Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
6443669 | Gondwana Research | 2013 | 19 Pages |
Abstract
⺠Nemegt and Altan Nuruu straddle the Dzolen-Edrengin terrane boundary. ⺠Ophiolite obduction occurred in the late Carboniferous. ⺠Oroclinal bending, shortening and lateral redistribution occurred in the Permo-Triassic.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
Stephen Rippington, Dickson Cunningham, Richard England, Bart Hendriks,