Sedimentology and detrital zircon geochronology of the Nanduan Formation (Carboniferous) of the Changning-Menglian Belt: indications for the evolution of Paleo-Tethys in western Yunnan, China

• Published in: International journal of earth sciences : Geologische Rundschau 2019-04, Vol.108 (3), p.1029-1048
• Main Authors: Zheng, Jianbin, Jin, Xiaochi, Huang, Hao, Zong, Pu
• Format: Article
• Language: English
• Subjects: Age; Allochthonous deposits; Carboniferous; Cherts; Continental margins; Devonian; Earth and Environmental Science; Earth Sciences; Evolution; Geochemistry; Geochronology; Geochronometry; Geological time; Geology; Geophysics/Geodesy; Igneous rocks; Magma; Mineral Resources; Mudstone; Neritic environment; Original Paper; Paleoceanography; Permian; Provenance; Radiometric dating; Sandstone; Seamounts; Sedimentology; Stratigraphy; Structural Geology; Zircon
• ISSN: 1437-3254; 1437-3262
• DOI: 10.1007/s00531-019-01694-x

The Changning-Menglian Belt in western Yunnan, China, has been considered for decades as a remnant of Paleo-Tethys in this region. However, the understanding of the geological evolution of the belt remains sketchy and incomplete. As a significant component of the stratigraphic successions in the eastern part of the belt, the siliciclastic Nanduan Formation preserved essential information of the developing history of the belt. Petrologic studies of the formation show that it was deposited in a neritic environment. The increase of mudstone beds and decrease of grain size of sandstones upwards suggest a gradual deepening of sedimentary environment. Petrographic and geochemical characteristics of sandstones show that they were derived from mature continental provenance and deposited in a passive continental margin setting. Detrital zircon ages of the formation range from 362 to 3685 Ma. The youngest detrital zircon age (362.2 ± 5.5 Ma) confines the deposition age of the sandstones to being younger than the latest Devonian. Dominant age populations of ca. 950 Ma and ca. 550 Ma can be correlated with the magmatic events that occurred in Eastern Ghats-northern Prince Charles (India–Antarctica) (ca. 950 Ma) and Pan-African orogens (Australia–India) (ca. 550 Ma), which are considered, therefore, to be the main provenance of the Nanduan Formation. These results let us consider that the Nanduan Formation and the underlying Lancang Group were formed on the margin of the Baoshan-Shan Block (therefore, autochthonous), and the Carboniferous‒Permian limestones of seamount resemblance, the oceanic bedded cherts, and basic and ultra-basic igneous rocks in the central zone of the belt are overthrusted slices (allochthonous).