Sentence examples for main boundaries of from inspiring English sources

Figures 3 and 4 summarise the main boundaries of the consumption and territorial systems.

In a longwall coal mine two long, horizontal and permanent tunnels known as gate roads are cut into the coal seam to form the main boundaries for a large rectangular block of coal, known as a longwall panel.

The Anko section along the Aoki River (Figure 1b) exhibits the main boundary fault of the MTL strikes NNE-SSW with a subvertical dip, which separates the Ryoke and the Sambagawa belts (Figure 2; Kawamoto et al. 2013a).

An attempt with the Canny method failed by extraction of three main boundaries with some isolated objects as boundaries.

Tectonic structures define the main boundaries between compartments, helping the understanding of why productive and non-productive wells were found in apparently similar structural settings within the Torre Alfina field.

The 50 km long stretch of the valley examined encompasses the mountain front from north of the Main Boundary Thrust (MBT) to south of the Himalayan Frontal Thrust (HFT).

This paper is summarizing the key facts for the assessment and showing the evaluation on the basis of two simulated cases including sensitivity analysis of main boundary conditions.

The negative residual anomalies with typical minima up to −2 mgal and locally up to < −3.5 mgal are located in the northwest, in the Buntsandstein formation of the Pfälzer Wald, directly to the east of the western Main Boundary fault (AN1a), to the east of the westernmost W-dipping fault (AN1b) within the URG and in the central part of the study area (AN2 to AN4; Figure 6a).

The ∼ 500 Ma detrital grains are from rocks in the frontal portions of the fold-thrust belt north of the Main Boundary thrust as well as directly in the footwall of the Main Central thrust in the hinterland.

This occurs beyond 3 s two-way time (3800 m), especially at locations corresponding to the footwall of main boundary faults on seismic.

The presence of strong subsurface reflectors and contacts between geologic bodies of different seismic properties at the footwall of the main boundary fault (beyond 3 s two-way time) is suggested as the probable causes of this multiple effect.