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- | isbn = 0-89181-602-X ...wells represent Marmaton wells; triangles, Mississippian wells; and large X's, study wells. The rest of the oil wells produce from the Morrow. Each uni3 KB (429 words) - 14:19, 11 April 2022
- ...sion-analysis fig1.png|300px|thumb|{{figure number|1}}Linear regression of x-on-y. Note the negative slope corresponding to a negative correlation. The ...tween two quantities or variables, that is, the tendency for one variable, x, to increase or decrease as the other, y, increases or decreases, in a stra9 KB (1,366 words) - 16:37, 19 January 2022
- ...al in a carbonate rock can be determined by [[SEM, XRD, CL, and XF methods|X-Ray Diffractometry]]. Carbonates more rich in calcite and/or aragonite are708 bytes (95 words) - 20:42, 7 July 2016
- | isbn = 0-89181-602-X ...y'') are available from the seismic data cube, ''t''(''x, y'') and ''a''(''x, y''). The traveltimes form a time structure map, and the amplitudes are a7 KB (1,117 words) - 17:51, 25 January 2022
- | isbn = 0-89181-602-X ...seismic data (with time axis) converted to a depth cube using a ''V'' ( ''X, Y, Z'' ) velocity model2 KB (320 words) - 19:10, 27 January 2022
- | isbn = 0-89181-602-X ...H<sub>y</sub>. (See [[Magnetotellurics survey measurements]].) The E<sub>x</sub> component is oriented perpendicular to the E<sub>y</sub> component. T5 KB (706 words) - 15:11, 31 January 2022
- | isbn = 0-89181-602-X ...g-reservoir-system-quality-and-performance_fig9-36.png|Figure 1]]. Use the x-axis for the resistivity (R<sub>t</sub>) scale and the y-axis for the poros6 KB (878 words) - 16:16, 5 April 2022
- ...evelopment Online, vol. 39, no. 6, p. 657–667.</ref><ref>Zhang, Y., X. Qi, X. Cheng, and Z. Luo, 2007, Approach to sedimentary environment of late carbo ...p. 48–60.</ref><ref name=Ymg2019b>Yang, Z., C. Zou, L. Hou, S. Wu, S. Lin, X. Luo, Z. Zhao, J. Cui, and S. Pan, 2019b. Division of fine-grained rocks an6 KB (850 words) - 17:56, 20 December 2023
- | isbn = 0-89181-602-X1 KB (154 words) - 22:26, 31 January 2022
- | isbn = 0-89181-602-X ..., temperature) can be measured, so we have temperature as a function of (''x, y, z''). As we move around the room to other points, the temperature chang5 KB (813 words) - 19:05, 27 January 2022
- * X-ray diffractometry (XRD) * X-ray fluoroscopy (XF)11 KB (1,477 words) - 15:25, 24 January 2022
- | isbn = 0-89181-602-X1 KB (179 words) - 16:23, 13 April 2022
- | isbn = 0-89181-602-X1 KB (166 words) - 16:13, 13 April 2022
- | isbn = 0-89181-602-X1 KB (182 words) - 17:24, 2 February 2022
- | isbn = 0-89181-602-X1 KB (179 words) - 20:54, 31 March 2022
- | isbn = 0-89181-602-X1 KB (187 words) - 17:53, 25 January 2022
- 3.Hao, F., X. Zhou, Y. Zhu, and Y. Yang, 2011, Lacustrine source rock deposition in resp 4.Tian, J., F. Hao, X. Zhou, and H. Zou, 2017, Distribution, controlling factors, and oil-source8 KB (1,251 words) - 15:51, 14 March 2022
- | isbn = 0-89181-602-X ...) + \mbox{MF}_{2}(\mbox{MW}_{2}) + \cdots \mbox{MF}_{\rm x}(\mbox{MW}_{\rm x})</math>7 KB (979 words) - 15:24, 17 February 2022
