![Structural geology . Fig. 49. Generalized fan fold or normal anticlinorium of central massif of the Alps. After Heim. folds are conveniently designated drag folds. The position of theiraxial planes is controlled Structural geology . Fig. 49. Generalized fan fold or normal anticlinorium of central massif of the Alps. After Heim. folds are conveniently designated drag folds. The position of theiraxial planes is controlled](https://c8.alamy.com/zooms/9/5b92b5a5ea674d9db51add139a7ed1d5/2awex61.jpg)
Structural geology . Fig. 49. Generalized fan fold or normal anticlinorium of central massif of the Alps. After Heim. folds are conveniently designated drag folds. The position of theiraxial planes is controlled
![Partitioned tectonic shortening, with emphasis on outcrop-scale folding and flattening, Pindos fold-and-thrust belt, Peloponnese, Greece Partitioned tectonic shortening, with emphasis on outcrop-scale folding and flattening, Pindos fold-and-thrust belt, Peloponnese, Greece](https://cdnsciencepub.com/cms/10.1139/cjes-2018-0210/asset/images/large/cjes-2018-0210f1.jpeg)
Partitioned tectonic shortening, with emphasis on outcrop-scale folding and flattening, Pindos fold-and-thrust belt, Peloponnese, Greece
![Structural geology . folds with referenceto the adjacent competent beds tells the direction of the differen-tial movement. The axial planes are nearly parallel to cleavage(see pp. 119-120). When this movement is of Structural geology . folds with referenceto the adjacent competent beds tells the direction of the differen-tial movement. The axial planes are nearly parallel to cleavage(see pp. 119-120). When this movement is of](https://c8.alamy.com/comp/2AWEHBC/structural-geology-folds-with-referenceto-the-adjacent-competent-beds-tells-the-direction-of-the-differen-tial-movement-the-axial-planes-are-nearly-parallel-to-cleavagesee-pp-119-120-when-this-movement-is-of-great-proportionsthe-axial-planes-of-the-minor-folds-may-become-so-rotated-as-togive-the-abnormal-type-of-composite-fold-beds-of-shale-mayindicate-a-differential-movement-of-quartzite-beds-above-and-be-low-in-the-direction-shown-on-diagram-56-drag-folds-115-the-position-of-the-major-fold-is-inferred-from-the-differentialmovement-indicated-by-the-minor-folds-the-major-fold-may-int-2AWEHBC.jpg)
Structural geology . folds with referenceto the adjacent competent beds tells the direction of the differen-tial movement. The axial planes are nearly parallel to cleavage(see pp. 119-120). When this movement is of
![Drag folds develop along normal faults and reverse faults. They can be... | Download Scientific Diagram Drag folds develop along normal faults and reverse faults. They can be... | Download Scientific Diagram](https://www.researchgate.net/profile/David-Tanner-11/publication/263807576/figure/fig5/AS:1080242965872648@1634561401442/Comparison-of-trishear-in-A-compressional-and-B-extensional-regimes-The-fault-dip-is_Q320.jpg)
Drag folds develop along normal faults and reverse faults. They can be... | Download Scientific Diagram
![Extensional fault-propagation folding in mechanically layered rocks: The case against the frictional drag mechanism - ScienceDirect Extensional fault-propagation folding in mechanically layered rocks: The case against the frictional drag mechanism - ScienceDirect](https://ars.els-cdn.com/content/image/1-s2.0-S0040195112003009-gr1.jpg)
Extensional fault-propagation folding in mechanically layered rocks: The case against the frictional drag mechanism - ScienceDirect
![The brittle and ductile components of displacement along fault zones | Geological Society, London, Special Publications The brittle and ductile components of displacement along fault zones | Geological Society, London, Special Publications](https://www.lyellcollection.org/cms/10.1144/SP439.21/asset/6a955b4a-da29-4c7c-96e0-04a6177594a5/assets/graphic/sp439-1394f01.jpeg)
The brittle and ductile components of displacement along fault zones | Geological Society, London, Special Publications
![Structural geology . Fig. 56. Figure showing differential movement between competent beds on limbsof a fold with the development of minor drag folds between them. districts it has been possible, by studying Structural geology . Fig. 56. Figure showing differential movement between competent beds on limbsof a fold with the development of minor drag folds between them. districts it has been possible, by studying](https://c8.alamy.com/comp/2AWEGT7/structural-geology-fig-56-figure-showing-differential-movement-between-competent-beds-on-limbsof-a-fold-with-the-development-of-minor-drag-folds-between-them-districts-it-has-been-possible-by-studying-the-minute-crenula-tions-of-the-softer-beds-to-determine-the-differential-movementof-the-controlling-strata-on-each-side-and-thereby-to-obtain-anotion-of-the-position-of-the-next-larger-unit-of-structure-thishas-led-to-a-study-of-still-larger-units-and-so-on-in-the-mar-quette-district-of-michigan-the-slate-beds-are-folded-in-the-mannerto-be-expected-from-the-control-of-the-harder-quart-2AWEGT7.jpg)
Structural geology . Fig. 56. Figure showing differential movement between competent beds on limbsof a fold with the development of minor drag folds between them. districts it has been possible, by studying
![Drag folds develop along normal faults and reverse faults. They can be... | Download Scientific Diagram Drag folds develop along normal faults and reverse faults. They can be... | Download Scientific Diagram](https://www.researchgate.net/profile/David-Tanner-11/publication/263807576/figure/fig4/AS:1080242965876739@1634561401392/Drag-folds-develop-along-normal-faults-and-reverse-faults-They-can-be-classified-into_Q640.jpg)
Drag folds develop along normal faults and reverse faults. They can be... | Download Scientific Diagram
![PDF] Quantitative kinematic flow and strain analyses of the drag folds associated to the Sananadaj- Sirjan HP-LT metamorphic belt, southwestern Iran | Semantic Scholar PDF] Quantitative kinematic flow and strain analyses of the drag folds associated to the Sananadaj- Sirjan HP-LT metamorphic belt, southwestern Iran | Semantic Scholar](https://d3i71xaburhd42.cloudfront.net/dd6282e53633a06540f0d916ac7c5ddbf9973ab8/4-Figure1-1.png)
PDF] Quantitative kinematic flow and strain analyses of the drag folds associated to the Sananadaj- Sirjan HP-LT metamorphic belt, southwestern Iran | Semantic Scholar
![Drag folds develop along normal faults and reverse faults. They can be... | Download Scientific Diagram Drag folds develop along normal faults and reverse faults. They can be... | Download Scientific Diagram](https://www.researchgate.net/profile/David-Tanner-11/publication/263807576/figure/fig4/AS:1080242965876739@1634561401392/Drag-folds-develop-along-normal-faults-and-reverse-faults-They-can-be-classified-into.png)