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Kangan Formation
Upper Dalan Member and Kangan Formation between the Zagros Mountains and offshore Fars, Iran: depositional system, biostratigraphy and stratigraphic architecture
Kuh-e Dena – facies and outcrop details – (g) Lower Kangan Formation, thinl...
Paragenetic sequence of the Kangan Formation in Well A.
Kuh-e Surmeh – facies and outcrop details – (h) Upper Dalan Member, wackest...
Kuh-e Dena – general log and panorama, Upper Dalan Member and Kangan Format...
Paleozoic stratigraphic lexicon and hydrocarbon habitat of Iraq
Sedimentological logs showing facies belts and poroperm values of the Kanga...
Kuh-e Surmeh – Northeast/Southwest panorama, Upper Dalan Member and Kangan ...
Idealized field-scale facies model for reservoir rocks (Upper Permian–Lower...
Kuh-e Dena – facies and outcrop details – (a) Uppermost Lower Dalan Member,...
The Permo–Triassic Sequence of the Arabian Plate Abstracts of the EAGE’s Third Arabian Plate Geology Workshop, Part II
Effects of depositional and diagenetic characteristics on carbonate reservoir quality: a case study from the South Pars gas field in the Persian Gulf
Early–Middle Triassic Dashtak Formation in the Zagros Domain, Iran: controls of eustasy, tectonic, and palaeoclimate
Abstract The Early to Middle Triassic Dashtak Formation provides an effective, regional seal for the Permian-Triassic Dalan-Kangan (Khuff) reservoirs and also forms the subordinate reservoir in a number of gas fields in eastern Zagros. This formation consists of four large-scale carbonate–evaporite cycles, which deposited in a vast epeiric carbonate/evaporite platform. Stacking of carbonates and anhydrites cycles was controlled by relative sea-level fluctuations under a prevailing arid palaeoclimate. After deposition, facies was subjected to extensive hypersaline diagenesis and compaction, which leads to major changes in their reservoir properties. Combination of lithostratigraphic correlation, strontium isotope data, and isopach map suggests that the upper cycles (A and B) of the formation were removed in offshore areas during the Pre-Jurassic uplifting event.