Maurizio Gaetani

TL;DR: The geologic evolution of northern India is best recorded in the stratigraphic succession of the Zanskar Range (northwestern Himalaya), which represents the most complete transect through this ancient continental margin this article.

TL;DR: In this paper, the authors use radiometrically dated Early Permian volcanic rocks from parts of Adria that are tectonically coherent with Africa (Gondwana), integrated with published coeval data from Gondwana and Laurasia, again only from igneous rocks, fully support a Pangea ‘B’ configuration in the early permian.

TL;DR: In this article, a robust agreement of palaeomagnetic poles of Iran and West Gondwana is observed for the Late Ordovician-early Carboniferous, indicating that Iran was part of the parent Gondwanan margin during that time.

TL;DR: In this article, the authors reconstruct the oceanic circulation pattern of the Tethys Ocean 300 m.y. ago by placing Late Carboniferous-Early Permian climate-sensitive biotic associations from Gondwana and Laurasia on a Pangea paleogeography constrained by selected paleomagnetic data.

TL;DR: In this paper, the Latemar buildup is used to illustrate the main character of a Lower Ladinian buildup on the slopes of the Southern Alps of Italy, with additional data for the slope taken from Mt. Coldai (Civetta) and Sass da Putia.