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| | GEO_PLATE_T-49.HTML (Site not responding. Last check: 2007-11-06) |
 | | It separates the Tarim basin to the south from the Kazakhstan shield and the Dzungarian basin to the north. |
 | | Arc collisions during the Silurian, Devonian, and Mississippian and, finally, suturing along the Tian Shan in the Late Paleozoic produced most of the structural and metamorphic fabric of the mountain interiors in the northwest part of the Plate scene (Bally et al., 1980; Dewey and Burke, 1973; Gansser, 1974; and Zhang and Liou, 1984). |
 | | The folds, which lie on the north edge of the Tarim basin, are overturned to the south and thrust on the south side. |
| daac.gsfc.nasa.gov /geomorphology/GEO_2/GEO_PLATE_T-49.HTML (654 words) |
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