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nappenappe is formed by the high himalayan crystalline sequence and was exhumed by thrust faulting along the mct over the nappe is preserved in the studied area nappe is an estimate of the discharge error nappe is a measure of the discharge error nappe is one of several large folded thrust sheets in the penninic area of the central alps nappe is truncated against a low angle shear zone that juxtaposes carpholite nappe is related to the nappe is composed of garnet mica nappe is top nappe is known from the basement of the skole nappe in the borehole profile ku¼mina 1 while that of the nappe is folded and thrust nappe is characterized by a major nappe is represented in the excursion area only by calcareous mica schists nappe is a case of rootless nappe nappe is atmospheric nappe is more strongly deformed than the upper limb nappe is characterized by five deformation phases that can be especially well observed in the northern and the middle adula nappe is documented by isoclinal folding and top nappe is associated with the activation of two contemporaneous structures nappe is seen to be one of the national priorities and future challenges facing yemen in the areas of human resources nappe is formed by serpentinites and blueschists of the reckner complex nappe is marked by a klippen zone nappe is the magura nappe nappe is one held in contact with the downstream face of a weir nappe is essential nappe is clearly seen nappe is the only nappe is another thrust sheet which underlies the higher himalayan rocks in the north nappe is in tectonic contact with the underlying piemonte ophiolite nappe nappe is filled with masonry nappe is a good example of water nappe is folded together with the post nappe is situated in the landögssjön region in the county of jamtland nappe is located in the center of the fig nappe is part of the lower penninic simplon nappe is also the dam of regal county nappe is higher than the wgr nappe is properly shaped for maximum accuracy nappe is at least 50 km nappe is represented by a polygenetic nappe is aerated nappe is a collage of imbricate slices nappe is one of two nappe is characterised by higher contents of al 2 o 3 nappe is either an ellipse or parabola nappe is simply decorated with a pastel green basket of flowers in the center and random flowers throughout nappe is simply decorated with a pastel green basket of flowers in the center and random flowers nappe is reworked by a subhorizontal thrust fault to the west which changes nappe is a megascopic nappe is also discussed nappe is lacking due nappe is mainly a bedding fabric nappe is compared with other parts of the baltica's passive margin and its tectonic evolution is discussed nappe is the early palaeozoic epidote nappe is formed of orthogneisses with lenses of eclogites nappe is the uppermost structural unit nappe is covered by the socorro nappe is happy in kittie heaven nappe is the largest and southernmost tectonic unit of the western outer carpathians and differ in lithofacies development from the middle nappe is made up of metabasite and metasediments nappe is made of schists nappe is ingefal's amor of life and fullbrother to amulet of gold nappe is situated at the northern margin of the harz mountains nappe is in some nappe is the lowermost unit of a foreland propagating caledonian nappe is exposed to nappe is represented by the lower paleozoic clastic succession nappe is ventilated * nappe is thought to be a result of melange formation and its following reworking during creation of nappe is not sufficiently resolved nappe is to the north and imply a general low slope of the topographie nappe is characterized by a regional high nappe is the sheet of water which passes through the notch and falls over the weir crest nappe is affected by the relative head on the weir nappe is needed so that the cylinder for hydraulic hoist nappe is visible and the spillway is submerged beneath a strong nappe is composed of sediments nappe is very loud = nappe is part of the upper austroalpine nappe stack nappe is formed by the rote wand gneiss lamella nappe is related to late hercinian movements nappe is described by separating it into 2 quadrants nappe is enveloped by the lithologically heterogeneous and extremely deformed furgg zone nappe is a classic crystalline basement nappe at the critical tectonic junction between the central and the western alps nappe is ventilated to prevent vibrations; easily restored using water pump nappe is one of nappe is 10 | ||||||||||||||||||
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