Van Buchen, F.S.P., Baghbani, D., Bulot, L.G., Caron, M., Gaumet, F., Hosseini, S.A., Keyvani, F., Schroeder, R., Swennen, R., Vedrenne V. and Vincent, B. (2010) Barremian— Lower Albian Sequence-Stratigraphy of Southwest Iran (Gadvan, Dariyan and Kazhdumi Formations) and Its Comparison with Oman, Qatar and the United Arab Emirates, GeoArabia Special Publication 4, Vol. 2, 503-548.

has been cited by the following article:

• TITLE: Sedimentology and depositional environment of the Kazhdumi Formation Sandstones in the northwestern area of the Persian Gulf

  AUTHORS: Bijan Noori, Nader Kohansal Ghadimvand, Bahram Movahed, Mohammadreza Yousefpour

  KEYWORDS: Kazhdumi Formation, Sedimentary Facies, Paleoenvironment, Paleocurrent, Persian Gulf

  JOURNAL NAME: Open Journal of Geology, Vol.6 No.11, November 17, 2016

  ABSTRACT: Kazhdumi is one of the Bangestan Group formations aging late early Cretaceous (Albian). Three subsurface sections of the sandstone bearing part of Kazhdumi in the studied area located at northwest of the Persian Gulf are assessed for determining sedimentary facies and depositional environment. Based on the recognized facies, the sandstone bearing zones of Kazhdumi and their relevant paleoenvironments can be addressed as: first one is the B sandstone zone containing thick sandstone layers alternating with shale and siltstone thin layers which are deposited by river influenced conditions because of the characteristics like: cross bedding, oxidized constituents and palesol. The second one, the A sandstone zone which is deposited under a key limestone layer, is composed of sand/sandstone layers with marine features and presents the interaction of marine-river condition in deltaic channels. This zone, is a transition interval showing the changes of river-dominated condition to marine one. The third one is the A sandstone zone deposited above the key limestone layer containing fine grained laminated siliciclastic and chemical sediments. Alternation of distal channel facies and green marine shale of delta containing glauconite, pyrite and organic matter residuals, all confirm the reduction condition in estuarine environment. Applying facies analyses results, isopach maps, porosity distribution maps and sandstone grain size study, the paleocurrent pattern is determined from the southwest to northeast.