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- W2391632805 abstract "The Proterozoic strata outcrop widely in Dongchuan and Central Yunnan but the outcrops are discontinuously distributed in these areas.Due to the lack of paleontological and age data,there have been conficting views on the stratigraphic sequence and correlation of these strata.We here report a SHRIMP zircon age of 1503±17 Ma from a volcanic tuff in the Heishan Formation of the Dongchuan region,and a 1047±15 Ma SHRIMP zircon age from the Heishantou Formation in Central Yunnan.Thus,the two Formations are of different depostional ages and ther cannot be correlated.We also confirm that the stratigraphic sequences in both regions are of nomal stratigraphic sequence.Therefore,it is recommended that the Mesoproterozoic stratigraphic units be maintained separately in these two regions because they are of different ages." @default.
- W2391632805 created "2016-06-24" @default.
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- W2391632805 date "2011-01-01" @default.
- W2391632805 modified "2023-09-22" @default.
- W2391632805 title "STRATIGRAPHIC FRAMEWORK OF THE MESOPROTEROZOIC IN DONGCHUAN AND CENTRAL YUNNAN REGION" @default.
- W2391632805 hasPublicationYear "2011" @default.
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