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Isopachs of the source rocks developed in the lower part of the Garau Formation (after Bordenave and Huc, 1995). Regional highs close to the Mesopotamian depression area are also indicated. 100 km (62.1 mi). From M. L. Bordenave, 2014, Petroleum System...
Isopachs of the source rocks developed in the lower part of the Garau Formation (after Bordenave and Huc, 1995). Regional highs close to the Mesopotamian depression area are also indicated. 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.