Global sedimentary hiatuses are well-documented in ancient pelagic sediment, and include
Paleocene, Eocene-Oligocene boundary, and Miocene hiatuses. Less clear is the extent of …

The stratigraphic development of foreland basins has mainly been related to surface loading
in the adjacent orogens, whereas the control of slab loads on these basins has received …

A complex interplay of palaeoclimatic, eustatic and tectonic processes led to fragmentation
and dissipation of the vast Tethys Ocean in Eocene–Oligocene times. The resulting …

Paratethys, the lost sea of central Eurasia, was an anoxic giant during Oligocene–early
Miocene (Maikop Series) times. With a size matching the modern-day Mediterranean Sea …

The timing of tectonic deformation in the Zagros foreland basin provides important
information about the tectonic propagation process driven by the Arabia‐Eurasia …

The northern deformation front of the European Alps, ie the northern limit of Alpine thrusting,
is characterized by structural variability along strike. It can be subdivided into four regions …

The onset, characteristics, and drivers of paleo‐monsoon conditions in East Asia remain a
topic of heated debate. Records from the Eocene suggest pronounced rainfall seasonality …

Abstract After Rock-Eval & TOC screening and heterogeneity evaluation on 91 Palaeogene
source rock samples from a well drilled in the Austrian Molasse Basin, ten shale samples …

Abstract The North Alpine Foreland Basin (NAFB) comprises one of the most complete
sedimentary records of the Oligocene and Miocene, driven by global sea-level fluctuations …

The sedimentary strata from the Late Cretaceous to Early Eocene in the Himalayan foothills
offer detailed insights into land collision processes. Unfortunately, a comprehensive dating …