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The Tighardine area in the Western High Atlas Massif is composed of rocks ranging in age from Neoproterozoic to Cenozoic. The area is intensely deformed with a multidirectional diversity of faults and also hosts a polymetallic ore deposit (Tighardine mine) and prospects of significant economic value, some of which are related to fault structures. In order to identify favourable areas of mineral deposition, structural and mineralogical mapping using satellite images was conducted in this region. For this purpose, various remote sensing approaches were employed on images from Landsat 8 OLI, Sentinel 2 and ASTER sensors. The process started with lineament extraction methods so as to identify faults manually from satellite images. Principal component analysis (PCA) and the optimal indexing factor (OIF) were used to achieve good discrimination of lithological units. Additionally, several band ratios were applied to ASTER, Landsat 8 OLI and Sentinel 2, in order to derive multiple maps corresponding to hydrothermal alteration zones. Analysis of the results from the obtained maps and their overlay with field data has allowed us to: (i) identify three main structural orientations. The most frequent and longest is the NE–SW direction, which coincides with the principal mineralised horizon of the Tighardine deposit. Results suggest an extension of this horizon towards the south-west at the Ait Zitoune and towards the west in the Ait Hsayn region. Two new fault set has been identified by remote sensing: NW-SE fracture, generally of Mesozoic-Cenozoic age, and an E-W fractures trend, particularly developed in the Neoproterozoic basement and considered of Ediacaran age; (ii) highlighting two potential mineralisation zones: in the Ediacaran basement, revealing alterations of silica, dolomite, clay minerals, iron oxide and alunite-kaolinite-pyrophyllite, hosting the main mineralisation axis (Tighardine mine); in the northern part corresponding to the overthrust zones of Cambrian onto Cenozoic formations.

1952 in Starachowice.He also attended primary and secondary school there.Then, in the years 1971-1976, he studied at the University of Warsaw, specializing in Quaternary geology.He completed his studies with a M.Sc.thesis entitled "Quaternary of the Suchedniw region (northern margin of the Holy Cross Mountains)", which he wrote under the supervision of prof.L. Lindner.In years 1976-2005, he worked at the University of Silesia.During this time, in 1987, he first defended his Ph.D. thesis entitled "The sedimentary environment of proglacial deposits on the example of selected outcrops of the Suwaki Lake District, the Sieradz Basin and the Silesian Upland".It was prepared under the supervision of prof.A.K. Teisseyre.Then, in 1997, based on two monographs ("End moraines of NE Poland -sediments and depositional processes", "Outwash plains of NE Poland -sediments and depositional processes") and other scientific achievements, Tomasz Zieliski received a habilitation degree.

In the northern part of the Marrakech High Atlas (MHA), along the southern Variscan segment of the Western Meseta, a Variscan granitic intrusion crops out, intruding metasediments and meta-volcanosedimentary rocks of Early Cambrian to Ordovician age. A new whole-rock Rb-Sr isochron age of 268 ± 9 Ma for the granite, combined with a previously published whole-rock Rb-Sr radiometric dating (271 ± 3 Ma), reveals a post-kinematic (tectonic) character with regard to the main Variscan deformational event, belonging within the tectonic context of the Moroccan Variscan orogenic belt. Geochemically, the Azegour intrusion is metaluminous to peraluminous and exhibits a calc-alkaline affinity with a ferruginous composition. The massif shows an extremely differentiated character (SiO2 = 77.53–78.14 per cent), K2O and high total alkali contents, FeOt/(FeOt + MgO) and Ga/Al ratios, which have typical characteristics of an A-type granite. In addition, the granite contains high concentrations of LREE (LaN/SmN= 7.9–13.67) relative to HREE (LaN/YbN= 4.81–11.61) and a well-defined Eu negative anomaly (Eu/Eu* = 0.44–0.75). The granitic samples exhibit a strong enrichment of the most incompatible elements (RbN/YbN = 69.84–159.98) and a strong depletion of Ba, Sr, Eu, Nb, P and Ti. These characteristics are similar to those of A1-type granites. The absence of mineralogy typical of an S-type granite, combined with its weakly peraluminous character [A/CNK (molar Al2O3/CaO+Na2O+K2O) = 1,013–1,045], suggest that there is little or no significant involvement of supracrustal sources in the petrogenesis of the intrusion studied. Despite the strongly differentiated character of Azegour granitic rocks samples, their multi-element patterns shows many similarities to those of I-type granitoids, which has led to postulate that the parental liquids of A1-type were derived from partial melting of mafic magmas. The representative samples studied show less depleted εNd(t = 270 Ma)values of –0.94 to –4.85 and lower positive to slightly negative εSr(t = 270 Ma) values of –1.45 to 9.32. The isotopic data suggest that the Azegour granite was emplaced 270 myr ago, apparently generated by partial melting of a mafic/intermediate magma source in the lower crust as a result of the underplating of the asthenosphere mantle-derived Oceanic Island Basalt-like magmas. Alternatively, their isotopic signatures also can be attributed to the interaction and/or hybridisation of basaltic liquids derived from the mantle with these lower crust materials. The generated parental magma probably occurred at deep structural levels and involved fractional crystallisation processes by the separation of a mineralogical association composed of plagioclase + potassium feldspar ± biotite ± amphibole ± sphene ± apatite. The whole-rock Rb-Sr age of 268 ± 9 Ma, whole-rock geochemistry and Sr-Nd isotopic compositions of εNd(t = 270 Ma) and εSr(t = 270 Ma), combined with fieldwork data, suggest that the Azegour granite was emplaced.

