| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6441189 | Lithos | 2011 | 15 Pages |
Abstract
⺠Gabbro and type I lavas with MORB and minor Nb-depletion indicate a Devonian back-arc basin. ⺠Type II lavas and tuff with MORB, OIB and SSZ features record a late Carboniferous ridge subduction. ⺠Devonian-Carboniferous intra-oceanic subduction constrains orogenic architecture of Altaids.
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Authors
Ji'en Zhang, Wenjiao Xiao, Chunming Han, Qigui Mao, Songjian Ao, Qianqian Guo, Chong Ma,