Abstract
We here provide an overview of our current understanding of the crustal structure of Tengchong in southwest China, a key intra-plate volcanic area along the Himalayan geothermal belt. Given that there is hitherto a lack of information about the near-surface structure of intra-plate volcanic areas, we present the first seismic reflection and velocity constraints on the shallow crust between intra-plate volcanoes. Our near-surface seismic images reveal the existence of dome-shaped seismic reflectors (DSRs) in the shallow crust between intra-plate volcanic clusters in Tengchong. The two DSRs are both ~2 km wide, and the shallowest parts of the DSRs are found at the depth of 200–300 m. The velocity model shows that the shallow low-velocity layer (<4 km/s) is anomalously thick (~1 km) in the region where the DSRs are observed. The presence of DSRs indicates significant levels of intra-plate magmatism beneath the along-axis gap separating two volcano clusters. Along-axis gaps between volcano clusters are therefore not necessarily an indicator of lower levels of magmatism. The seismic images obtained in this technically challenging area for controlled-source seismology allow us to conclude that shallow crustal structures are crucial for understanding the along-axis variations of magmatism and hydrothermal activities in intra-plate volcanic areas.
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Acknowledgments
We would like to thank S. Li, C. Qian, X. Tang and L. Fan for their scientific contributions to the study, and L. Cobden for help with the Generic Mapping Tools. Funding from SinoProbe-05-07 is gratefully acknowledged.
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Qian, R., Tong, V.C.H. Crustal Structure of the Tengchong Intra-plate Volcanic Area. Surv Geophys 36, 683–691 (2015). https://doi.org/10.1007/s10712-015-9329-z
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DOI: https://doi.org/10.1007/s10712-015-9329-z