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and tight folds from 30° to 0 Isoclines, or isoclinal folds, have an interlimb angle of between 10° and zero, with essentially parallel limbs.
Kaynak: Fold (geology)

It was so named by the Ohio State University Geological Party, 1967–68, because an isoclinal fold is well exposed on the side of the
Kaynak: Isocline Hill

Lift-off detachment folds are characterized by isoclinal folding in all units, with a tight isoclinal folded weak unit in the anticline
Kaynak: Detachment fold

Canigou Massif the group's metasediments together with the gneisses and the augengneisses were folded into a gigantic flat-lying isoclinal fold.
Kaynak: Canaveilles Group

It shows kilometer-scale isoclinal recumbent folding with thrusting to the South. It comprises a low-grade to non-metamorphic sedimentary
Kaynak: Massif Central (geology)

Mapping by Hausel identified numerous shear structures along with steeply plunging ore shoots associated with isoclinal and open folding
Kaynak: South Pass greenstone belt

Folds can be of the simple open style or of the more compressed isoclinal style, and thrusts may develop in the fold limbs to produce
Kaynak: Glacitectonism

Structurally the belt is composed of overturned west-vergent isoclinal fold trains, separated by thrusts . Deformation intensity is
Kaynak: Emily Ann and Maggie Hays nickel mines

Folds of D1, D2 and D3 rare; D4 isoclinal upright, and D5 and D6 restricted to cleavage formation or small scale interference folds.
Kaynak: Petermann Orogeny

At least three periods of regional deformation have been identified, the most important being large scale isoclinal folding with axes
Kaynak: Thasos

It was a small pod of low-grade nickel sulfide mineralisation hosted in a parasitic isoclinal syncline developed on the 132 Anticline on
Kaynak: Widgiemooltha Komatiite

Most Yellowknife Supergroup metasediments are tightly folded (isoclinal ) or occur in plunging anticline s. 37 Nain province : The Archean
Kaynak: Algoman orogeny

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