This paper presents depth maps for eight key horizons and seven thickness maps covering
the onshore and offshore areas for the Late Permian to recent sedimentary section of the …

The Proterozoic basement of Suriname consists of a greenstone–tonalite–trondhjemite–granodiorite
belt in the northeast of the country, two high-grade belts in the northwest and …

In this paper, we discuss the response of a sedimentary basin to compressional reactivation
of extensional faults in distinct pulses. The inversion of the Broad Fourteens Basin in the …

The ‘Late Jurasic’ stratigraphy of the Dutch Central North Sea Graben is revised. The sediments,
ranging in age from Callovian to Ryazanian, are grouped in two lithological units: the …

Time-stratigraphic interpretations of Late Pliocene to Early Pleistocene sediments from
onshore locations and from marginal marine settings of the North Sea Basin often refer to the …

The sediments of the Upper Cretaceous to lower Palaeogene Chalk Group were deposited
through a wide range of depositional processes. Chalk was originally formed by settlement of …

Within the Cenozoic sedimentary section of the Roer Valley Graben ten seismostratigraphic
units have been identified. They are closely related to the lithological framework which …

The Pleistocene Coropina Formation largely constitutes the Old Coastal Plain of Suriname.
It is exposed fully only in open-pit bauxite mines in the central coastal plain as part of the …

The Broad Fourteens Basin is a NW-SE trending Mesozoic structural element that was
affected by inversion movements during the Late Cretaceous (Subhercynian Phase) and Early …

Geochemical studies on Upper Carboniferous marine bands showed that marked enrichment
in redox-sensitive trace elements (uranium (U), vanadium (V), molybdenum (Mo)) mostly …