After inter-continental collision orogeny (Late Triassic to Early Jurassic), Dabashan orocline
continue reshaping during Late Jurassic to Early Cretaceous, proved by the sediment sequence and strata unconformity (Dong et al.
Arc-continent collision and orocline
formation: closing of the Central American seaway.
The Central Iberian arc, an orocline
centered in the Iberian Massif and some implications for the Variscan belt.
A seismic geotraverse across the Iberian Variscides: orogenic shortening, collisional magmatism and orocline
2010): Geochemical variations in igneous rocks of the Central Andean orocline
(13[grados]S to 18[grados]S): Tracing crustal thickening and magma generation through time and space.
1992, Kinematics of Lugosilesian orocline
accretion wedge in relation to the brunovistulian forland.
triggered lithospheric delamination.
Seismicity and state of stress in the Central Andes: Bolivian orocline
region, in: Third ISAG extended abstracts.
2011): Diachronous post-orogenic magmatism within a developing orocline
in Iberia, European Variscides.
1990: Implications of the north and south Panama thrust belts for the origin of the Panama orocline
2003): Orogenic shortening of the Patagonian orocline
, Syntaxes: the Curvatures of Mountain Belts in Pakistan.