Late to post-Variscan molassic basins of Late Pennsylvanian-Permian age are exposed in
Sardinia (Italy). Here, the compositional and stratigraphic evolution of the Mulargia …

Late Paleozoic tectonic links between Luliang Uplift and the adjacent West Junggar terrane
remain poorly understood, despite their significant implications for the tectonic …

Abstract The Greater Caucasus (GC) fold-and-thrust belt lies on the southern deformed edge
of the Scythian Platform (SP) and results from the Cenozoic structural inversion of a deep …

The geodynamic setting along the SW Gondwana margin during its early breakup (Triassic)
remains poorly understood. Recent models calling for an uninterrupted subduction since …

A tectono-stratigraphic and paleoenvironmental comparison between Sardinia and the
coeval surrounding chains allowed to identify and characterize several Alpine-age tectonic …

Differing interpretations of geophysical and geologic data have led to debate regarding
continent-scale plate configuration, subduction polarity, and timing of collisional events on …

The Junggar Basin in northwest China is located in the southern part of Central Asian
Orogenic Belt (CAOB). The tectonic mechanisms controlling sedimentary fill through space …

Detrital zircon geochronology of Neoproterozoic to Devonian sedimentary rocks from the
Georgina and Amadeus basins has been used to track changes in provenance that reflect …

The geological evolution of Central Asia commenced with the evolution of a complex
Precambrian–Palaeozoic orogen. Cimmerian blocks were then accreted to the southern …

The formation and evolution of an intracontinental basin triggered via the subduction or
collision of plates at continental margins can record intracontinental tectonic processes. As a …