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result is a transformation matrix indicating   Two data sets, (i.e., photos and images   discrepancy in the estimated horizontal plane
         that to align the two point clouds, a scaling   extracted from a video sequence) have been   between the two models, considering the
         factor of 1.0012 is required. The rotations   tested to produce and later register the Photo   orientation of the fault, is 1.1° around the
         around the X, Y, and Z axes are –0.38°,   and Video models, respectively. These models   strike direction and 0.29° around the horizon-
         1.00°, and 0.34° (1.1° around the strike direc-  have been compared together and with the   tal direction perpendicular to the fault’s strike.
         tion and 0.29° around the horizontal direc-  Reflex Model, which represents a benchmark   In other words, the registration of the horizon-
         tion perpendicular to the strike).  build with photos obtained in 2016, although   tal plane is sensitive to the orientation of the
                                             probably minor morphological changes due to   photographs, so that the inclusion of oblique
         DISCUSSION                          weathering can have occurred since then.   to the scene photographs may improve the
          We have described a workflow for gener-  Manual alignment of the Photo and Video   “horizontalization” of ρ.
         ating georeferenced 3D models of geologi-  models shows that discrepancies ranging
         cal  outcrops ranging  in  size  from  tens of   from 0 to 5 mm occur between the surface   CONCLUSION
         meters down to a few centimeters. The   reconstructions. There are notable discrepan-  This paper faces the need encountered by
         required tools are extremely portable. Their   cies between the Video and Reflex models,   many field geologists to efficiently capture
         use in the field is straightforward, with sur-  whereas the Photo and Reflex models are   images of outcrops with ultra-portable tools
         vey acquisition taking a few minutes for our   much more comparable, with surface  dis-  to produce detailed, scaled, and properly ori-
         case study. During the development and   placements ranging between 0 and 2 mm.   ented “pocket” 3D digital representations of
         testing of the procedure, it was notable that   Despite the lower number of input photos, the   rock exposures. Submillimeter point-cloud
         video sequence acquisition can provide a   Photo Model outperforms the Video Model in   resolution is achieved with the suggested
         more coherent scene, assuming that the   terms of accuracy. The major reason for this is   procedure, equaling that of models obtained
         mapped area is relatively continuous. On   the  problematic  reconstruction  of  the  scene   by means of reflex cameras, and proving the
         the other hand, video sequences may gener-  from extremely narrow baseline images   efficiency of the proposed registration proce-
         ate excessive scene overlap, complicating   extracted from the video sequence. Despite   dure for several quantitative applications in
         image matching. Also, the use of video   the video capture having a more straightfor-  geology (e.g., fracture and fault orientation
         frames implies the lack of control on shutter   ward acquisition procedure, it may require a   and associated kinematic indicators, bedding
         speed, aperture, ISO, etc., limiting the use   more  complex  and  time-consuming  user-  attitude and thickness, fault roughness, etc.).
         of video frames mostly to small outcrops.   assisted procedure of image selection and   Furthermore, the proposed method is intui-
         Thus, selectively captured still images gen-  repeated runs of photo alignment.  tive so that it can be applied by all geoscien-
         erally ensure a better result and a shorter   Apart from minor differences in recon-  tists irrespective of background or experi-
         processing time, as long as the acquisition is   struction quality and errors that may arise   ence. In this regard, we hope that this
         correctly carried out. Video models instead   from manual detection of the key points used   workflow will favor the widespread use of
         provide a simpler acquisition scheme, albeit   in the similarity transform, the registration   3D models from smartphones.
         with greater risk of reconstruction artifacts.  procedure of the  two smartphone-generated
          Once the models are built, post-process-  models led to models with consistent orienta-  REFERENCES CITED
         ing registration using the proposed method   tion and scaling characteristics. In detail, we   Allmendinger, R.W., Siron, C.R., and Scott, C.P.,
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                                                                                  gy: American Association of Petroleum Geolo-
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         acquisition strategy include this item as   ment was made of the same object present in   (last accessed 27 Feb. 2021).
         part of their standard equipment. Using a   the two models. Models of the same geologi-  Bemis, S.P., Micklethwaite, S., Turner, D., James,
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                                                                                  and Lakshmikantha, M.R., 2018, Quantitative
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