Late cretaceous conglomerates of the Qahlah formation, North Oman

Iftikhar A. Abbasi, O. Salad Hersi, A. Al-Harthy

Research output: Contribution to journalArticle

9 Citations (Scopus)

Abstract

Conglomerate sequences over 700 m thick were deposited subsequent to ophiolite emplacement during Late Cretaceous time in north Oman. The conglomerates were deposited by streams draining the allochthonous ophiolite and Hawasina complex after their obduction onto autochthonous Mesozoic and older Oman shelf sequences and subsequent uplift. The conglomerates belong to the Qahlah Formation of Late Cretaceous age, which is sandwiched between the Semail Ophiolite/Hawasina complex and Maastrichtian-Palaeogene carbonate rocks. The siliciclastics of the Qahlah Formation are the first sediments deposited over the obducted oceanic crust sequence of ophiolite and Hawasina lithologies. In five locations studied in north Oman, the thickness of the formation varies from 140 m to over 700 m and comprises interbedded conglomerate, sandstone and siltstone. The sediments were deposited in isolated segmented depressions each characterized by its source terrain depending on lithologies exposed in the source area. Lithofacies associations, clast sorting and grain roundness suggest deposition in stream-dominated alluvial fans. Clasts in the conglomerates range from subangular to subrounded pebbles to boulders with both grain and matrix (sandstone) support. Cross-bedded fining-upwards sequences in channelized conglomerate and sandstone suggest deposition by high-energy flows in the proximal to distal reaches of alluvial fans. High proportions of chert and ophiolite fragments in the conglomerates suggest rapid erosion of obducted oceanic crust. The presence of Loftusiabearing carbonate beds and bivalve-bearing conglomerate beds in different sections indicates occasional interruption of alluvial deposition by marine transgressions

Original languageEnglish
Pages (from-to)325-341
Number of pages17
JournalGeological Society Special Publication
Volume392
Issue number1
DOIs
Publication statusPublished - 2014

Fingerprint

Sandstone
conglomerate
Lithology
Cretaceous
ophiolite
Fans
Carbonates
Sediments
Bearings (structural)
Sorting
Erosion
sandstone
alluvial fan
Rocks
clast
oceanic crust
lithology
fining sequence
obduction
energy flow

ASJC Scopus subject areas

  • Ocean Engineering
  • Water Science and Technology
  • Geology

Cite this

Late cretaceous conglomerates of the Qahlah formation, North Oman. / Abbasi, Iftikhar A.; Hersi, O. Salad; Al-Harthy, A.

In: Geological Society Special Publication, Vol. 392, No. 1, 2014, p. 325-341.

Research output: Contribution to journalArticle

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