Abstract The Neo-Tethys Ocean was an eastward-ga** triangular oceanic embayment
between Laurasia to the north and Gondwana to the south. The Neo-Tethys Ocean was …

Cenozoic strike-slip faults in Indochina were initially interpreted as related to SE expulsion of
rigid blocks of continental crust between narrow, high-displacement strike-slip faults away …

Chalcidoidea are mostly parasitoid wasps that include as many as 500 000 estimated
species. Capturing phylogenetic signal from such a massive radiation can be daunting …

Abstract The India-Asia collision is an outstanding smoking gun in the study of continental
collision dynamics. How and when the continental collision occurred remains a long …

The formation of a global network of plate boundaries surrounding a mosaic of lithospheric
fragments was a key step in the emergence of Earth's plate tectonics. So far, propositions for …

We report paleomagnetic data showing that an intraoceanic Trans-Tethyan subduction zone
existed south of the Eurasian continent and north of the Indian subcontinent until at least …

The enigmatic geodynamic processes involved in the India-Asia collision shape our
understanding of uplift and deformation of the Tibetan Plateau and the subsequent changes …

The Asian monsoons are triggered by complex interactions between the atmosphere, Asian
and African orography, and the surrounding oceans, resulting in highly seasonal climate …

Based on the marine magnetic anomalies identified in the Argo Abyssal Plain offshore
northwestern Australia, the conceptual continent of Argoland must have rifted off in the Late …

Abstract Knowledge of the size of Greater India is critical to deciphering the geodynamic
processes of the India-Asia collision, as the size of this landmass primarily determines the …