Add to ORKGThe lateral distribution of predominantly terrestrial kerogen or humics enriched with copper(II) porphyrins (Cu-P) across the Danish marine basin implies that the alleged Cretaceous-Tertiary (KT) boundary deposits in western Denmark (at the Nye Kløv/Dania locations) were probably formed by erosion/emplacement of the boundary clay (Fiskeler) in eastern Denmark by marine currents, as originally proposed by Hulteberg
During the Jurassic - Early Cretaceous, the Danish Central Graben developed as a N-S- to NNW- SSE-tr...
During the Jurassic – Early Cretaceous, the Danish Central Graben developed as a N–S- to NNW– SSE-tr...
Results of detailed mineralogical, chemical, and oxygen isotope analyses of the clay minerals and ze...
Abstract: The lateral distribution of predominantly terrestrial kerogen or humics enriched with copp...
High concentrations (up to 4000 ppm) of copper(rr) porphyrins have been detected in the kerogen of t...
Geochemical analyses of Zn, Pb and rare earth elements (La, Ce, Nd, Sm, Eu, Tb, Yb and Lu) in the ke...
Trace metals in the four discrete layers of the Cretaceous-Tertiary boundary (Fiskeler) at Stevns Kl...
Geochemical analyses of trace metals (Ir, Ni, Co, Cr, Zn, Au and Pb) and rare earth elements (La, Ce...
Geochemical analyses of Zn, Pb and rare earth elements (La, Ce, Nd, Sm, Eu, Tb, Yb and Lu) in the ke...
High levels of copper(II) (Cu2+) were found with the major part ( GT 90%) of the total Cu located in...
The black marl of the Fish Clay at Højerup is mainly made up of biogenic calcite and cheto-Mg-smecti...
Geochemical analyses of trace metals (Ir, Ni and Zn) in the kerogen of the black marl of the Cretace...
The early Miocene was an important period for the development of the eastern North Sea. Tectonism in...
The Danish term ‘moler’ is the name for a special and unique marine deposit of Lower Eocene age foun...
In the light of integrated biostratigraphic and geochemical data, a complete shallow-marine successi...
During the Jurassic - Early Cretaceous, the Danish Central Graben developed as a N-S- to NNW- SSE-tr...
During the Jurassic – Early Cretaceous, the Danish Central Graben developed as a N–S- to NNW– SSE-tr...
Results of detailed mineralogical, chemical, and oxygen isotope analyses of the clay minerals and ze...
Abstract: The lateral distribution of predominantly terrestrial kerogen or humics enriched with copp...
High concentrations (up to 4000 ppm) of copper(rr) porphyrins have been detected in the kerogen of t...
Geochemical analyses of Zn, Pb and rare earth elements (La, Ce, Nd, Sm, Eu, Tb, Yb and Lu) in the ke...
Trace metals in the four discrete layers of the Cretaceous-Tertiary boundary (Fiskeler) at Stevns Kl...
Geochemical analyses of trace metals (Ir, Ni, Co, Cr, Zn, Au and Pb) and rare earth elements (La, Ce...
Geochemical analyses of Zn, Pb and rare earth elements (La, Ce, Nd, Sm, Eu, Tb, Yb and Lu) in the ke...
High levels of copper(II) (Cu2+) were found with the major part ( GT 90%) of the total Cu located in...
The black marl of the Fish Clay at Højerup is mainly made up of biogenic calcite and cheto-Mg-smecti...
Geochemical analyses of trace metals (Ir, Ni and Zn) in the kerogen of the black marl of the Cretace...
The early Miocene was an important period for the development of the eastern North Sea. Tectonism in...
The Danish term ‘moler’ is the name for a special and unique marine deposit of Lower Eocene age foun...
In the light of integrated biostratigraphic and geochemical data, a complete shallow-marine successi...
During the Jurassic - Early Cretaceous, the Danish Central Graben developed as a N-S- to NNW- SSE-tr...
During the Jurassic – Early Cretaceous, the Danish Central Graben developed as a N–S- to NNW– SSE-tr...
Results of detailed mineralogical, chemical, and oxygen isotope analyses of the clay minerals and ze...