syncline$81113$ - Definition. Was ist syncline$81113$
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Was (wer) ist syncline$81113$ - definition

GEOLOGICAL STRUCTURE
Doming (geology); Fold and fold systems; Anticline and Syncline; Synsedimentary fold; Folded mountains; Youngfold mountains; Fold (geography); Folded mountain; Layer-parallel shortening; Folded strata; Folding (geology); Folded rock; Isocline (geology); Interlimb angle; Ptygmatic folds; Geologic fold; Geological fold; Fold belt
  •  Dextral sense shear folds in [[mylonite]]s within a [[shear zone]], [[Cap de Creus]]
  • Ramp anticline
  • Fold sketch 3D model
  • Kink band folds in the Permian of New Mexico, USA
  • Interlimb angles
  • An anticline in New Jersey
  •  Box fold in [[La Herradura Formation]], [[Morro Solar]], Peru
  • Rainbow Basin [[syncline]] in the [[Barstow Formation]] near [[Barstow, California]]
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  • Rollover anticline
  • Fault-propagation fold

Prüm Syncline         
  • The limestone basins of the Eifel on the line between the [[Lower Rhine Bay]] in the north and the [[Trier Bay]] in the south.
Prümer Kalkmulde; Prüm Basin; Prüm syncline; Prüm Limestone Basin
The Prüm Syncline, Prüm Limestone Basin () or Prüm Basin (Prümer Mulde) is a landscape unit of the southern Limestone Eifel in Germany, which in turn is part of the Eifel mountain range. The region lies in the German state of Rhineland-Palatinate.
Synclinorium         
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TYPE OF GEOLOGICAL FOLD
Synform; Synform.; Synclinorium; Synforms; Synclines; Synclinal fold
·noun A mountain range owing its origin to the progress of a geosynclinal, and ending in a catastrophe of displacement and upturning.
Syncline         
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TYPE OF GEOLOGICAL FOLD
Synform; Synform.; Synclinorium; Synforms; Synclines; Synclinal fold
In structural geology, a syncline is a fold with younger layers closer to the center of the structure, whereas an anticline is the inverse of a syncline. A synclinorium (plural synclinoriums or synclinoria) is a large syncline with superimposed smaller folds.

Wikipedia

Fold (geology)

In structural geology, a fold is a stack of originally planar surfaces, such as sedimentary strata, that are bent or curved during permanent deformation. Folds in rocks vary in size from microscopic crinkles to mountain-sized folds. They occur as single isolated folds or in periodic sets (known as fold trains). Synsedimentary folds are those formed during sedimentary deposition.

Folds form under varied conditions of stress, pore pressure, and temperature gradient, as evidenced by their presence in soft sediments, the full spectrum of metamorphic rocks, and even as primary flow structures in some igneous rocks. A set of folds distributed on a regional scale constitutes a fold belt, a common feature of orogenic zones. Folds are commonly formed by shortening of existing layers, but may also be formed as a result of displacement on a non-planar fault (fault bend fold), at the tip of a propagating fault (fault propagation fold), by differential compaction or due to the effects of a high-level igneous intrusion e.g. above a laccolith.