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Copyright
2004-2011 by Roberto Weinberg. All rights reserved. Unlimited
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notice and acknowledgment of the source URL: users.monash.edu.au/~weinberg. I would very much appreciate an email stating how this material will be used: Roberto Weinberg, Monash University, Australia. Thanks, RW. DISCLAIMER. The material on this website has not undergone the scrutiny of Monash University and does not conform to its corporate web design. It is entirely based on a free-spritied, curiosity-driven research effort by the author, and therefore in no way expresses the official position of the University. |
Ptygmatic folds Mylonitic Granite Dykes Graded Bedding Folded Cross-Bedding in High-Grade Rocks
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Leucosomes
Sheared Pegmatite Pseudotachylyte Melt-lubricated thrusts: an evolution |
Mylonitic granite dykes randomly folded, outcrop on Adelaide road, 13 km from Broken Hill. | Mylonitic granite randomly folded, outcrop on Adelaide road, 13 km from Broken Hill. |
Mylonitic granite randomly folded, outcrop on Adelaide road, 13 km from Broken Hill. | Mylonitic granite randomly folded, outcrop on Adelaide road, 13 km from Broken Hill. |
Inverted graded bedding: from sandstone at the base (just above the finger) through to mudstone at the top, now a coarse biotite-sillimanite schist. Notice the refraction of the foliation indicating that the schist is more competent than the sandstone. | Same. | Same, note sharp transition from the coarse schist below to sandstone above. |
Folded cross-bedding. Note the truncation of folded layers below by the beds above (just below the coin). preserved in concretions within sedimentary rocks that underwent high-grade metamorphism during the 1600M Olarian Orogen. | Two sets of truncated cross-beds, later folded marked by * . Preserved in concretions within sedimentary rocks that underwent high-grade metamorphism during the 1600M Olarian Orogen. | Channel in psammite, preserved in concretions within sedimentary rocks that underwent high-grade metamorphism during the 1600M Olarian Orogen |
Axial planar leucosome. Twanging locality in Purnamoota road, outside Broken Hill. Late, steep, D3 leucosome bending earlier D2 leucosome. | Conjugate set of leucosomes in shear bands. Note the strong axial planar foliation in the paleosome, bisecting the angle defined by the two sets. Broken Hill. | Axial planar leucosome. Close to the previous locality, leucosomes are found in the axial plane. |
Sheared Pegmatite. Dextral deformation of K-feldspar grains in pegmatite margin in the Eldee Creek, Broken Hill Block. |
Same shear zone in pegmatite. |
Pseudotachylyte from the detachment fault zone in Stellida, Naxos, Greece. |
Early stages. Tml-leucosome segregation in an incipient fold. | A more developed stage, diffuse segregation of leucosome into thrust plane. | Tighter fold with a better developed segregation. |
A tight fold riding on a narrow leucosome detached from the foliated rock below. |