Add to ORKGThe Peniche section (Portugal) is considered as a potential stratotype (GSSP) for the Pliensbachian/Toarcian boundary and it is analysed on the background of the available data on the ammonite successions from other Tethyan and NW European areas
Based on a continuous succession of ammonite and calcareous nannofossil assemblages, the main purpos...
This paper discusses the extinction pattern of the Pliensbachian-Toarcian boundary (PTB) ostracod as...
In the Lusitanian Basin (Central Portugal), the Middle-Upper Liassic series are characterized by an ...
The Peniche section (Portugal) is considered as a potential stratotype (GSSP) for the Pliensbachian/...
The Peniche section (Ponta do Trovão) in Portugal is presented as potential stratotype (GSSP) for th...
The Global Stratotype Section and Point (GSSP) for the base of Toarcian Stage is proposed at the bas...
The Global Stratotype Section and Point (GSSP) for the base of Toarcian Stage, Lower Jurassic, is pl...
ABSTRACT – The Pliensbachian/Toarcian boundary (Lower Jurassic) is well represented in the Lusitania...
The Peniche section in the Lusitanian Basin (western Portugal) provides an exceptional, continuous r...
The Pliensbachian/Toarcian boundary (Lower Jurassic) is well represented in the Lusitanian Basin (Po...
The marl-limestone succession that encompasses the Pliensbachian–Toarcian Stage Boundary (Lower Jura...
The marl-limestone succession that encompasses the Pliensbachian–Toarcian Stage Boundary (Lower Jura...
We present the biostratigraphy (ammonites, brachiopods, foraminifers, and ostracodes), lithostratigr...
The Global Boundary Stratotype Section and Point (GSSP) for the Aalenian Stage, formally defined at ...
Revista electrónica de Ciências da Terra,http://e-terra.geopor.pt,Geociences on-line journal, Vol. 6...
Based on a continuous succession of ammonite and calcareous nannofossil assemblages, the main purpos...
This paper discusses the extinction pattern of the Pliensbachian-Toarcian boundary (PTB) ostracod as...
In the Lusitanian Basin (Central Portugal), the Middle-Upper Liassic series are characterized by an ...
The Peniche section (Portugal) is considered as a potential stratotype (GSSP) for the Pliensbachian/...
The Peniche section (Ponta do Trovão) in Portugal is presented as potential stratotype (GSSP) for th...
The Global Stratotype Section and Point (GSSP) for the base of Toarcian Stage is proposed at the bas...
The Global Stratotype Section and Point (GSSP) for the base of Toarcian Stage, Lower Jurassic, is pl...
ABSTRACT – The Pliensbachian/Toarcian boundary (Lower Jurassic) is well represented in the Lusitania...
The Peniche section in the Lusitanian Basin (western Portugal) provides an exceptional, continuous r...
The Pliensbachian/Toarcian boundary (Lower Jurassic) is well represented in the Lusitanian Basin (Po...
The marl-limestone succession that encompasses the Pliensbachian–Toarcian Stage Boundary (Lower Jura...
The marl-limestone succession that encompasses the Pliensbachian–Toarcian Stage Boundary (Lower Jura...
We present the biostratigraphy (ammonites, brachiopods, foraminifers, and ostracodes), lithostratigr...
The Global Boundary Stratotype Section and Point (GSSP) for the Aalenian Stage, formally defined at ...
Revista electrónica de Ciências da Terra,http://e-terra.geopor.pt,Geociences on-line journal, Vol. 6...
Based on a continuous succession of ammonite and calcareous nannofossil assemblages, the main purpos...
This paper discusses the extinction pattern of the Pliensbachian-Toarcian boundary (PTB) ostracod as...
In the Lusitanian Basin (Central Portugal), the Middle-Upper Liassic series are characterized by an ...