| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4723239 | Precambrian Research | 2013 | 14 Pages |
Abstract
⺠The Xiaoqinling area was southernmost segment of the Trans-North China Orogen. ⺠Taihua Complex from Xiaoqinling area was formed within the Paleoproterozoic. ⺠Collision between W- & E-Blocks along TNCO occurred in the Paleoproterozoic. ⺠Xiaohe granite consist the late Archean crust and newly formed mantle materials. ⺠Primary magma of granite gneisses derived from the late Archean depleted mantle.
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Authors
Xinqi Yu, Junlai Liu, Chunlin Li, Shuaiqi Chen, Yanpei Dai,