Maturity modelling integrated with apatite fission-track dating: Implications for the thermal history of the Mid-Polish Trough (Poland)

Abstract

a b s t r a c tThe Mid-Polish Trough (MPT) is situated in the easternmost part of the Central European Basin System (CEBS) and stretches NW-SE across the Polish Basin. It was characterised by pronounced subsidence and thick sediment accumulation between the Permian and the Late Cretaceous. Late Cretaceous-early Paleogene basin inversion led to the formation of the Mid-Polish Swell (MPS). The study area is located within the Pomeranian segment of the MPT/MPS (NW Poland) and experienced up to 7 km PermianMesozoic subsidence. PetroMod 1-D modelling was performed on several well-sections in order to study Permian to recent burial-uplift evolution. The modelling was calibrated with new vitrinite reflectance (VR r ) data and allowed to constrain the magnitude of uplift and related erosion as well as provided a first overview of the temperature history. The base of the studied Permian-Mesozoic successions attained maximum burial depths of 4800-5400 m before the onset of the inversion, less than in the axial trough area. The thickness of pre-and most probably also syn-inversion Upper Cretaceous deposits is estimated as 300 m. Erosion associated with inversion processes removed between 900 and 1400 m of the Mesozoic sediments, i.e. 1000-1500 m less than in the most inverted central part of the trough. VR r data suggest constant Permian-Mesozoic heat flows corresponding to present-day values (40-45 mW/m 2 ). Apatite fission-track (AFT) ages modelled with the PetroMod module PetroTracks show a good fit with AFT ages directly measured on well samples, and further support the assumption of steady heat flow in the range 40-45 mW/m 2 . Palaeotemperatures appear to have decreased towards the East European Craton margin, which is compatible with the present day distribution of heat flow. Thermal history modelling shows a relatively simple Permian-Mesozoic heat flow pattern in the Pomeranian segment of the MPT. Such a scenario implies that the present-day heat flow distribution has not changed essentially since Mesozoic times.

Reply on RC1

“…The highest frequency of the AFT ages is in the Jurassic and Early Cretaceous (Tab. 3) i.e., they are older than inversion of the German-Polish Basin (e.g., Senglaub et al, 2005;Resak et al, 2010;Łuszczak et al, 2020).…”

Lower Cretaceous source rock evaluation and thermal maturity evolution of the Chagan depression, Inner Mongolia, Northern China

“…Along with the development of petroleum geology theory and the wide application of computing technology, quantitative research on the thermal maturity evolution of source rocks in the geological period is of great significance. Basin simulation method has become an important method in the thermal maturity evolution and spatial distribution characteristics of source rocks in sedimentary basin (Belaid et al, 2010;Berthonneau et al, 2016;El-Shahat et al, 2009;Hakimi and Ahmed, 2016;Hudson and Hanson, 2010;Kosakowski et al, 2013;Pang et al, 2004Pang et al, , 2012Qiu et al, 2010Qiu et al, , 2012Resak et al, 2010;Zhu et al, 2016;Zuo et al, 2011Zuo et al, , 2013aZuo et al, , 2014Zuo et al, , 2015aZuo et al, , 2015bZuo et al, , 2016aZuo et al, , 2016b.…”