Articles | Volume 10, issue 1
https://doi.org/10.5194/se-10-225-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Special issue:
https://doi.org/10.5194/se-10-225-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Structural expression of a fading rift front: a case study from the Oligo-Miocene Irbid rift of northwest Arabia
The Dr. Moses Strauss Department of Marine Geosciences, Leon H.
Charney School of Marine Sciences, Haifa University, Mt. Carmel, Haifa
31905, Israel
Amit Segev
Geological Survey of Israel, 30 Malkhe Israel, Jerusalem 95501,
Israel
Zvi Ben-Avraham
Department of Geophysics and Planetary Sciences, Tel Aviv University,
Tel Aviv 69978, Israel
Uri Schattner
The Dr. Moses Strauss Department of Marine Geosciences, Leon H.
Charney School of Marine Sciences, Haifa University, Mt. Carmel, Haifa
31905, Israel
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Cited
17 citations as recorded by crossref.
- Why does volcanism associated with the Dead Sea fault occur only along its crossing with the Irbid rift and Harrat Ash-Shaam volcanic field? A. Segev & U. Schattner https://doi.org/10.1016/j.tecto.2023.229718
- Tethys ocean withdrawal and continental peneplanation—An example from the Galilee, northwestern Arabia R. Wald et al. https://doi.org/10.1016/j.jog.2019.06.002
- Detailed Regional Magnetic Mapping on a Bike, A Case Study from Northern Israel U. Schattner et al. https://doi.org/10.1007/s00024-022-03100-1
- Crustal Structure Across the Central Dead Sea Transform and Surrounding Areas: Insights Into Tectonic Processes in Continental Transforms U. ten Brink et al. https://doi.org/10.1029/2023TC007799
- Analyzing Recent Tectonic Activity Along the Karak Wadi Al Fayha Fault System Using Seismic, Earthquake, and Remote Sensing Data M. Al Hseinat et al. https://doi.org/10.3390/geosciences15050177
- Monsoonal upwelling and organic matter preservation in the Eocene Rashrashiyah Formation: Implications for hydrocarbon potential in the Turayf-Sirhan Basin, northwestern Arabia S. Allam et al. https://doi.org/10.1016/j.jafrearsci.2026.106110
- Fragmentation of the Sinai Plate indicated by spatial variation in present-day slip rate along the Dead Sea Fault System F. Gomez et al. https://doi.org/10.1093/gji/ggaa095
- Almost a sharp cut – A case study of the cross point between a continental transform and a rift, based on 3D gravity modeling M. Rosenthal et al. https://doi.org/10.1016/j.tecto.2019.04.012
- Deciphering the Africa-Arabia breakup: Insights from U-Pb dating along the Carmel-Gilboa fault system and its triple junction with the Dead Sea transform O. Oren et al. https://doi.org/10.1016/j.epsl.2023.118152
- When did the Dead Sea fault become a transform? A. Segev et al. https://doi.org/10.1016/j.tecto.2024.230543
- Miocene to sub-Recent magmatism at the intersection between the Dead Sea Transform and the Ash Shaam volcanic field: evidence from the Yarmouk River gorge and vicinity A. Segev et al. https://doi.org/10.1017/S0016756821001072
- Uplift and subsidence at the periphery of the Lebanese Restraining Bend, Northern Dead Sea Fault N. Wetzler et al. https://doi.org/10.1016/j.tecto.2022.229292
- Post-rift regional volcanism in southern Santos Basin and the uplift of the adjacent South American coastal range U. Schattner & M. Michaelovitch de Mahiques https://doi.org/10.1016/j.jsames.2020.102855
- Tectono-stratigraphic framework and evolution of the northwestern Arabian plate, Central Jordan M. Al Hseinat et al. https://doi.org/10.1016/j.tecto.2023.229993
- Tectono-stratigraphic evolution of the Late Cretaceous-Eocene of Jordan and implications for the Arabian Plate convergent margin phase A. Kalifi et al. https://doi.org/10.1016/j.marpetgeo.2025.107525
- Oligocene—Miocene Tectono‐Stratigraphic Development of the Southern Levant Basin, Eastern Mediterranean Sea A. Joffe et al. https://doi.org/10.1111/bre.70075
- Petrogenesis and tectonic implications of peralkaline-metaluminous magmatism in Kila and Shira ring complexes, north-central Nigeria V. Kamaunji et al. https://doi.org/10.1080/00206814.2024.2432014
17 citations as recorded by crossref.
