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Tectonic Study of the Fracture Zone on Tibetan Plateau’s Eastern Margin

Advanced seismic monitoring to uncover the mysteries of tectonic activity in a high-seismicity region.

Research Overview

As part of the National Key Research and Development Programme, the Institute of Geophysics of the China Earthquake Administration (IGU) initiated a detailed study of the Freshwater River-Longmenshan-Anning River-Daliangshan Fracture Zone in mid-September 2020. The project aims to analyze:

  • Microseismic Activity: Understanding the frequency and distribution of small-scale earthquakes.
  • Fault Morphology: Mapping the physical structure and dynamics of the fault zones.
  • Deep Structural Characteristics: Investigating the underlying geological features that influence tectonic activity.

Special Focus: The “Three Forks” Area

Located at the intersection of the Freshwater River, Longmenshan, and Anning River fault zones, the “Three Forks” area is a unique tectonic region on the eastern edge of the Tibetan Plateau. Known for its high seismicity, this area serves as a natural laboratory for studying:

  • The seismic behavior of the Sichuan-Yunnan rhomboid-shaped block.
  • The deep deformation and morphology of one of the most seismically active regions on the planet.

Equipment Deployed

The project utilized 160 units of the SmartSolo IGU-16HR EB 3C short-cycle, integrated seismic observation system. This advanced equipment provided significant advantages:

  • Compact and Lightweight: Facilitating easy transport and deployment.
  • Simple Operation: Streamlined setup for efficient fieldwork.
  • Durability: Exceptional waterproofing and endurance capabilities.
  • Extended Power Supply: Supporting continuous data collection for up to 130 days.

Observation Timeline

  • Duration: 105 days (mid-September 2020 to early January 2021).
  • Data Collected: Approximately 5TB of high-quality raw seismic data.
  • Power Reserve: Devices retained sufficient power for an additional 25 days of operation.

Significance of the Study

This project offers critical insights into:

  • Seismicity Patterns: Identifying areas of heightened microseismic activity.
  • Fault Zone Dynamics: Providing detailed information on fault morphology and movement.
  • Tectonic Processes: Enhancing our understanding of the deformation characteristics of the Tibetan Plateau’s eastern margin.

The findings are expected to contribute significantly to:

  • Earthquake risk assessment in the Sichuan-Yunnan region.
  • Improved disaster preparedness and mitigation strategies.
  • Advancing geophysical research methodologies for tectonic studies.

Conclusion

The Tectonic Regional Study of the Fracture Zone on the Eastern Margin of the Tibetan Plateau underscores the importance of cutting-edge seismic monitoring technologies like SmartSolo IGU-16HR EB 3C. By enabling precise and efficient data collection in challenging environments, this project paves the way for a deeper understanding of earthquake mechanisms and tectonic processes, fostering safer and more resilient communities in seismic-prone regions.