Sentence examples for resistive features from inspiring English sources

Structures at 5-km depth (Figure 4c) show more resistive features than those at shallower depths.

The outlined resistive features R1 and R6 (~ 5000 Ω-m) in the western part of the profile at depths of ~ 2 km may relate to the Precambrian basement.

The eastern part of the profile shows highly resistive features denoted as R2, R4 and R5 (5000–10,000 Ω-m) beneath stations 313 324.

In the apparent resistivity pseudo-sections of the TE and TM modes, the demarcation of conductive and resistive features can be easily recognized.

The model responses with and without these resistive features are shown in Additional file 1: Fig. S2a, b along with the observed data.

The first and latter phases are described by the quasi-propagatory approach that represents the inertial, capacitive and resistive features of one-dimensional unsteady flows.

The resistive feature R2 extends beneath the Cambay rift basin and may indicate an extension of these formations toward the western margin.

North of C1, volcanic unit Yaylaçayı Formation (YF) is visible as a resistive feature, over-thrusting the whole sequence (Fig. 4b).

Resistive body south of the NAF was interpreted as the tectonic amalgamation of emplaced oceanic material and intra-oceanic Kösdağ Arc, while on the other side of the fault CPS shows itself as a convex-shaped resistive feature.

The resistive feature R3 (2500–5000 Ω-m) may be due to the felsic-intermediate granulitic composition of igneous intrusives, observed across the Son-Narmada region of central India (Naganjaneyulu and Santosh 2010 and references therein).

The geo-electric section is characterized by several less-resistive to high-resistive features all along the traverse.