Structural style & kinematic analysis of deformation in the northern Dezful Embayment, Zagros Fold-Thrust Belt, SW Iran

被引:0
|
作者
Joudaki, Masoud [1 ]
Faghih, Ali [1 ]
Mukherjee, Soumyajit [2 ]
Seraj, Mohammad [3 ]
Soleimany, Bahman [4 ]
机构
[1] Shiraz Univ, Coll Sci, Dept Earth Sci, Shiraz, Iran
[2] Indian Inst Technol, Mumbai 400076, India
[3] Natl Iranian South Oil Co NISOC, Ahvaz, Iran
[4] Natl Iranian Oil Co, Explorat Directorate, Seoul Ave, Tehran, Iran
关键词
Structural style; Folding kinematic; Oilfields; Folding; Subsurface anticline; Northern Dezful Embayment; Zagros; INTERMEDIATE DECOLLEMENT; INCOMPETENT STRATA; LURESTAN REGION; DETACHMENT FOLD; BASIN EVOLUTION; SALT MOVEMENT; PERSIAN-GULF; GEOMETRY; CONSTRAINTS; TECTONICS;
D O I
10.1016/j.marpetgeo.2024.107122
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
A comprehensive understanding of structure and kinematic characteristics of fold and thrust belts provides significant information for hydrocarbon exploration and production. The kinematic evolution and structural style of three subsurface oilfields, Zeloi, Lali and Karun, in the northern part of the Dezful Embayment, a significant petroleum province of the Zagros Fold-Thrust Belt in SW Iran, were investigated using 2D seismic data. Interpretation of the 2D seismic profiles with up to 5 km depth consisting of upper Jurassic to Pleistocene sediments and the balanced cross-sections constructed revealed diverse geometries and kinematics along the oilfields. These results demonstrate that the structural style of the oilfields was controlled by the Gachsaran and Dashtak formations as upper and middle detachment levels, respectively. Tear faults affected the along-strike variations in structural style of the oilfields. Based on the analysis of growth strata, folding evolved as limbs rotated and hinges migrated, beginning in the mid-Miocene. During the later stages of deformation, the initial detachment folds transformed into fault-bend folds.
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页数:18
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