- Why does volcanism associated with the Dead Sea fault occur only along its crossing with the Irbid rift and Harrat Ash-Shaam volcanic field? A. Segev & U. Schattner https://doi.org/10.1016/j.tecto.2023.229718
- Tethys ocean withdrawal and continental peneplanation—An example from the Galilee, northwestern Arabia R. Wald et al. https://doi.org/10.1016/j.jog.2019.06.002
- Detailed Regional Magnetic Mapping on a Bike, A Case Study from Northern Israel U. Schattner et al. https://doi.org/10.1007/s00024-022-03100-1
- Crustal Structure Across the Central Dead Sea Transform and Surrounding Areas: Insights Into Tectonic Processes in Continental Transforms U. ten Brink et al. https://doi.org/10.1029/2023TC007799
- Analyzing Recent Tectonic Activity Along the Karak Wadi Al Fayha Fault System Using Seismic, Earthquake, and Remote Sensing Data M. Al Hseinat et al. https://doi.org/10.3390/geosciences15050177
- Monsoonal upwelling and organic matter preservation in the Eocene Rashrashiyah Formation: Implications for hydrocarbon potential in the Turayf-Sirhan Basin, northwestern Arabia S. Allam et al. https://doi.org/10.1016/j.jafrearsci.2026.106110
- Fragmentation of the Sinai Plate indicated by spatial variation in present-day slip rate along the Dead Sea Fault System F. Gomez et al. https://doi.org/10.1093/gji/ggaa095
- Almost a sharp cut – A case study of the cross point between a continental transform and a rift, based on 3D gravity modeling M. Rosenthal et al. https://doi.org/10.1016/j.tecto.2019.04.012
- Deciphering the Africa-Arabia breakup: Insights from U-Pb dating along the Carmel-Gilboa fault system and its triple junction with the Dead Sea transform O. Oren et al. https://doi.org/10.1016/j.epsl.2023.118152
- When did the Dead Sea fault become a transform? A. Segev et al. https://doi.org/10.1016/j.tecto.2024.230543
- Miocene to sub-Recent magmatism at the intersection between the Dead Sea Transform and the Ash Shaam volcanic field: evidence from the Yarmouk River gorge and vicinity A. Segev et al. https://doi.org/10.1017/S0016756821001072
- Uplift and subsidence at the periphery of the Lebanese Restraining Bend, Northern Dead Sea Fault N. Wetzler et al. https://doi.org/10.1016/j.tecto.2022.229292
- Post-rift regional volcanism in southern Santos Basin and the uplift of the adjacent South American coastal range U. Schattner & M. Michaelovitch de Mahiques https://doi.org/10.1016/j.jsames.2020.102855
- Tectono-stratigraphic framework and evolution of the northwestern Arabian plate, Central Jordan M. Al Hseinat et al. https://doi.org/10.1016/j.tecto.2023.229993
- Tectono-stratigraphic evolution of the Late Cretaceous-Eocene of Jordan and implications for the Arabian Plate convergent margin phase A. Kalifi et al. https://doi.org/10.1016/j.marpetgeo.2025.107525
- Oligocene—Miocene Tectono‐Stratigraphic Development of the Southern Levant Basin, Eastern Mediterranean Sea A. Joffe et al. https://doi.org/10.1111/bre.70075
- Petrogenesis and tectonic implications of peralkaline-metaluminous magmatism in Kila and Shira ring complexes, north-central Nigeria V. Kamaunji et al. https://doi.org/10.1080/00206814.2024.2432014
Saved (final revised paper)
Latest update: 09 Jun 2026
Short summary
Plate-scale rifting is frequently expressed by the subsidence of structural basins along an axis, but postdating tectonic and magmatic activity mostly obscures them. A 3-D subsurface imaging and facies analysis down to 1 km reveals uniquely preserved Galilean basins subsiding along a failing rift front in two main stages. Rifting within a large releasing jog (20–9 Ma), followed by localized grabenization off the Dead Sea fault plate boundary (9–5 Ma), prevents them from dying out peacefully.
Plate-scale rifting is frequently expressed by the subsidence of structural basins along an...
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