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Cumulative isopach map from the top of the Hith Anhydrite to the top of the Mishan Formation indicating the geometry of the Arab reservoir before the Zagros folding, together with the isopach map of the Hanifa–Tuwaiq Mountain and Diyab source rocks (...
Cumulative isopach map from the top of the Hith Anhydrite to the top of the Mishan Formation indicating the geometry of the Arab reservoir before the Zagros folding, together with the isopach map of the Hanifa–Tuwaiq Mountain and Diyab source rocks (TOC in excess of 1%), their current thermal maturity expressed as vitrinite reflectance equivalent (after Ayres et al., 1982; Loufti and El Bishlawy, 1986 for Abu Dhabi; Carrigan et al., 1995 for Saudi Arabia), and migration paths from the kitchens toward the Gavbendi High. 100 km (62.1 mi). From M. L. Bordenave, 2014, Petroleum Systems and Distribution of the Oil and Gas Fields in the Iranian Part of the Tethyan Region, in L. Marlow, C. Kendall, and L. Yose, eds., Petroleum systems of the Tethyan region: AAPG Memoir 106, p. 505-540.