ArticleACS omega2026
Geochemical Evidence for the Evolution of the Deyang-Anyue Rift in the Ediacaran-Cambrian Period on the Northwestern Margin of the Yangtze Block.
Article in ACS omega, 2026. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Not yet cited in PubMed.
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Abstract
The evolution of a large intracratonic rift trough in the northern Sichuan Basin, China, along the northwestern margin of the Yangtze Block, is documented during the significant Ediacaran-Cambrian Transition (ECT). Three prevailing perspectives exist regarding the specific genesis of this rift: the inherited development of rift basins, erosional troughs, and tensional erosional troughs. However, the dynamic mechanisms underlying rift trough development and the precise timing of this transition remain contentious. Consequently, this paper conducts a systematic geochemical and chronological investigation for the first time, utilizing siliceous sediments from the Dengying Formation and detrital zircons from the Cambrian Canglangpu Formation. Detrital zircons are used to constrain the Neoproterozoic tectonic evolution of the northwestern Yangtze Block, and geochemical records of siliceous sediments are adopted to reconstruct the evolutionary history of the rift trough. The study's results indicate the following: 1. Neoproterozoic zircons in the study area are dominated by continental arc signatures, with features of arc-associated orogenic compression and partially depleted mantle affinities. Crustal thickness variations calculated from zircon Eu/Eu* ratios indicate that arc-related extensional rifting occurred in the study area after ∼650 Ma. 2. The δ
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