Spatio-temporal analysis of Permian-Cretaceous magmatic activities in the Tengchong block: Implications for tectono-magmatic evolution

Xinkun Yang , Zhenjie Zhang , Yuanzhi Zhou , Jie Yang

Geoscience Frontiers ›› 2024, Vol. 15 ›› Issue (6) : 101920

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Geoscience Frontiers ›› 2024, Vol. 15 ›› Issue (6) :101920 DOI: 10.1016/j.gsf.2024.101920

Spatio-temporal analysis of Permian-Cretaceous magmatic activities in the Tengchong block: Implications for tectono-magmatic evolution

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Abstract

Understanding the tectono-magmatic evolution history of the Tengchong block is crucial for elucidating the formation of the Eastern Tethys tectonic domain. However, the correlation and evolution of the Tengchong block with the Sibumasu and Lhasa blocks is controversial during the Permian and Cretaceous. This study explores the information contained within magmatic rocks using big data and spatio-temporal analysis, providing quantitative constraints for the discussion of the tectono-magmatic evolution of the Tengchong block. To more accurately assess true magma activities and reduce errors caused by preservation and sampling processes, we utilized local singularity analysis to obtain the singularity index time-series. Correlation analysis of zircon ages and εHf(t) (correlation coefficient ≥ 0.5) values indicates that the Tengchong block is more similar to the Sibumasu block. Results from time-lagged cross-correlation analysis indicate that the Tengchong block and Sibumasu block exhibit a shorter lag in magmatic activities (3 Myr). Wavelet analysis reveals similar periods of collision-related magmatic activities (57 Myr and 43 Myr). Integrating evidence from paleontology and ophiolite belts, we propose that the Tengchong block co-evolved more closely with the Sibumasu block than with the Lhasa block, suggesting similar tectonic processes during the Early Permian to Early Cretaceous. Approximately 250–236 Ma, in the western Tengchong block, partial melting of the lower crust occurs due to crustal thickening. Around 219–213 Ma and 198–180 Ma, after the Tengchong block collided with the Eurasian continent, the subduction of the Meso-Tethys Ocean commenced. Around 130–111 Ma, the overall tectonic feature was a scissor-like closure of the Meso-Tethys Ocean from north to south.

Keywords

Big data / Local singularity analysis / Spatio-temporal analysis / Tengchong block / Zircon and whole-rock

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Xinkun Yang, Zhenjie Zhang, Yuanzhi Zhou, Jie Yang. Spatio-temporal analysis of Permian-Cretaceous magmatic activities in the Tengchong block: Implications for tectono-magmatic evolution. Geoscience Frontiers, 2024, 15(6): 101920 DOI:10.1016/j.gsf.2024.101920

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CRediT authorship contribution statement

Xinkun Yang: Writing – review & editing, Writing – original draft, Validation, Resources, Methodology, Investigation, Formal analysis, Data curation, Conceptualization. Zhenjie Zhang: Writing – review & editing, Resources, Methodology, Investigation, Formal analysis, Conceptualization. Yuanzhi Zhou: Writing – review & editing, Resources, Investigation, Conceptualization. Jie Yang: Investigation, Conceptualization.

Acknowledgments

We sincerely appreciate the editor for the insights and suggestions provided for this study. This work was supported by the National Key R & D Program of China (Grant No. 2023YFC2906402); the Fundamental Research Funds for the Central Universities (Grant No. 2652023001); and the National Natural Science Foundation of China (Grant Nos. 42472358, 42430111 and 42050103).

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