1 |
Feldspar dissolution, authigenic clays, and quartz cements in open and closed sandstone geochemical systems during diagenesis: Typical examples from two sags in Bohai Bay Basin, East China Yuan GH, Cao YC, Gluyas J, Li XY, Xi KL, Wang YZ, Jia ZZ, Sun PP, Oxtoby NH AAPG Bulletin, 99(11), 2121, 2015 |
2 |
Reservoir quality, textural evolution and origin of fault-associated dolomites Wilson MEJ, Evans MJ, Oxtoby NH, Nas DS, Donnelly T, Thirlwall M AAPG Bulletin, 91(9), 1247, 2007 |
3 |
The origin of dolomite in the Asmari Formation (Oligocene-Lower Miocene), Dezful Embayment, SW Iran Aqrawi AAM, Keramati M, Ehrenberg SN, Pickard N, Moallemi A, Svana T, Darke G, Dickson JAD, Oxtoby NH Journal of Petroleum Geology, 29(4), 381, 2006 |
4 |
Gas souring by thermochemical sulfate reduction at 140 degrees C: Reply Worden RH, Smalley PC, Oxtoby NH AAPG Bulletin, 82(10), 1874, 1998 |
5 |
Gas souring by thermochemical sulfate reduction at 140 degrees C: Reply Worden RH, Smalley PC, Oxtoby NH AAPG Bulletin, 81(5), 816, 1997 |