Sentence examples for chaotic reflections from inspiring English sources

Exploration seismology has been widely employed to study mass-transport deposits (landslides, glacigenic debris flows, mass flows, etc)., which are usually characterized by chaotic reflections.

The basement with an infinite thickness exhibits chaotic reflections with macro diffractions; this probably due to the compact nature of the basement bedrock.

Basin-filling strata are roughly divided into a lower unit showing discontinuous or chaotic reflections and an upper unit accompanied with transparent and/or thinly laminated continuous reflection patterns.

We define the deformation front as the seafloor trace where either chaotic reflections of the landward slope or the frontal thrust contact coherent, continuous reflections of the incoming plate (Figures 5 and 7).

In many areas, the regional lines display only chaotic reflections around the imbricate thrusts due to their lower resolution.Where a horst block is subducted beneath the base of the landward trench slope, the décollement is localized near the top of the chert layer at the top of the horst (Figure 7).

The specially designed multi-layer perceptron (MLP) neural network-modelled seismic chimneys are usually associated with chaotic reflections on seismic sections with low energy and low trace-to-trace similarity associated with the propagation of fluids through fissures and fractures in strata.

This unit (U3b) consists of a semitransparent, chaotic reflection pattern suggesting mass transport deposition (MTD).

The location of horizon (H1) shows a chaotic reflection and was not correlated and may require further seismic processing to define it.

Small antiform shape is not clearly defined, and the uplift is considered to be related to the local topographic high due to fault and possible gas migration from deeper geology forming a chimney type of structure with chaotic reflection observed below the antiform structure (Figs. 7, 8).

The largest offsets in successive channel floor position occur after periods of significant vertical CF fill ('thalweg plugging' with deposits commonly consisting of lower amplitude, transparent to chaotic seismic reflections).

Aikulola et al. (2010) related these chaotic and distorted reflections beyond 3 s two-way time most especially, at the footwall of regional faults to the onset of overpressure.