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X-ray diffraction configuration. Knowledge of the wavelength (X) and angle of incidence allows the ''d'' spacing to be calculated.

...ps A and B along both variables <italic>x</italic>₁ and <italic>x</italic>₂. Groups can be distinguished by protecting members of

...aph of disturbed structures in mudflow deposit that caps a slump block. E. X-ray radiograph of core in normally deposited marine clays, which often cap

X-ray diffraction patterns.

...odes in a trace's data values (<italic>x</italic>₁, and <italic>x</italic>₂) within a given formation are related to geology. Node

(a) X-ray fluoroscopy slab photograph and (b) plane light slab photograph of a Pe

Linear regression of ''x''-on-''y''. Note the negative slope corresponding to a negative correlation

...nt. Organic stringers and peat deposits are common in this environment. I. X-ray radiograph of core taken in backswamp deposit. Note the stringers of or

An example of an x-ray spectrum acquired from a shale sample. Individual peaks indicate an ele

...d transmission electron micrograph of a calcium dolomite (Ca1.12Mg0.88(CO2)x) of Eocene age. The prominent modulated structure is typical of sedimentary

...d when misties are averaged. Dots show times of events on seismic lines A, X, and N where those lines intersect line Q. Solid lines show true attitude o

Burial history curve for location X represented by the dot in Figure 2 of [[Basin modeling: identifying and qua

Map with cross sections X-Z and Y-Z showing basinward-stepping geometries exhibited by lobe-shaped sa

...al., 2003]]). Note that both the U.K. and Norway areas are divided into 1° x 1° Quadrants (numbered on map around the SVG), with each quadrant being su