Source provenance
Khan, U., Khan, M., Shiguo, W. & Gao, J. (2024). Geodynamics and structural evolution of Makran accretionary prism, Arabian-Eurasian convergent plate boundary. EGU General Assembly 2024, Vienna, abstract EGU24-17684.
Cited by 2 units (2 published) · 0 field-level citations · 2 revision notes.
Structural framework of the Makran accretionary prism; context for the Panjgur and Hoshab formations.
This page is the reverse of each unit's per-field citations — it shows exactly what this reference supports, making the dataset's “no source, no fact” rule browsable both ways.
Units citing this source
-
- Geological significance: Khan et al. (2024): the abyssal-to-deep-marine Hoshab Formation belongs to the fill of the offshore Makran accretionary prism — the world's largest — formed by Arabian-under-Eurasian convergence (Early Cretaceous onset, Middle Miocene renewed subduction), whose thrust-wedge shortening and continuous sediment influx built a ~7.5-km-thick succession.
-
- Geological significance: Khan et al. (2024): the Panjgur Formation's deep-sea submarine-fan turbidites form part of the offshore Makran accretionary prism — the world's largest — built by convergence of the Arabian plate beneath Eurasia (Early Cretaceous onset, with Middle Miocene renewed subduction); tectonic shortening and imbricate thrust faulting, with a continuous sediment influx, produced a ~7.5-km-thick sedimentary succession.