The Patagonian Andean foreland system includes several intermountain basins filled with a Miocene non-marine record deposited under syn-tectonic conditions related to the Andean uplift and a regional climate change triggered by a rain shadow effect. Many of those basins, such as the Collón Cura basin in Neuquén Province, Argentina, present a well-preserved fluvial record (i.e. the Limay Chico Member

The recent article of Loreto et al. (2021) reported new stratigraphic and structural data of the Tyrrhenian backarc basin and used them to propose a new model of crustal architecture of the basin including oceanic sectors. However, we want to open a discussion on the inconsistencies between the interpreted tectonic structures, as well as the age of faults and the data observations. In particular, data

Nielsen and Balling (2022) studied the thermo-tectonic history of the eastern North Sea Basin from inversion of temperature, vitrinite reflectance and apatite fission tracks in boreholes, and found no evidence of Neogene exhumation. This contrasts with previous studies that reported the removal of 500–950 m of Cenozoic sediments during Neogene exhumation, partly based on velocity-depth data in the

Corrigendum to “Assessing first-order BQART estimates for ancient source-to-sink mass budget calculations”. Nyberg, B., Helland- Hansen, W., Gawthorpe, R., Tillmans, F., & Sandbakken, P. (2021). Assessing first-order BQART estimates for ancient source-to-sink mass budget calculations. Basin Research, 33, 2435–2452. https://doi.org/10.1111/bre.12563 The legend for Figure 7 was omitted in the originally-published