Figure 14. Folded and transposed bedding in calc-silicate hornfels. Unit Jcsh in Monarch Lakes basin (36.4510°N, 118.5650°W). Jackknife is 9 cm in length.

Figure 3.  Examples of transposed foliation and lineation resulting from change of tectonic stress system during recrystallization of gneissic rocks and granites. A , Cartoon of “S/C” structure in a foliated rock after Evans et al. ( 1997 ). B , Discrete deformational features associated

Figure 3. Eight example feature maps generated by the transposed convolution upsample filters.

Fig. 3. Continued . ( g ) SE Betics, near La Parra. High strain D 3 folding and transposed layering of pelitic/psammitic layering (S 0 /S 2 ). Note steeply dipping S 3 –L 3 fabric. ( h ) Same location as (g). Asymmetrical quartz lenses consistent with top-to-the-north shear (D 3 ). ( i ) SE

Figure 23 Core box photographs shows that two pieces of core were transposed and mislabeled. This error originated soon after the core was acquired, either at the wellsite or when the full-diameter core was cut into 3 ft. lengths, boxed, and labeled. This error compromises the entire core dataset

Figure 4. (A) Lithostratigraphy transposed into S T ; metapelitic schist (gray) interlayered with marbles (whitish). Picture taken some 500 m south of Joss Mountain top, looking WNW-ward. (B) Impure marble layer recording an F 2 intrafolial fold within S T . Picture taken on the eastern slope

Figure 3 ( A ) Amphibolite dykes transposed into parallelism with the fabric in the Abbabis Complex. ( B ) Amphibolite dyke (left of photograph) cross-cutting the fabric in Abbabis Complex gneisses. ( C ) Photomicrograph of amphibolite LKR021, showing plagioclase (pl), opaques (op – ilmenite

Figure 7. Truncation of metatexite by transposed band of diatexite oriented roughly E-W and steep, parallel to the axial plane. Leucosomes in diatexite are linked continuously with layer-parallel leucosomes in metatexite. The transposed zones have a well-defined, boundary-parallel foliation

Fig. 7 ( a ) Form surface map of the multiply deformed and transposed tectonic horizon corresponding to the contact between the pre-Alpine continental margin of the Adria plate (Sesia-Lanzo Zone) and the Mesozoic calcschists at the border of the Tethyan ocean (Piemonte Zone), E slope of Salvini

Figure 8. Interpreted seismic data of Line 1C is transposed on the mine map. The blue cross-hatched segment of the seismic line indicates a potential washout or old mine works. The red cross-hatched segment is assoiated with the old mine works.

F igure 5. Heat of transposed-temperature drop of samples 1 to 11 vs. mol% of Fe 2 O 3 . The square symbol represents measured values and circle symbol represents corrected values.

Fig. 9. Geraldton area. ( a ) Transposed quartz–feldspar porphyry dyke in the hinge of the Hard Rock anticline. ( b ) F1 overprinted by F2 on north limb of Hard Rock anticline. Coin for scale (21 mm diameter). ( c ) Z F3 fold in polymictic conglomerate. S2 in volcanic clast (arrow

Fig. 10. Williams A Zone area. (A) F 2 -folded and partly transposed sedimentary rocks, about 65 m into the hanging wall (i.e., to the north) from the uppermost ore zone contact, or 45 m north of the structurally upper limit of the Lake Superior shear zone (LSSZ) and about 180 m east of Moose

Fig. 13. Photograph of marble ridge, characterized by near-horizontal transposed bedding, Lake Harbour Group (level 3). Location of field photograph given in Fig.  12 . Height of cliff is 30 m.

Fig. 3. Map of bedding (S0) and S0 transposed parallel to S2 (S2//S0) in the metasedimentary rocks of the Meguma Group in the vicinity of the boundary of the SMB. The Portuguese Cove location is shown as an inset (see Fig.  2 for location). Strike lines from air photo interpretation shown

Fig. 5. Transposed feldspar–quartz–chlorite phyllite (top right) and more siliceous chlorite–muscovite–quartz schist (left and bottom), folded by F 3 in the hinge of the F 3 Grizzly synform. Viewed looking northwest. Tip of pencil is 2.5 cm long.

Figure 16 —Clastic dikes and transposed sandstone in Tongue River Member, southwestern Powder River basin.

340°; S2 was related to the east–west dextral shear. ( d–g ) Folded S1 foliation in zones, showing transposed S1. ( h , i ) Photomicrographs showing S1 is transposed by the dominant S2 fabric.