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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.
A person in a black jacket and cap is crouching, connecting a blue cable to a SmartSolo seismometer node on the ground. A white vehicle is parked behind them. This is part of a seismic survey for geophysical exploration.

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.
A map showing the distribution of SmartSolo seismometer nodes (blue triangles) in a region of China, indicating a seismic survey for earthquake monitoring and geophysical exploration.
A seismograph plot showing seismic activity over 110 days, with significant events around day 0, day 18, and day 108, useful for earthquake monitoring.

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.
Smart Solo Observation Summary chart showing observation days (blue) and data volume in GB (orange) for SmartSolo nodes.

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.