Thick and thin quartz veins Stock Photos and Images
(2)See thick and thin quartz veins stock video clipsThick and thin quartz veins Stock Photos and Images
Multiple Quartz Veins in Rock #3 Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/multiple-quartz-veins-in-rock-3-image417601991.htmlRF2F7BBGR–Multiple Quartz Veins in Rock #3
Bulletin of the Geological Society of America . y^. Figure 4.—Boudinage, Bastogne, BelgiumTraced from photograph used In figure 8. Transverse lines are quartz veins. bands of quartzite, which arched both upward and downward into theless resistant ^^hyllites. The natural conclusion is that after compressionthe quartzite yielded to tension, giving rise to cracks which were dis-tributed equally throughout. The yielding to tension was more closelyspaced in the thin beds than in the thick beds. The actual openings appear to have been wider near the axes of thebeds than near the edges. The edges of Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/bulletin-of-the-geological-society-of-america-y-figure-4boudinage-bastogne-belgiumtraced-from-photograph-used-in-figure-8-transverse-lines-are-quartz-veins-bands-of-quartzite-which-arched-both-upward-and-downward-into-theless-resistant-hyllites-the-natural-conclusion-is-that-after-compressionthe-quartzite-yielded-to-tension-giving-rise-to-cracks-which-were-dis-tributed-equally-throughout-the-yielding-to-tension-was-more-closelyspaced-in-the-thin-beds-than-in-the-thick-beds-the-actual-openings-appear-to-have-been-wider-near-the-axes-of-thebeds-than-near-the-edges-the-edges-of-image339468830.htmlRM2AM83XP–Bulletin of the Geological Society of America . y^. Figure 4.—Boudinage, Bastogne, BelgiumTraced from photograph used In figure 8. Transverse lines are quartz veins. bands of quartzite, which arched both upward and downward into theless resistant ^^hyllites. The natural conclusion is that after compressionthe quartzite yielded to tension, giving rise to cracks which were dis-tributed equally throughout. The yielding to tension was more closelyspaced in the thin beds than in the thick beds. The actual openings appear to have been wider near the axes of thebeds than near the edges. The edges of
