- structure,
whereas an
anticline is the
inverse of a syncline. A
synclinorium (plural
synclinoriums or synclinoria) is a
large syncline with
superimposed smaller...
-
situated in the
western wing of the
Yangozero synclinorium, the
second largest (after the
Onega synclinorium) on the
Karelian Craton.[citation needed] Vottovaara...
-
Central Thrust" (MCT). The
Tethys Himalaya is an
approximately 100-km-wide
synclinorium formed by
strongly folded and imbricated,
weakly metamorphosed sedimentary...
- The Aye
Formation is a
geologic formation in the
Dinant synclinorium, Ardennes, Belgium. It is part of the
Condroz Group, at the base of the
middle Famennian...
- D.; Banks, M. R. (1973). "Ordovician
stratigraphy of the
Florentine Synclinorium,
southwest Tasmania" (PDF).
Papers and
Proceedings of the
Royal Society...
-
veinlets along fractures, joints, and
minor faults within the
Katanga synclinorium.
Uraninite mineralization occurred 630 Ma ago, when
uraniferous solutions...
- units: the
southern peneplain, the
Inini synclinorium, the
central granite m****ifs and the
northern synclinorium. The
southern peneplain consists of a set...
-
slide to form
talus slopes. The M****anutten
Sandstone is
folded in a
synclinorium, and it
outcrops at the
ridge tops. M****anutten Peak
Green Mountain Three...
-
events in the
Nismes – Vireux-Molhain area,
southern border of the
Dinant Synclinorium (Belgium,
northern France)".
Geologica Belgica. 22 (1–2): 7–33. doi:10...
- M****if, and
Stavelot M****if, from
north to
south respectively The
Dinant Synclinorium The
Ardennes Anticlinorium The
Hercynian complexes The
Silurian Sambre...
