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Hisham A. Al-Siyabi
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Journal Article
Limits to the sealing capacity of rock salt: A case study of the infra-Cambrian Ara Salt from the South Oman salt basin
Johannes Schoenherr, Janos L. Urai, Peter A. Kukla, Ralf Littke, Zsolt Schléder, Jean-Michel Larroque, Mark J. Newall, Nadia Al-Abry, Hisham A. Al-Siyabi, Zuwena Rawahi
Journal: AAPG Bulletin
Publisher: American Association of Petroleum Geologists
Published: 01 November 2007
AAPG Bulletin (2007) 91 (11): 1541–1557.
Journal Article
Exploration history of the Ara intrasalt carbonate stringers in the South Oman Salt Basin
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 October 2005
GeoArabia (2005) 10 (4): 39–72.
Journal Article
Digital characterization of thrombolite-stromatolite reef distribution in a carbonate ramp system (terminal Proterozoic, Nama Group, Namibia)
Erwin W. Adams, John P. Grotzinger, Wesley A. Watters, Stefan Schröder, David S. McCormick, Hisham A. Al-Siyabi
Journal: AAPG Bulletin
Publisher: American Association of Petroleum Geologists
Published: 01 October 2005
AAPG Bulletin (2005) 89 (10): 1293–1318.
Journal Article
Sedimentology and play potential of the late Neoproterozoic Buah Carbonates of Oman
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 October 2004
GeoArabia (2004) 9 (4): 11–36.
Journal Article
Surface-piercing salt domes of interior North Oman, and their significance for the Ara carbonate ‘stringer’ hydrocarbon play
Jeroen M. Peters, Jacek B. Filbrandt, John P. Grotzinger, Mark J. Newall, Mark W. Shuster, Hisham A. Al-Siyabi
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 April 2003
GeoArabia (2003) 8 (2): 231–270.
Book Chapter
Anatomy of a Type II Turbidite Depositional System: Upper Jackfork Group, Degray Lake Area, Arkansas
Author(s)
Hisham A. Al-Siyabi
Series: AAPG Memoir
Publisher: American Association of Petroleum Geologists
Published: 01 January 2000
DOI: 10.1306/M72703C22
EISBN: 9781629812625
Abstract The upper Jackfork Group in the DeGray Lake area, Arkansas, represents a Type II turbidite depositional system with proximal lobes, distal lobes, and channel fills. Diagnostic facies assemblages and sand/shale ratios characterize each of these deposits. In addition, vertical facies arrangements, upward bed thickness trends, and downcurrent bed continuity vary among these deposits. The depositional setting is divided into three areas: upper fan, transition zone, and middle to lower fan. In these settings, channel fills are envisioned to occur in the upper-fan region. While proximal lobes dominate the transition zone, distal lobes populate the middle- to lower-fan region.