Match tier
Confirmed
Presence
Current · Arkansas
Last published
2023
Sources
OpenAlex · ORCID
Refreshed
2026-08-08
H
Hayder Al-Shukri
Affiliation confirmed via AI analysis of OpenAlex, ORCID, and web sources.
Researcher
Graduate Student Researcher
1 h-index
1 pubs
1 cited
Research Areas
Biography and Research Information
OverviewAI-generated summary
Hayder Al-Shukri's research investigates geological phenomena, including recent publications on repeated large-magnitude earthquakes in Arkansas and seismic anisotropy under the Zagros foreland. Al-Shukri also studies the assessment of levee slurry walls using ground penetrating radar, with a case study presented in a 2023 publication. His scholarly work includes one publication and one citation, with an h-index of 1. Al-Shukri collaborates with researchers at the University of Arkansas at Little Rock, including Hanan Mahdi, Muntadher Al-Kaabi, and Taher Ameen.
Metrics
- h-index: 1
- Publications: 1
- Citations: 1
Selected Publications
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Comprehensive earthquake catalogue update and spatiotemporal distribution analysis for Iraq and surrounding regions, northeastern Arabian Plate (2026)
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Repeated Large-Magnitude Earthquakes in the Marianna Area of East-Central Arkansas During the Middle-Early Holocene and Possibly the Late Pleistocene (2026)
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Seismic anisotropy under Zagros foreland from SKS splitting observations (2026)
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Levee Slurry Wall Assessment Using Ground Penetrating Radar, A Case Study (2023)
Collaboration Network
Top Collaborators
Hanan K. Mahdi
University of Arkansas at Little Rock
2 shared publications
In database
- Repeated Large-Magnitude Earthquakes in the Marianna Area of East-Central Arkansas During the Middle-Early Holocene and Possibly the Late Pleistocene
- Seismic anisotropy under Zagros foreland from SKS splitting observations
Hussein Khalefa Chlaib
1 shared publication
- Levee Slurry Wall Assessment Using Ground Penetrating Radar, A Case Study
Hanan Mahdi
University of Arkansas at Little Rock
1 shared publication
In database
- Levee Slurry Wall Assessment Using Ground Penetrating Radar, A Case Study
Khalil Motaghi
Institute for Advanced Studies in Basic Sciences (IR)
1 shared publication
- Seismic anisotropy under Zagros foreland from SKS splitting observations
Ayoub Kaviani
Goethe University Frankfurt (DE)
1 shared publication
- Seismic anisotropy under Zagros foreland from SKS splitting observations
Wathiq Abdulnaby
University of Basrah (IQ)
1 shared publication
- Seismic anisotropy under Zagros foreland from SKS splitting observations
Martitia P. Tuttle
M. Tuttle & Associates (US)
1 shared publication
- Repeated Large-Magnitude Earthquakes in the Marianna Area of East-Central Arkansas During the Middle-Early Holocene and Possibly the Late Pleistocene
Rauf Hussein
Coral Reef Alliance (US)
1 shared publication
- Repeated Large-Magnitude Earthquakes in the Marianna Area of East-Central Arkansas During the Middle-Early Holocene and Possibly the Late Pleistocene
Taher Ameen
University of Arkansas at Little Rock
1 shared publication
In database
- Repeated Large-Magnitude Earthquakes in the Marianna Area of East-Central Arkansas During the Middle-Early Holocene and Possibly the Late Pleistocene
Steven L. Forman
Baylor University (US)
1 shared publication
- Repeated Large-Magnitude Earthquakes in the Marianna Area of East-Central Arkansas During the Middle-Early Holocene and Possibly the Late Pleistocene
Martha Kopper
Arkansas State Hospital (US)
1 shared publication
- Repeated Large-Magnitude Earthquakes in the Marianna Area of East-Central Arkansas During the Middle-Early Holocene and Possibly the Late Pleistocene
Muntadher Al-Kaabi
University of Arkansas at Little Rock
1 shared publication
In database
- Repeated Large-Magnitude Earthquakes in the Marianna Area of East-Central Arkansas During the Middle-Early Holocene and Possibly the Late Pleistocene
Okba R. Al-Qadhi
Cincinnati State Technical and Community College (US)
1 shared publication
- Repeated Large-Magnitude Earthquakes in the Marianna Area of East-Central Arkansas During the Middle-Early Holocene and Possibly the Late Pleistocene
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