(Laufer, 1991): Errors resulting from sound-alike or look-alike confusion; e.
2010, Fine-grained non-carbonate particles embedded in neritic to pelagic limestones (Lochkovian to Emsian, Prague Synform
, Czech Republic): composition, provenance and links to magnetic susceptibility and gamma-ray logs.
12a), a general indication of the northward dip of the southern limb of the synform
can be ascertained by strong reflections from the scarp slopes facing the sun (south) and less reflection along the dip slopes (see location A on Fig.
Intraplate volcanism in compressive regimes has been recently suggested to be driven by the compression near collisional/subduction plate boundaries that causes lithospheric folding of the foreland region, resulting in a decrease of the pressure beneath the swell of the antiform while the pressure beneath the synform
increases (Shin et al.
Late Aeronian graptolite sedgwickii Event, associated carbon isotope excursion and facies changes in the Prague Synform
Structural analysis will determine the exact nature of the geology, though it is possible that the mineralisation outline defines an overturned isoclinal synform
with both limbs truncated by erosion below shallow surface cover.
Further drilling during 1999 targeted at 150 depth on the southern limb of the Nifty synform
also encountered chalcocite mineralisation.
Slavik gives an interesting study of Silurian conodonts from the Prague Synform
7 km long monocline with a synform
in the lower flexure (Fig.
At an early stage of exploration the main structural feature was thought to be a doubly-plunging synform
with its axis running NE-SW, with the host rock forming the core of the synform