| Article ID | Journal | Published Year | Pages | File Type | 
|---|---|---|---|---|
| 8912534 | Precambrian Research | 2018 | 59 Pages | 
Abstract
												In situ zircon U-Pb dating of 173 detrital zircons from the meta-calcsilicate rocks yield Archean ages up to 3.04â¯Ga; a further predominant age population clusters at ca. 2.68â¯Ga with subordinate clusters at ca. 2.87, 2.78, which are interpreted to represent magmatic ages. A subordinate cluster at 2.51â¯Ga associated with zircon rim domains reflects a metamorphic event. Further frequently textureless rims of zircon of an age range between ca. 2.5 and â2.1â¯Ga indicate subsequent metamorphic events. The deposition of the meta-calcsilicate precursors occurred around of shortly after 2.1â¯Ga on an Archaean basement.
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											Authors
												Xu-Ping Li, Xiao Wang, Shuang Chen, Craig Storey, Fan-Mei Kong, Hans-Peter Schertl, 
											