Sentence examples for deformational events from inspiring English sources
m Biotite (blue arrow) mineral showing elongated shape possibly as a result of deformation in PL. n Elongated mica (blue arrow) mineral resulting from deformational events under XP.
Strike-slip faults dissected rock masses locally affected by pervasive, pre-existing fractures related to previous deformational events.
Several orogenic or deformational events occurred during the existence of the Tasman Geosyncline, and these episodes folded and crumpled the rock strata.
The Tasman Line, originally defined to represent the eastern limit of Precambrian rocks in Australia, has a complicated geometry in three dimensions, which is related to regional deformational events during the Paleozoic.
The NNE trending, late Jurassic Cretaceous sedimentary basins in the region display a complete structural record to analyze the nature of deformational events, and a unique stratigraphic archive to discern sediment sources and drainage patterns during their evolution.
For this the age of the last deformational event, and slip rates (where possible) are taken into account, but their classification as active or inactive structures is avoided.
The assumption being that the fractures formed in the same homogenous stress field i.e. related to the same deformational event, that the rocks themselves are fairly homogenous, the fractures do not significantly perturb the stress field in their vicinity and also that the structures have not rotated significantly since their initiation (Ramsay and Lisle 2000).
We evaluate the new limiters using a deformational flow test case for advection on the surface of the sphere.
Meta-sedimentary and igneous rocks preserved in the hanging wall of the Paralana Fault, northern Mount Painter Province, record a protracted (ca. 1600 Myr) multi-staged metamorphic and poly-deformational evolution related to Mesoproterozoic and Palaeozoic orogenic events.
Common structural features of wackes include repeated graded bedding and such deformational features as folds and deformed bedding, which appear to have formed soon after deposition; cross bedding is absent.
TDC formed by different deformational mechanisms have been divided into three deformation series and ten classes (Ju and Li 2009; Figs. 3, 4, 5).
