Add to ORKGABSTRACT. The investigated dykes are located eastern of the Chelopech volcanic complex situated in the Central Srednogorie magmatic zone which host one of the largest Cu-Au deposits in Europe. These rocks are porphyritic with plagioclase and amphibole phenocrysts, and quartz and biotite are rare. These dykes have andesitic, latitic, dacitic and trachydacitic compositions. The trace element distribution is typical for an active continental margin
The epithermal high-sulphidation Cu-Au Chelopech deposit is characterized by a well-developed and we...
Five strata-bound massive sulfide deposits of the Cu-Zn type are located at three different stratigr...
This review compiles geological, mineralogical, and isotopic data from the four largest Cu–Au epithe...
The Chelopech volcano is the host of one of the largest Au-Cu deposits in Europe. The volcano, part ...
The Chelopech deposit is one of the largest European gold deposits and is located 60 km east of Sofi...
The study focuses on a subvolcanic rhyodacite dyke intruding a fine grained biotite granite and para...
The Chelopech volcanic complex is located in the Central Srednogorie magmatic zone and hosts one of ...
Palaeoproterozoic (ca. 1.8 Ga) mafic and ultramafic dykes are widely distributed within thewhole Sar...
International audiencePalaeoproterozoic (ca. 1.8 Ga) mafic and ultramafic dykes are widely distribut...
This publication is a series of datasets that accompany a manuscript on petrology of lamprophyre dyk...
The paper presents new major and trace element and first Sr-Nd isotope data from selected lavas amon...
The Chelopech high-sulphidation Cu-Au deposit is situ-ated about 65 km east of the town of Sofia in ...
We present new geochemical and Nd isotopic data on two Mesoproterozoic Listvyanka (1350 ± 6 Ma)...
The geochemistry and REE of magnesite and host carbonate rocks of two Lower Riphean deposits of the ...
Representative samples covering all petrographic types of the Miocene subvolcanic (dykes and sills) ...
The epithermal high-sulphidation Cu-Au Chelopech deposit is characterized by a well-developed and we...
Five strata-bound massive sulfide deposits of the Cu-Zn type are located at three different stratigr...
This review compiles geological, mineralogical, and isotopic data from the four largest Cu–Au epithe...
The Chelopech volcano is the host of one of the largest Au-Cu deposits in Europe. The volcano, part ...
The Chelopech deposit is one of the largest European gold deposits and is located 60 km east of Sofi...
The study focuses on a subvolcanic rhyodacite dyke intruding a fine grained biotite granite and para...
The Chelopech volcanic complex is located in the Central Srednogorie magmatic zone and hosts one of ...
Palaeoproterozoic (ca. 1.8 Ga) mafic and ultramafic dykes are widely distributed within thewhole Sar...
International audiencePalaeoproterozoic (ca. 1.8 Ga) mafic and ultramafic dykes are widely distribut...
This publication is a series of datasets that accompany a manuscript on petrology of lamprophyre dyk...
The paper presents new major and trace element and first Sr-Nd isotope data from selected lavas amon...
The Chelopech high-sulphidation Cu-Au deposit is situ-ated about 65 km east of the town of Sofia in ...
We present new geochemical and Nd isotopic data on two Mesoproterozoic Listvyanka (1350 ± 6 Ma)...
The geochemistry and REE of magnesite and host carbonate rocks of two Lower Riphean deposits of the ...
Representative samples covering all petrographic types of the Miocene subvolcanic (dykes and sills) ...
The epithermal high-sulphidation Cu-Au Chelopech deposit is characterized by a well-developed and we...
Five strata-bound massive sulfide deposits of the Cu-Zn type are located at three different stratigr...
This review compiles geological, mineralogical, and isotopic data from the four largest Cu–Au epithe...