GeoLines (Praha), 7 (1998) 3 Salt Plugs in the Eastern Zagros, Iran: Results of Regional Geological Reconnaissance Pavel BOSÁK1, Josef JAROŠ2, Jiøí SPUDIL3, Petr SULOVSKÝ4 and Vladimír VÁCLAVEK5 1 Geological Institute, Czech Academy of Sciences, Rozvojová 135, 165 02 Praha 6, Czech Republic; e-mail:
[email protected] 2 Institute of Geology and Paleontology, Faculty of Natural Sciences, Charles University, Albertov 6, 128 43 Praha 2, Czech Republic 3 GET Ltd., Korunovaèní 29, 170 00 Praha 7, Czech Republic, e-mail:
[email protected] 4 Department of Mineralogy, Petrology and Geochemistry, Masaryk University, Kotláøská 2, 611 37 Brno, Czech Republic; e-mail:
[email protected] 5 Pod Spoøilovem 2779, 141 00 Praha 4, Czech Republic ABSTRACT. Regional reconnaissance study of salt plugs cov- temperature is needed to start the glacier flow. Unbreached ered the area of about 50,000 square kilometers (coordinates salt plugs were discussed. Their occurrence is highly limited. It 53o50' to 56o30' E and 26o30' to 28o15‘N). Altogether 68 salt is shown, that “collapse structures” are connected rather with plugs were characterized from the viewpoint of their position other processes than solution collapse after leached salt. Tec- in the structure of area, morphological and evolution stages, tonic effects, erosion and pedimentation took part substantial- rock content and mineralization. ly in the formation of cauldrons. Linear cauldrons are connect- Prevailing amount of plugs lies in the flanks of anticline ed with tension regime in the apical zone of anticlines. Primary folds and is bounded to fold plunges and sigmoidal bends, where and secondary rim synclines have not been yet detected.