with respect to lithologies indicate diagenetic to epigenetic emplacement of ore. While many crucial questions have been answered, several remain
Sediment-hosted stratiform copper deposits comprise disseminated to veinlet Cu and Cu-Fe sulfides in...
In this study, two mineralized horizons in the Nussir copper deposit were compared. The horizons wer...
Themost significant copper reserves in Poland are confined to sediment-hosted stratiform Kupferschie...
In the western part of the Lubin-Sieroszowice mining district, processes of secondary oxidation of t...
Extensive and rich Cu-Ag sulfide mineralization occurs in Poland across the contact between the Uppe...
New Re–Os age determinations on mineralized material from the Polish Kupferschiefer elucidate the ti...
International audienceMetallogenic provinces in Europe range in age from the Archaean to the Neogene...
Main U minerals in the Lubin and Polkowice mines in decreasing order of abundance are: uraninite, br...
This study deals with the spatial distribution and the PAAS-normalized patterns of rare earth elemen...
Minerals of the Cu-Fe-S system from the Lubin and Rudna mines in the Polish Kupferschiefer display t...
The Spessart district (SW Germany), located at the southwestern margin of the Permian Kupferschiefer...
The Nördlinger Ries is a circular, flat depression of 22-24 km diameter separating the Jurassic lim...
The Konrad mine is the only North German mine that is located in the Upper Jurassic. Lithologically,...
The Western Syncline hosts reduced-facies, or Kupferschiefer-type, sedimentary rock-hosted stratifor...
In this paper we review a number of the major basin-hosted ore deposits in Europe and argue that mos...
Sediment-hosted stratiform copper deposits comprise disseminated to veinlet Cu and Cu-Fe sulfides in...
In this study, two mineralized horizons in the Nussir copper deposit were compared. The horizons wer...
Themost significant copper reserves in Poland are confined to sediment-hosted stratiform Kupferschie...
In the western part of the Lubin-Sieroszowice mining district, processes of secondary oxidation of t...
Extensive and rich Cu-Ag sulfide mineralization occurs in Poland across the contact between the Uppe...
New Re–Os age determinations on mineralized material from the Polish Kupferschiefer elucidate the ti...
International audienceMetallogenic provinces in Europe range in age from the Archaean to the Neogene...
Main U minerals in the Lubin and Polkowice mines in decreasing order of abundance are: uraninite, br...
This study deals with the spatial distribution and the PAAS-normalized patterns of rare earth elemen...
Minerals of the Cu-Fe-S system from the Lubin and Rudna mines in the Polish Kupferschiefer display t...
The Spessart district (SW Germany), located at the southwestern margin of the Permian Kupferschiefer...
The Nördlinger Ries is a circular, flat depression of 22-24 km diameter separating the Jurassic lim...
The Konrad mine is the only North German mine that is located in the Upper Jurassic. Lithologically,...
The Western Syncline hosts reduced-facies, or Kupferschiefer-type, sedimentary rock-hosted stratifor...
In this paper we review a number of the major basin-hosted ore deposits in Europe and argue that mos...
Sediment-hosted stratiform copper deposits comprise disseminated to veinlet Cu and Cu-Fe sulfides in...
In this study, two mineralized horizons in the Nussir copper deposit were compared. The horizons wer...
Themost significant copper reserves in Poland are confined to sediment-hosted stratiform Kupferschie...