Exact(5)
The Montecchio cave, with passage length development of over 1700 m, is characterised by the presence of several sub-horizontal passages and many medium- and small-scale morphologies indicative of sulphuric acid speleogenesis (SAS).
The failed segment between the distance 40 125 m is characterised by low resistivity thin topsoil and the subsoil (weathered layer) in the depth range 0 11 m and are composed of clayey materials as observed at the geoelectric section.
The failed segment at SW flank between the distance 0 150 m is characterised by relatively high resistivity topsoil in the depth range 0 1.9 m with resistivity varying from 106 to 165 Ωm.
The stable segment of the road pavement at station distance between 80 and 190 m and 230 300 m is characterised by relatively high resistivity (> 147 Ωm, lateritic formation) topsoil in the depth range 0 1.7 m.
The stable segment of the road pavement at the NE flank, between distance 150 300 m is characterised by relatively high resistive topsoil in the depth range 0 6 m with resistivity values greater than 130 Ωm which is composed of sandy clay, clayey sand and laterite observed in the geoelectric section.
Similar(55)
In addition to standard analysis by NMR spectroscopy and mass spectrometry, products 2 t, 3 j, and 3 m were characterised by X-ray crystallography studies.
The last component map (map 4, from 25.6 to 50 ms) was characterised by a voltage inversion as compared to map 3.
The upper interval of 70 350 m of the drillcore is characterised by amphibolites and subordinate metagabbro, whereas below that down to slightly more than 755 m of the drillcore, rocks are mainly represented by granitic to quartz-dioritic mica gneisses and mica gneisses with interlayers of granitic pegmatites.
The tropical lowland rainforest at 300 m.a.s.l. is characterised by species of the Dipterocarp family such as Shorea sp., Dipterocarpus sp., Anisoptera sp., and Hopea sp. among other high quality timber species.
m. domesticus contact zone in Europe is characterised by sharp frequency discontinuities for sex chromosome markers at the centre of wider clines in allozyme frequencies.
In contrast, the Motur Formation is characterised by a thick (∼500 m thick) succession of red mudstone with usually isolated, comparatively thinner (1 15 m thick) sandstone bodies.
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