- | isbn = 0-89181-602-X1 KB (179 words) - 21:39, 4 February 2022
- | isbn = 0-89181-602-X2 KB (184 words) - 18:52, 31 January 2022
- | isbn = 0-89181-602-X1 KB (191 words) - 18:46, 12 April 2022
- | isbn = 0-89181-602-X ...ntersection of formation temperature (from Y-axis) and R<sub>w</sub> (from X-axis), find the NaCl concentration (in ppm) by reading diagonal line labels5 KB (714 words) - 15:19, 13 September 2022
- | isbn = 0-89181-602-X1 KB (189 words) - 18:53, 4 February 2022
- | isbn = 0-89181-602-X1 KB (176 words) - 17:29, 13 April 2022
- | isbn = 0-89181-602-X ...to the amount of anomalous mass. Size differences in three dimensions are X<sup>3</sup> functions. [[:file:applying-gravity-in-petroleum-exploration_fi4 KB (551 words) - 14:51, 31 January 2022
- | isbn = 0-89181-602-X2 KB (211 words) - 17:54, 2 February 2022
- | isbn = 0-89181-602-X2 KB (195 words) - 15:17, 17 February 2022
- | isbn = 0-89181-602-X2 KB (212 words) - 14:19, 13 April 2022
- | isbn = 0-89181-602-X2 KB (207 words) - 18:56, 16 February 2022
- | isbn = 0-89181-602-X2 KB (230 words) - 19:23, 24 January 2022
- | isbn = 0-89181-602-X2 KB (220 words) - 16:10, 10 February 2022
- ...dependent variables(s). It is related linearly to the second set, denoted x, called the independent variable(s). (For details of multiple and multivari ...problem from P, the number of original quantities ''x''<sub>1</sub>, ... ''x''<sub>P</sub>, to fewer combinations of those quantities, called ''principa16 KB (2,349 words) - 15:46, 19 January 2022
- | isbn = 0-89181-602-X ...eologic time as the Y-axis and distance across the area of interest as the X-axis. A [[dip]]-oriented chronostratigraphic chart should be made. But we a5 KB (599 words) - 18:54, 4 February 2022
- | isbn = 0-89181-602-X2 KB (215 words) - 15:43, 23 February 2022
- | isbn = 0-89181-602-X2 KB (227 words) - 13:38, 5 April 2022
- | isbn = 0-89181-602-X2 KB (239 words) - 14:58, 4 February 2022
- | isbn = 0-89181-602-X ...oil: Organic Geochemistry, vol. 9, p. 1–10., 10., 1016/0146-6380(86)90077-X</ref> [[:file:oiloil-and-oilsource-rock-correlations_fig8-38.png|Figure 3]]6 KB (775 words) - 21:49, 15 February 2022
- | isbn = 0-89181-602-X # Enter the X-axis at percent pore volume (S<sub>w</sub> value).6 KB (898 words) - 16:21, 4 April 2022
- | isbn = 0-89181-602-X2 KB (229 words) - 16:31, 4 April 2022
- | isbn = 0-89181-602-X2 KB (266 words) - 15:45, 31 March 2022
- | isbn = 0-89181-602-X2 KB (250 words) - 17:52, 31 January 2022
- | isbn = 0-89181-602-X2 KB (242 words) - 15:48, 1 March 2022
- | isbn = 0-89181-602-X2 KB (261 words) - 18:12, 29 March 2022
- | isbn = 0-89181-602-X2 KB (251 words) - 18:32, 6 April 2022
- | isbn = 0-89181-602-X2 KB (244 words) - 13:38, 5 April 2022
- | isbn = 0-89181-602-X2 KB (248 words) - 17:04, 28 March 2022
- | isbn = 0-89181-602-X2 KB (260 words) - 16:31, 13 April 2022
- | isbn = 0-89181-602-X2 KB (258 words) - 18:41, 31 March 2022
- | isbn = 0-89181-602-X2 KB (298 words) - 18:35, 25 January 2022
- | isbn = 0-89181-602-X2 KB (268 words) - 15:18, 31 January 2022