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The facies were identified based on regional facies distribution, well log characteristics, lithologic association, and well correlation; d West-to-east cross section showing the residual pressure (difference between formation pressure and hydrostatic pressure) distribution and permeability of the Chang7 source rock interval (Section location in a) (After Yao et al. 2013).
The green and red dots denote oil and gas production, respectively; b Properties of Chang7 source rock interval in L189 well (After Yang et al. 2013); c West-to-east cross section showing the stratigraphic variation of the Chang 7 source rock interval across the Xifeng Oilfield (Section location in a).
The Hybrid Plays were identified based on the lithofacies, geochemistry, and production test results; c West-east cross section showing the Es3 sedimentary facies variation (Section location in a), compiled and reinterpreted from data published by Zhang et al. (2008b) and Jiu et al. (2013).
Figure 2 East-west cross sections (keograms) of 630-nm airglow images obtained at (a) Sata and (b) Darwin on 8 August 2002.
The local time is 9 h ahead of UT. Figure 2 shows the east-west cross sections (keograms) of the 630-nm airglow images obtained at (a) Sata and (b) Darwin on 8 August 2002.
The inclined cluster of hypocenters to the east shown in the cross section of Figure 4c appears as a thick slab.
Four east-west vertical cross sections are shown in (b) to (e).
(b), (c), (d), and (e) East-west vertical cross sections are shown.
The cross section was selected roughly in an east-west direction to identify the velocity variation along the coastline, effects of the topography, and alluvial creek beds.
A section of Ringway 1 known as the East Cross Route was built to motorway standards in the late 1960s and early 1970s and designated as the A102(M).
The geoelectrical cross section (a) shows gradual decrease in the resistivity values toward the east in both the shallow and main aquifers.
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