Citation: | QI Liang, XU Yajun, DU Yuansheng, HOU Mingcai. 2023. Neoproterozoic sedimentary records in the Cathaysia Block and their implications for the supercontinent reconstruction. Sedimentary Geology and Tethyan Geology, 43(1): 188-211. doi: 10.19826/j.cnki.1009-3850.2023.02017 |
The tectonic framework and paleogeographic evolution of Neoproterozoic-early Paleozoic successions in the South China Block provides the first-order constraint on its role in the break-up of Rodinia and the subsequent amalgamation of Gondwana. However, there still is much disagreement in defining the paleoposition of the Cathaysia Block and its relationship with the Yangtze Block. In this thesis, isotopic geochronology, Neoproterozoic glaciations, and mineralization records were found in the Cathaysia Block, providing new evidence for the stratigraphic framework. Detrital zircon U-Pb dating results provide evidence of prominent provenance transition during late Tonian to Ediacaran, and bidirectional sources in the western margin of Cathaysia Block at late Cryogenian, integrating with the evidence from a sedimentary environment of neritic shelf, a closure of paleo-South China Ocean is suggested during late-Neoproterozoic. The detrital records of the early Tonian -Ediacaran strata in the Cathaysia Block present abundant late Mesoproterozoic to early Neoproterozoic(
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Simplified geological map of the South China Craton showing the main Precambrian and early Paleozoic stratigraphic units and Neoproterozoic volcanic rocks of Cathaysia Block.
Stratigraphic correlation chart for mid-late Neoproterozoic units of southeastern South China and their radiometric ages.
Simplified geological map and sample locations.
Field photographs, representative micro-images, and Raman images for selected samples in this study
Mid-late Neoproterozoic stratigraphic column and radiometric ages results of this study.
Compilation of detrital zircon age distribution of southeastern South China and continental blocks/terranes from northern East Gondwana.
U-Pb age vs. εHf (t) diagram for the zircon grains from Neoproterozoic sediments of the Cathaysia Block
(a) The distribution of sedimentary rocks from southeastern South China showing the dominant peak age of detrital zircons. (b) Schematic model showing the source direction on the western margin of Cathaysia Block.
Palaeogeography map of southeastern South China during Cryogenian interglacial period.
Paleoposition of the South China Block in Rodinia supercontinent and Gondwanaland.