Metamorphic patterns in Zambia and their bearing on problems of Zambian tectonic history

Metamorphic mineral assemblages determined in thin-sections have been used to compile metamorphic maps showing the distribution of metamorphic facies and minerals in Zambia. These maps lead to the recognition of two non-parallel metamorphic belts. The Lufilian Belt curves along the southern margin of the Lufilian (structural) Arc, and the Luangwa—Kariba Belt covers the entire eastern and south-eastern borders of the country. Stratigraphic and mineralogical relationships, and radiometric data, indicate that the two belts are contemporaneous and their present major features are the result of a single tectonothermal episode which ended c. 500 m.y. ago. In particular, the Irumide fold belt is not recognisable as a metamorphic entity.     

Characterizing uncertainties for quantifying bathymetry change between time-separated multibeam echo-sounder surveys

Changes of bathymetry derived from multibeam sonars are useful for quantifying the effects of many sedimentary, tectonic and volcanic processes, but depth changes also require an assessment of their uncertainty. Here, we outline and illustrate a simple technique that aims both to quantify uncertainties and to help reveal the spatial character of errors. An area of immobile seafloor is mapped in each survey, providing a common ‘benchmark’. Each survey dataset over the benchmark is filtered with a simple moving-averaging window and depth differences between the two surveys are collated to derive a difference histogram. The procedure is repeated using different length-scales of filtering. By plotting the variability of the differences versus the length-scale of the filter, the different effects of spatially uncorrelated and correlated noise can be deduced. The former causes variability to decrease systematically as predicted by the Central Limit Theorem, whereas the remaining variability not predicted by the Central Limit Theorem then represents the effect of spatially correlated noise. Calculations made separately for different beams can reveal whether problems are due to heave, roll, etc., which affect inner and outer beams differently. We show how the results can be applied to create a map of uncertainties, which can be used to remove insignificant data from the bathymetric change map. We illustrate the technique by characterizing changes in nearshore bed morphology over one annual cycle using data from a subtidal bay, bedrock headland and a banner sand bank in the Bristol Channel UK.     

Early Ordovician terne-linkages between oceanic and continental ternes in the central Scandinavian Caledonides

The presence of a first-order unconformity in the central part of the Scandinavian Caledonides, linking together early Ordovician/late Cambrian outboard oceanic ternes and the continental margin of Baltic, is of considerable importance for interpreting the geodynamic framework of the orogen. This and other criteria for terne linkage are described, together with implications for the regional tectonostratigraphic development in this segment of the Caledonides.     

The obscured QSO 1SAX J1218.9+2958

We present results from XMM–Newton observations of the obscured quasi-stellar object 1SAX J1218.9+2958. We find that the previously reported optical and soft X-ray counterpart positions are incorrect. However, we confirm the spectroscopic redshift of 0.176. The optical counterpart has a K magnitude of 13.5 and an R – K colour of 5.0 and is therefore a bright extremely red object. The X-ray spectrum is well described by a power law  (Γ= 2.0 ± 0.2)  absorbed by an intrinsic neutral column density of  8.2^+1.1_−0.7× 10²² cm⁻²  . We find that any scattered emission contributes at most 0.5 per cent to the total X-ray flux. From the optical/near-infrared colour we estimate that the active nucleus must contribute at least 50 per cent of the total flux in the K band and that the ratio of extinction to X-ray absorption is 0.1–0.7 times that expected from a Galactic dust–gas ratio and extinction curve. If 1SAX J1218.9+2958 were 100 times less luminous it would be indistinguishable from the population responsible for most of the 2–10 keV X-ray background. This has important implications for the optical/infrared properties of faint absorbed X-ray sources.