A reappraisal of the Carboniferous macrofloras of the Zonguldak - Amasra Coal Basin, north-western Turkey
The Zonguldak – Amasra Coal Basin in north-western Turkey has Carboniferous terrestrial deposits ranging in age from Arnsbergian to late Asturian or possibly early Cantabrian. They yield macrofloras that allow detailed biostratigraphical correlations with sequences in Europe. These correlations suggest there are substantial gaps in the Zonguldak – Amasra succession, with middle to upper Namurian, upper Langsettian, Duckmantian and lower Asturian strata apparently being missing. This in turn suggests the area was subjected to significant tectonic instability during Pennsylvanian (late Carboniferous) times and that this might have been instrumental in initiating the progressive change in composition and eventual collapse of the coal swamp biome across Variscan Euramerica during Westphalian times.
Coal petrography, mineralogy, elemental compositions and palaeoenvironmental interpretation of Late Carboniferous coal seams in three wells from the Kozlu coalfield (Zonguldak Basin, NW Turkey)
Abstract A number of coal seams of Late Carboniferous age in the coal-bearing Karadon, Kozlu, and Alacaagzi formations have been mined in several deep underground mines in the Zonguldak Basin (NW Turkey). For this study, a total of 154 coal core samples were collected from three research wells that were drilled in the tectonically complex settings of the Kozlu coalfield. All the coal samples were studied by means of coal petrography, mineralogy, and geochemistry. Special attention was given to the compositions and origins of fracture/cleat-filling minerals that were identified by SEM-EDX on polished blocks. The coal seams investigated are of bituminous rank. They are characterized by low total sulphur contents (≤ 1.0%, on dry basis) and high gross calorific values (22.5–40.2 MJ/kg, on dry, ash-free basis), whereas ash yields and volatile matter contents are variable. X-ray powder diffraction data indicate that the mineralogical compositions of the studied coal seams are rather similar, and clay minerals, along with quartz and carbonate minerals, were identified in almost all seams. The statistical evaluations and SEM data show that some elements such as Mg, Ti, Zr, Nb, and Th are generally affiliated with silicate minerals, whereas elements like Cu, Zn, Mo, and Pb are mainly associated with sulphide minerals. The silicate minerals are generally detrital, and the majority of carbonate minerals are of epigenetic origin. The epigenetic carbonate and sulphide minerals suggest that circulated solutions within coal seams were mainly derived from Ca2 +-rich solutions leached from overlying formations such as Cretaceous aged Zonguldak formations and from hydrothermal solutions that likely were derived from andesitic dykes within the basin. The regional tectonic activities during coalification seem to have deformed coal-bearing formations and, therefore, intra-basinal solutions could have penetrated into the studied coal seams. The epigenetic mineralisation also resulted in elemental enrichments and elevated ash yields, total sulphur, and volatile matter contents in some coal seams. Thus, deformation during coalification controlled some coal quality parameters in the studied wells. The coal facies diagrams suggest that palaeomires mostly accumulated under limno-telmatic conditions, whereas a telmatic environment was more common in palaeomires of the Kozlu Formation. Coal petrography suggests that peat-forming vegetation and water tables in palaeomires were changeable during the Late Carboniferous.
High resolution sequence stratigraphy of the late Namurian in the Widmerpool Gulf (East Midlands, UK)
Abstract Analysis of facies stacking patterns and stratal surfaces within late Namurian deltas of the Widmerpool Gulf has revealed 10 high frequency (fourth-order) depositional sequences. Sequence correlation is based on the characteristic ‘marine band’ fauna of their condensed sections. In many instances, sequence boundaries are difficult to recognize unless there is clearly demonstrable lowstand incision. Consequently, it is often difficult to separate late highstand from falling stage progradation with any degree of confidence. Sequence thickness variations and the dominance of particular stratal surfaces and systems tracts were controlled by a longer period (third-order) cycle of relative sea-level rise and fall during the Marsdenian-Yeadonian. Major fluvio-deltaic sand bodies in the Widmerpool Gulf were formed by distributary channel progradation (e.g. Chatsworth Grit) during the late highstand and/or falling stage systems tracts, and by the filling of incised valleys (e.g. Ashover Grit and Rough Rock) following marked sea-level falls. Channel belt and valley fill orientation was initially influenced by differential compaction, but this influence decreased during the late Namurian. The recognition of incised valley fills within the late Namurian has implications for estimating the magnitudes and periodicities of Carboniferous relative sea-level change.