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...above we find the dominant angel at NE quadrant is 39 – 42 degree, and at NW quadrant is 333–336°. 39–42° and 333–336° area form angel 60°, to

...tight oil in the Permian saline lacustrine dolomitic rock, Junggar Basin, NW China: Petroleum Exploration and Development Online, vol. 39, no. 6, p. 657

...adients caused by the different densities of the nonwetting (''&rho;''_nw) and wetting (''&rho;''_w) phases (right).]] :<math>P_\mathrm{c} = (\rho_\mathrm{w} - \rho_\mathrm{nw}) g h</math>, or

[[File:CovenantFieldFig2.png|thumb|400px|{{figure number|3}}A NW-SE trending cross section showing the Covenant oil field structure, Paxton

:<math>P_b = (\rho_w - \rho_{nw})gh</math> * ρw and ρnw are the specific gravities of the wetting and nonwetting phases respectivel

The '''Main Central Thrust''' is one of the north-dipping and NW—SE strike [[thrust fault]]s along the [[Himalaya]]<ref>Upreti, B. N., 199 ...leading edge of the Greater Himalayan Crystalline complex revealed in the NW Indian Himalaya: Implications for the evolution of the Himalayan orogen: Ge

:<math>P_b = (\rho_w - \rho_{nw})gh</math><br> where P_b is the buoyancy pressure; ρ_w and ρ_nw are the specific gravities of the wetting and nonwetting phases respe

....8% R_o.<ref name=ch11r3>Bartenstein, H., 1980, Coalification in NW Germany: Erdöl und Kohle-Erdgas-Petrochemie: vol. 33, p. 121–125.</ref>

...merate, Block 16/17, North Sea, in J. R. Parker, ed., Petroleum geology of NW Europe: Proceedings of the 4th Conference: Geological Society (London), p.

| rowspan=4 | NW Offshore || Eocene || Carbonate || Jedier || U. Cretaceous || Argub || rows

...retaceous/Eocene source-rocks which have fed the Palmyrides, Euphrates and NW corner hydrocarbon fields are potential shale oil and gas opportunities.<re

.... Underhill, A. J. Hewett, and J. E. A. Marshall, eds., Paleozoic plays of NW Europe: Geological Society (London) Special Publication 471, [https://doi.o

...e Late Ordovician, it is possible that part of Armorica had rifted off the NW Gondwanan margin; however, Robardet<ref name=Robardet_2003 /> casted doubts ...a number of minor, semi-independent blocks such as Apulia, Taurides, Iran (NW and Central), Sanandaj Sirjian, Heland, and Northern Tibet.<ref name=Rubane

...015, Geology of the Sarnoo Hills, eastern rift-margin of the Barmer Basin, NW India: Basin Research, v. 27, p. 636–655.</ref>; Dolson et al., 2015<ref

...er, 2012, Characterization of microbial activity in pockmark fields of the NW Barents Sea: Marine Geology, v. 332-334, p. 152–162.</ref>; Ostanin et al

The Thrace Basin is a SE-NW trending trough controlled by fault systems, and the sediment fill reaches ...stimations for natural gas and associated condensates in the Thrace Basin, NW Turkey: Applied Geochemistry, v. 20, no. 11, p. 2017–2037.</ref> has anal

...P., and Goodarzi, M. G. H., 2010, Structure of the Mountain Front flexure (NW Zagros, Iran): Insights from sand box model, in P. Leturmy and C. Robin, ed

...rm-generated sandstone in the Miocene Miri Formation, Seria Field, Brunei (NW Borneo), in R. J. Knight and J. R. McLean, eds., Shelf Sands and Sandstones

...ult zone thickness versus displacement in the Permo-Triassic sandstones of NW England: Journal of the Geological Society, v. 151, p. 17–25.</ref> <ref