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May 6, 2026Geophysical Journal International0 citationsOpen Access

Comprehensive Earthquake Catalog Update and Spatiotemporal Distribution Analysis for Iraq and Surrounding Regions, Northeastern Arabian Plate

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MAMuntadher Al-KaabiWAWathiq AbdulnabyNANajah Abd

Key Points

  • This research aims to update the earthquake catalog for Iraq and analyze the spatiotemporal distribution of seismic activity.
  • Compiled a comprehensive earthquake catalog for Iraq from 1900 to 2021 with over 37,000 records.
  • Calculated moment magnitudes for 2,800 earthquakes using the coda envelope technique and waveform data from MPSN.
  • Applied the Gutenberg-Richter relationship to determine a- and b-values specific to the region.
  • Identified significant variations in seismic activity, particularly in the Zagros Fold-Thrust Belt and Mesopotamian Foredeep.
  • Determined seismogenic layers ranging from 1 to 33 km deep across different tectonic features.
  • Revealed high seismic activity around the Mandili-Badra-Teeb fault and mapped the main areas of seismic concern.

Abstract

Summary The updated earthquake catalog for Iraq covers the period from 1900 to the end of 2021 and includes over 37 000 recorded earthquakes. To create this comprehensive catalog, five key steps were taken: compiling bulletins, calculating moment magnitudes, harmonizing magnitudes, establishing empirical conversion relations, and evaluating the completeness of the catalog. A notable enhancement in this update is the direct calculation of moment magnitudes for approximately 2 800 earthquakes, achieved through the coda envelope technique and waveform data from the Mesopotamian Seismological Network (MPSN) in Iraq. This updated catalog serves as a valuable resource for examining the spatiotemporal distribution of earthquakes, with respect to earthquake density, maximum moment magnitude, and seismogenic depths. Additionally, the Gutenberg-Richter relationship was applied to calculate the a- and b-values specific to Iraq. The findings show that the Zagros Fold-Thrust Belt has a seismogenic layer (source) that ranges from 2 to 33 km deep and experiences high seismic activity. In contrast, the Mesopotamian Foredeep has a seismogenic layer ranging from 1 to 25 km deep and has lower seismic activity. The greatest seismic activity is concentrated around the Mandili-Badra-Teeb fault, which has experienced significant ruptures over time. The Outer Arabian Platform is identified as the main area of seismic activity, while additional activity occurs on the Inner Arabian Platform. Three major tectonic boundaries define the distribution of earthquakes in the northeastern Arabian Plate. These boundaries are defined by the Main Zagros Reverse Fault, the Zagros Foredeep Fault, and the Anah Graben and Abu Jir-Euphrates Fault Zone. These boundaries highlight variations in seismicity levels and the spatial distribution of deformation in the region. The updated earthquake catalog presented in this study is expected to play a vital role in regional seismicity assessments and seismic hazard analyses for Iraq and its surrounding areas.

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Cite This Study

Al-Kaabi et al. (2026) studied this question.

synapsesocial.com/papers/69fa8e8904f884e66b530d95https://doi.org/10.1093/gji/ggag162
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