| Cambrian Jutana Formation (dominated by dolostone) is a proven producing hydrocarbon reservoir rock in Potwar Plateau, Pakistan (Khan et al., 1986). Middle - Upper Ordovician Red River Formation (North Dakota, USA) is producing from intercrystalline porosity (Scholle and Ulmer-Scholle, 2003). The Lower Triassic Kangan Formation is the major carbonate (dolomite-rich) reservoir of natural gas in southwest Iran and Persian Gulf (Peyravi et al., 2016). Upper Jurassic Arab D Carbonate (Dukhan Field, Qatar) is producing from biomoldic and oomoldic porosities (Scholle and Ulmer-Scholle, 2003). Lower Cretaceous Shuaiba Formation (Offshore Qatar) is producing from patchy and intercrystalline porosities (Scholle and Ulmer-Scholle, 2003). Oligocene to Lower Miocene Asmari Formation (containing dolomite) is a giant hydrocarbon producing reservoir in Iran (Lackpour et al., 2008). | | Cambrian Jutana Formation (dominated by dolostone) is a proven producing hydrocarbon reservoir rock in Potwar Plateau, Pakistan (Khan et al., 1986). Middle - Upper Ordovician Red River Formation (North Dakota, USA) is producing from intercrystalline porosity (Scholle and Ulmer-Scholle, 2003). The Lower Triassic Kangan Formation is the major carbonate (dolomite-rich) reservoir of natural gas in southwest Iran and Persian Gulf (Peyravi et al., 2016). Upper Jurassic Arab D Carbonate (Dukhan Field, Qatar) is producing from biomoldic and oomoldic porosities (Scholle and Ulmer-Scholle, 2003). Lower Cretaceous Shuaiba Formation (Offshore Qatar) is producing from patchy and intercrystalline porosities (Scholle and Ulmer-Scholle, 2003). Oligocene to Lower Miocene Asmari Formation (containing dolomite) is a giant hydrocarbon producing reservoir in Iran (Lackpour et al., 2008). |
| Adams, A.E., MacKenzie, W.S., 1998. A colour atlas of Carbonate sediments and rocks under the microscope. Manson Publishing. | | Adams, A.E., MacKenzie, W.S., 1998. A colour atlas of Carbonate sediments and rocks under the microscope. Manson Publishing. |