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Two different fracture systems, separated at a depth of 3270 m, were identified.
Objects as small as 30 m × 30 m were identified on the aerial photographs and were classified.
All watersheds with a maximum elevation ≥ 1,800 m were identified as regions where the neighbourhood should be adjusted.
The punctual sample RMSE was 8.6 m, conforming to previous estimates of SRTM error, but many errors in excess of 50 m were identified.
The coefficient of thermal expansion of 22.5 × 10−6 K−1 and thermal conductivity of 190 W/(K m) were identified, in agreement with literature.
Twelve seismites thicker than 0.2 m were identified from the Tokha Formation, the major part of which was deposited at about 20 – 17 ka (calibrated 14C ages).
Similar(42)
Rhododendron (R. ponticu m) was identified at 25% of the sites listed in the National Survey of Native Woodlands (Perrin et al, 2008).
The daily trough minimum position (T M) was identified from each latitudinal TEC profile between 45° and 70° N (see Fig. 2b).
For instance, an SIPE of 8.6 m was identified in the cycle slip analysis, resulting in erroneous cycle slip fix outcome (Liu 2011).
The possible distance between trawl doors, 22 m, 80 m and 125 m was identified by reference to published literature [39] and personal communication (Dick Ferro, Fisheries Research Services, Aberdeen, UK).
In these approaches, certain columns in the alignment M are identified as SNP columns.
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