| 893 - 916 |
New insights into the formation mechanism of high hydrogen sulfide-bearing gas condensates: Case study of Lower Ordovician dolomite reservoirs in the Tazhong uplift, Tarim Basin
Su J, Zhang SC, Huang HP, Wang Y, Wang HT, He K, Wang XM, Zhang B, Wang HJ |
| 917 - 941 |
Recovery rates of fracturing fluids and provenance of produced water from hydraulic fracturing of Silurian Qusaiba hot shale, northern Saudi Arabia, with implications on fracture network
Birkle P |
| 943 - 967 |
Geochemistry of formation waters from the subsalt Tubular Bells Field, offshore Gulf of Mexico: Implications for fluid movement and reservoir continuity
Franks SG, Uchytil SJ |
| 969 - 1002 |
Comprehensive assessment of source rocks in the Bohai Sea area, eastern China
Jiang FJ, Pang XQ, Bai J, Zhou XH, Li JP, Guo YH |
| 1003 - 1031 |
Microanalysis of carbonate cement delta O-18 in a CO2-storage system seal: Insights into the diagenetic history of the Eau Claire Formation (Upper Cambrian), Illinois Basin
Sliwinski MG, Kozdon R, Kitajima K, Denny A, Valley JW |
| 1033 - 1059 |
Evidence for a petroleum subsystem in the Frontier Formation of the Uinta-Piceance Basin petroleum province
Hutsky AJ, Fielding CR, Frank TD |
| 1061 - 1066 |
The discovery and significance of a sedimentary hiatus within the Carboniferous Taiyuan Formation, northeastern Ordos Basin, China: Discussion
Zheng WB, Hu XY, Chen SW, Liu JD, Jia C |
| 1067 - 1072 |
The discovery and significance of a sedimentary hiatus within the Carboniferous Taiyuan Formation, northeastern Ordos Basin, China: Reply
Jiang ZX, Xu J, Wang GT |
