RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 21, ES1007, doi:10.2205/2020ES000757, 2021

Table 3. Structural geological features of the Vineh Structure and its surroundings according to different authors. Orientations are given as strike (in wind directions)
No. Type of feature Observation in literature Author(s)
fault system of Purkan-Vardij [Hassanpour et al., 2010 and 2014],
V_F1 faults Fault, strikes of NW–SE in this [Rajabi et al., 2012]
area
V_F2 faults fault system of Northern Tehran [Hassanpour et al., 2010 and 2014],
Fault, strikes E–W generally [Rajabi et al., 2012]
brittle fracture system conju-
gated to fault system of Purkan-
V_f1 fractures Vardij Fault (F1), shear zones [Hassanpour et al., 2010 and 2014]
(10–50 m thick), in the middle
of KWCT (Part 1)
V_f2 fractures joint sets along KWCT [Hassanpour et al., 2010]
(Parts 1 and 2)
KWCT intersecting fault sys- [Jalali, 2018],
V_I1 intersections tem of Purkan-Vardij Fault (F1) [Khanlari et al., 2012],
with 70° in the middle of KWCT [Khanlari and Ghaderi-Meybodi,
(Part 1) 2011 and 2013]
V_B1 bedding Syncline of Azgilak [Hassanpour et al., 2010 and 2014]
V_B2 bedding Anticline of Vardij [Hassanpour et al., 2010 and 2014]

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Citation: Faber R., G. Domej (2021), 3D Computer-Assisted Geological Mapping: Testing WinGeol's FaultTrace for semi-automatic structural geological assessment, Russ. J. Earth Sci., 21, ES1007, doi:10.2205/2020ES000757.
 

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