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Pakistan Stratigraphy
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Mesozoic • Cretaceous formation Literature

Tupop Formation

Late Cretaceous

Karakoram-Hindukush Basin · Central Karakoram Batholith

Cretaceous in the time scale →

Cited in 2 sources Last reviewed Jul 31, 2026

Unit summary
Rank
formation
Status
Published
Age
Mesozoic · Cretaceous · Late CretaceousLate Cretaceous
Named by
Gaetani et al. (1990a)
Type locality
Widely exposed west and south of Babaghundi Ziarat in the Chapursan Valley, along the Buattar valley and northward up the Irshad Uwin Valley (Sost Unit).
Thickness
Not recorded
Lithology
Channelized red cobble–pebble conglomerates in amalgamated several-metre beds interbedded with sandstone and red shales; usually clast-supported with carbonate cement, clasts predominantly carbonate with subordinate terrigenous and few volcanic clasts. Basal rhyolitic ignimbrites (top of the Hidden Gorge) and a ~10 m dark red ignimbrite occur locally.
Synonyms
Not recorded

The Tupop Formation is a Late Cretaceous fluviatile red-conglomerate unit of the Chapursan Valley area (Sost Unit, Karakoram). It consists of channelised, clast-supported red cobble–pebble conglomerates with sandstone and red-shale interbeds and local basal rhyolitic ignimbrites; no fossils were found, so its age rests on regional correlation. It unconformably covers the Triassic Aghil Formation carbonates and is in turn unconformably overlain by the Campanian marls of the Darband Formation — the Reshun/Tupop unconformity marking an important Karakoram deformational event.

Fossils

Not recorded

Contacts

Lower contact — unconformable; upper contact — unconformable.

In the Hindukush-Chitral column
ConglomerateLimestoneSandstoneFossils recordedConformableUnconformity

Band colour = period; texture = dominant rock type. Lines between bands mark the contact type. True scale makes height ∝ recorded thickness; hatched = thickness not recorded. Ages approximate, for ordering.

This unit (highlighted) within its province column; faded ends continue above and below. Line style marks the contact type.

Distribution & setting

Basin
Karakoram-Hindukush Basin
Region
Central Karakoram Batholith
Depositional environment
fluvial, continental
Coordinates
Not recorded

Correlation

Not recorded. Compare this unit against other basins on the correlation panel →

Economic significance

Not recorded

Remarks

A Late Cretaceous fluviatile red-conglomerate unit (age by correlation to the Chapursan Valley; no fossils found) that unconformably covers the Triassic Aghil Formation carbonates and is in turn unconformably covered by the Campanian marls of the Darband Formation. The Reshun/Tupop unconformity marks an important deformational event in the Karakoram.

Sources (3)

Every fact on this page is source-cited. This entry is part of the peer-archived Pakistan Stratigraphy Dataset (doi.org/10.5281/zenodo.21363991, CC‑BY‑4.0).

Lexicon status: Defined in journal or other literature; not found in a GSP memoir. There is no body currently ratifying unit status, so provenance is shown in place of a formal ruling.

Cite this unit
APA

Qudsi, L. (2026). Tupop Formation. In Pakistan Stratigraphy Dataset [Data set]. Zenodo. https://doi.org/10.5281/zenodo.21363991

BibTeX
@misc{stratigraphypk_tupopformation,
  author    = {Qudsi, Lareb},
  title     = {{Tupop Formation} --- Pakistan Stratigraphy Dataset},
  year      = {2026},
  publisher = {Zenodo},
  doi       = {10.5281/zenodo.21363991},
  url       = {https://doi.org/10.5281/zenodo.21363991}
}

Archived dataset: doi.org/10.5281/zenodo.21363991 (CC‑BY‑4.0) · Direct link to this entry: https://stratigraphy.pk/formation/tupop-formation (accessed August 30, 2026).

To cite the unit's original definition instead, see: Gaetani et al. (1990a).

    Saved on this device only.