![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
![High-angle reverse fault with drag folds: Folding and faulting on the west ridge of Mount Evan-Thomas, Opal Range, Peter Lou… | Geology, Geology rocks, Mineralogy High-angle reverse fault with drag folds: Folding and faulting on the west ridge of Mount Evan-Thomas, Opal Range, Peter Lou… | Geology, Geology rocks, Mineralogy](https://i.pinimg.com/474x/d8/84/27/d88427ade66b9f81fc67a15af241d37d.jpg)
High-angle reverse fault with drag folds: Folding and faulting on the west ridge of Mount Evan-Thomas, Opal Range, Peter Lou… | Geology, Geology rocks, Mineralogy
![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)
Drag folds develop along normal faults and reverse faults. They can be... | Download Scientific Diagram
![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)