Zobrazeno 1 - 10
of 26
pro vyhledávání: '"Iliana Boncheva"'
Publikováno v:
Rivista Italiana di Paleontologia e Stratigrafia, Vol 113, Iss 3 (2007)
Asadabad section in Central Iran is one of the most complete sequences so far described across the Carboniferous of Iran. The stratigraphic and biostratigraphic data on the sediments overlying the Devonian carbonate platform give evidence about the d
Externí odkaz:
https://doaj.org/article/a3fe0d598e0e44e3804892534e892f24
Publikováno v:
Rivista Italiana di Paleontologia e Stratigrafia, Vol 110, Iss 2 (2004)
The uppermost layers of the Ayineburnu member of the Büyükada Formation in the Istanbul-Gebze area are represented by Griotte-type pelagic nodular limestones. They yielded conodont elements (Bispathodus stabilis and Siphonodella lobata) that can id
Externí odkaz:
https://doaj.org/article/c745ad32d04b45219d33f45326ae586a
Publikováno v:
Review of the Bulgarian Geological Society. 83:141-144
Paleozoic (Silurian and Devonian) cherts from Western Bulgaria occur in three tectonic units: Svoge, Lyubash-Golo Bardo and Morava. The SiO2 content in these rocks varies from 76.06% to 96.02%. The silica source and depositional settings of the chert
Publikováno v:
Acta Geologica Sinica - English Edition.
Publikováno v:
Palaeobiodiversity and Palaeoenvironments.
Publikováno v:
Review of the Bulgarian Geological Society. 82:99-101
Geochemical studies of different Paleozoic intervals composed of bedded cherts, revealed in the western parts of the Srednogorie and Morava-Rhodope zones are presented: Saltar Fm; the lower and middle part of Katina Fm; the lowest part of Parchar Fm,
Publikováno v:
Review of the Bulgarian Geological Society. 81:121-123
The Late Devonian (372–359 million AD) is a time of prolonged climate instability with catastrophic disturbances to global marine ecosystems at the Frasnian–Famennian (F/F) and Devonian–Carboniferous (D/C) boundaries. Global atmospheric CO2 con
Publikováno v:
Palaeobiodiversity and Palaeoenvironments. 99:477-494
The Middle to Upper Devonian Kuh-e-Bande-Abdol-Hossein section in eastern Central Iran is an overall shallow marine, nearshore to open marine facies setting that contains a highly variable conodont record generally characterised by an Icriodid-Polygn
Publikováno v:
Palaeobiodiversity and Palaeoenvironments. 97:541-552
A bryozoan fauna from the Late Devonian (Frasnian) of the Bahram Formation of the Zefreh section in central Iran contains four species: three trepostomes and one rhabdomesine cryptostome. Two species are new: the trepostome Coeloclemis zefrehensis sp
Autor:
Mehdi Yazdi, Ali Bahrami, Ulrich Jansen, Iliana Boncheva, Peter Königshof, Sarah K. Carmichael, Johnny A. Waters
Publikováno v:
Palaeobiodiversity and Palaeoenvironments. 97:517-540
The Zefreh section in central Iran represents a carbonate ramp succession with a general shallow-marine palaeoenvironment. This section represents most of the Bahram Formation (Givetian to at least Middle falsiovalis Zone) and consists of a very hete