Timing and Provenance Transition of the Neoproterozoic Wuling Unconformity and Xihuangshan Unconformity of the Yangtze Block: Responses to Peripheral Orogenic Events
Abstract
:1. Introduction
2. Geological Setting and Sampling
2.1. Geological Setting
2.2. Sample Descriptions
3. Analytical Methods
3.1. Zircon LA−ICP−MS U−Pb Dating
3.2. Zircon Lu−Hf Isotope Analysis
4. Analytical Results
4.1. Upper Lengjiaxi Group
4.2. Lowermost Madiyi Formation
4.3. Uppermost Madiyi Formation
4.4. Lowermost Wuqiangxi Formation
5. Discussion
5.1. Constraints on Timing of the Middle Neoproterozoic Unconformities
5.1.1. Regional Geological Features and Timing of the Wuling Unconformity
5.1.2. Regional Geological Features and Timing of the Xihuangshan Unconformity
5.2. Provenance Variability of the Neoproterozoic Sedimentary Rocks
5.2.1. Provenance of the Lengjiaxi Group and the Lower Banxi Group
5.2.2. Provenance of the Upper Banxi Group
5.3. Implications for the Tectonic Evolution
6. Conclusions
Supplementary Materials
Author Contributions
Funding
Data Availability Statement
Acknowledgments
Conflicts of Interest
References
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Sample | GPS | Rock Type | Compositions |
---|---|---|---|
GZ01 | N 28°41′25.5″, E 110°06′17.5″ | Fine-grained lithic sandstone | 45% quartz, 35% debris, 10% feldspar, 5% sericite, 5% cement |
GZ03 | N 28°41′05.6″, E 110°05′51.3″ | Fine-grained iron lithic sandstone | 38% quartz, 35% debris, 10% sericite, 4% feldspar, 10% ferruginous cement, 3% matrix |
GZT11 | N 28°36′18.9″, E 109°57′56.2″ | Fine-grained lithic sandstone | 50% quartz, 40% debris, 5% feldspar, 5% sericite, 5% cement |
GZT12 | N 28°36′18.3″, E 109°57′57.6″ | Pebbly lithic quartz sandstone | 70% quartz, 17% debris, 3% feldspar, 5% sericite, 5% calcareous cement |
ZJ05 | N 27°30′18.4″, E 109°38′12.8″ | Feldspar lithic sandstone | 45% quartz, 30% debris, 10% feldspar, 10% calcareous cement, 5% matrix |
ZJ11 | N 27°26′38.4″, E 109°28′17.4″ | Medium-grained lithic sandstone | 40% quartz, 36% debris, 5% sericite, 4% feldspar, 10% ferruginous cement, 5% matrix |
ZJ14 | N 27°32′48.8″, E 109°37′53.4″ | Silty slate | 30% quartz, 15% sericite, 5% ferruginous cement, 50% argillaceous |
ZJ28 | N 27°32′48.8″, E 109°37′53.4″ | Sandy conglomerate | 80% quartz, 4% feldspar, 6% debris, 7% cement, 3% matrix |
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Li, D.; Yang, Z.; Liu, Y.; Yang, K.; Wu, D.; Cai, P. Timing and Provenance Transition of the Neoproterozoic Wuling Unconformity and Xihuangshan Unconformity of the Yangtze Block: Responses to Peripheral Orogenic Events. Minerals 2022, 12, 596. https://doi.org/10.3390/min12050596
Li D, Yang Z, Liu Y, Yang K, Wu D, Cai P. Timing and Provenance Transition of the Neoproterozoic Wuling Unconformity and Xihuangshan Unconformity of the Yangtze Block: Responses to Peripheral Orogenic Events. Minerals. 2022; 12(5):596. https://doi.org/10.3390/min12050596
Chicago/Turabian StyleLi, Dinghua, Zhenning Yang, Yu Liu, Kunguang Yang, Dehai Wu, and Pingting Cai. 2022. "Timing and Provenance Transition of the Neoproterozoic Wuling Unconformity and Xihuangshan Unconformity of the Yangtze Block: Responses to Peripheral Orogenic Events" Minerals 12, no. 5: 596. https://doi.org/10.3390/min12050596
APA StyleLi, D., Yang, Z., Liu, Y., Yang, K., Wu, D., & Cai, P. (2022). Timing and Provenance Transition of the Neoproterozoic Wuling Unconformity and Xihuangshan Unconformity of the Yangtze Block: Responses to Peripheral Orogenic Events. Minerals, 12(5), 596. https://doi.org/10.3390/min12050596