Sentence examples for major tectonic features from inspiring English sources

Topography and major tectonic features of the region surrounding the 2005/07/20 Hatanbulag earthquake.

The electrical structures, their locations, and the major tectonic features in the northwestern Pacific are graphically summarized in Fig. 13.

The red boxes in the inset map outline the area represented in Fig. 1 and Fig. 2. Fig. 2. Topography and major tectonic features of the region surrounding the 2009/01/19 Büsiin Gol earthquake.

It translates widely the CVL direction as the major tectonic feature of the study area trending NE SW.

The thermal springs on the west coast are aligned along this major tectonic feature, i.e., the West Coast Fault (Chandrasekharam [1985]; Minissale et al. [2000]).

However, there is one exception where higher incision rates (~ 6 mm/yr) were calculated upstream of the Darvaz Fault Zone, a major tectonic feature that forms the western boundary of the Pamir.

Compilation of interpretations of magnetic and gravity data showing the major units and tectonic features beneath the pre-Late Carboniferous - Permian basin (Baillieux et al. [2013]).

The major morpho-tectonic features observed in the Andaman Basin are the outerarc, AFB, Invisible Bank (IB), back-arc basin, volcanic arc and Alcock-Sewell seamount complexes, etc. (Fig. 1).

This strike direction is coincident with the major strike direction of tectonic features in the Son Narmada region, and it is close to the strike direction reported in other MT studies in Central India, such as the study of Patro et al. (2005), who obtained N75°E as the strike direction.

As one of the other important tectonic features of the Fergana basin, the major north-dipping reverse faults (North Fergana Fault, NFF) in the north and south-dipping reverse faults (South Fergana Fault, SFF) in the south mark the edges of the basin (Chedia 1986; Judachin 1983; Osmonbetov et al. 1989; Cobbold et al. 1993).

The nonlinear relationship between drainage area and proportion of the incised valley filled is somewhat weaker, but still significant, and major deviations are readily explained in terms of local inherited morphology or tectonic features.