The phrase "active thrust" is correct and usable in written English.
It can be used in contexts related to physics, engineering, or aerodynamics, where it refers to the force exerted by an engine or propulsion system.
Example: "The rocket achieved a significant increase in speed due to the active thrust generated by its engines."
Alternatives: "propulsive force" or "dynamic thrust".
These observations also provide a model for recognizing active thrust faults in Pakistan, for targeting trenches across these faults that could expose prehistoric ruptures, and for predicting the distribution of potential damage associated with seismogenic rupture of these faults.
The solutions for the horizontal and vertical seismic coefficients are proposed, which allow one to determine the intensity of the active thrust and its inclination δ with respect to the horizontal.
The reason may that, at the point of sudden change, the direction of Q v changes for critical active thrust.
Later, Greco [5] developed an analytical solution to determine the static and pseudo-static active thrust on walls with bilinear backface.
The sequence matches the well-known tectonic settings of the area, characterized by a northward verging active thrust front buried under thick alluvial deposits of the Po River plain, with little evidence at the surface (Burrato et al. 2012).
It can be seen from Fig. 5 that for ω s H/V s = 0.5, the critical condition for active thrust occurs when Q v acts downward for low intensity motions (low range of a h0/g).
These profiles were used to model topographic growth and perturbation of fan slopes by active thrusting and fault-propagation folding by Boundary Element Method based dislocation modelling.
Avouac, J. P., Tapponnier, P., Bai, M., You, H. & Wang, G. Active thrusting and folding along the Northern Tien Shan and late Cenozoic rotation of the Tarim relative to Dzungaria and Kazakhstan.
The majority of these topics were covered to variable degrees in the field of breast cancer, with educational sessions focusing on current controversies and future directions, and scientific sessions filling in the gaps between our current standards and the active thrusts of research.
Some distinctive examples are: in the eastern extremity of NE Himalaya across the Dibang River valley, the NW-SE trending mountain front is attenuated by the active Mishmi Thrust that has thrust the Mishmi crystalline complex directly over the alluvium of the Brahmaputra plains.
Though in the past it was recognized as a low-activity thrust fault, our present survey has revealed that it has been active with a predominantly right-lateral strike-slip with thrust component.