Review:Pliny and the eruption of Vesuvius, by Pedar W. Foss, 2022. Routledge, 1st edition; 334 pages. Hardback: price £136.00, e-book: price £39.99; ISBN: 978-0415705462.

This study aims to analyse the geosite candidates of the Betong District (Yala Province) in Southern Thailand by means of several methods including inventory, characterisation, classification, assessment and SWOT analysis. Results of the present study are illustrated through seven proposed geosites that become resources for the development of the Betong District, namely Betong Hot Spring, Inthasorn Waterfall, Chaloem Phra Kiat Waterfall, Mount Silipat and Nakor Hot Spring, as well as Piyamit Tunnel and Aiyerweng Skywalk, two human-modified sites which can be used to observe geological and geomorphological features. The present study is expected to promote the conservation and development of these resources as geological heritage of the district.

Abstract From a geological and palaeogeographical point of view, the area of the Adamów Graben in the vicinity of Turek ranks amongst the best known in central Poland, with several opencast mines located here where lignite was exploited for 57 years. These large-surface exposures provide a good opportunity for detailed geological studies of strata of Late Cretaceous to Holocene age. However, the present research focuses mainly on those deposits, forms and structures that have been most thoroughly examined and are best exposed. These are Cretaceous marls and gaizes, Paleogene ‘blue clays’ and the ‘Koźmin Gravels’, Neogene sandstones, as well as the Quaternary glacial ‘Lake Koźmin’, involutions and ‘Koźmin Las’. Some of these, e.g., the ‘Koźmin Gravels’ and ‘Koźmin Las’, are not known from other Polish territories. Furthermore, results obtained by the authors over a period of nearly 30 years also include data on palaeogeographical changes across some Cenozoic intervals, especially during the early Oligocene and late Weichselian.

Abstract Science classes in public schools are usually strictly linked to several subjects and taught by reference to the reading-listening model. Non-formal educational institutions and events such as ‘children universities’ and science fairs (and to some degree also some private schools) implement elements of interdisciplinary teaching of science and learning through experiments and the use of scientific methods. Workshops conducted within non-formal educational structures prove that only is this method engaging and understandable to primary school pupils, it also is possibly much more effective than the traditional learning style for coding information and explaining common misconceptions in teaching evolution, palaeontology and biodiversity. The example of a scenario for science classes presented here (the so-called ‘aquatic problem’, i.e., adaptations of primarily terrestrial animals – amniotes – to the aquatic environment) uses simple props, such as everyday items, to address the problems that teachers in public school face. Thus, it can be implemented independently of school budgets and availability of school equipment.

Abstract Sediment accumulation is a process that is typical of all types of water reservoirs. The rate and pattern of such accumulation are related to processes taking place in catchments that produce the sediments and to those within reservoirs that determine the percentage of the inflowing load that is trapped and where it is deposited. To keep reservoirs in working order requires desilting and managing of such bottom sediments once they are removed. The choice of strategy for sediment management depends on chemical and physical properties which result from both natural and anthropogenic processes. To varying degrees, these sediments may be contaminated with chemical compounds, especially trace metals. Therefore, research is needed in order to assess the quality of sediments, which will allow to opt for the proper management strategy. Based on an analysis of the available literature, the possibility of using sediments from reservoirs has been determined, using quality criteria and in accordance with applicable law and regulations.

Abstract Soft-sediment deformation structures play an important role in interpreting regional tectonics and basin evolution during slumping events. The Satpura Basin is interpreted as pull-apart with a monoclinal northerly palaeoslope throughout its evolution. The basin formed as a result of sinistral strike-slip faulting, induced by the ENE–WSW-trending Son-Narmada South fault in the north and the Tapti North fault in the south. We have analysed the slump folds within the basalmost Talchir Formation and related these to regional tectonics and palaeoslope changes in the Satpura Basin. The glaciofluvial strata of the Talchir Formation, exposed in the southern part of the Satpura Basin, record intricacies of folds created during slumping. Several fold styles can be distinguished, within alternations of competent sandstone and incompetent shale layers, some of which indicate buckling. Upright folds, resulting from pure shear, underwent rotation of their axial planes and fold axes during simple shear-dominated progressive deformation when the slump moved downslope. The soft-sediment deformation structures that we have studied show refolding patterns that closely resemble comparable folds known from lithified rocks. These layers with refolded structures are overlain by unde-formed sediments, which proves that they are the product of a single ongoing slumping process, rather than of successive deformation events. Our analysis of their fold axes and axial planes, together with fold vergences and thrust directions within the slumps, suggests a mean slumping direction towards the southwest. Analyses of slump folds and their relationship with regional tectonics have allowed us to reinterpret basin evolution history. The southwesterly trending palaeoslope of the basin suggest that the slope of the basin was not uniform throughout its evolution. At the opening, the oblique slip fault, which trended NE–SW, generated due to movement along the ENE–WSW basin bounding faults, was more active and triggered slumping event within the Talchir deposits in the basin. With progressive overlapping of the basin-bounding faults, the Satpura Basin gradually tilted towards the north.