عنوان مقاله :
In-situ stress regime in the Asmari reservoir of the Zeloi and Lali oil fields, northwest of the Dezful embayment in Zagros fold-thrust belt, Iran
پديد آورندگان :
Hossein، Talebi Department of Geology - Faculty of Earth Sciences - Shahid Beheshti University - Tehran , Ahmad، Alavi Department of Geology - Faculty of Earth Sciences - Shahid Beheshti University - Tehran , Shahram، Sherkati NIOC Exploration Directorate - Tehran , Mohammad Reza، Ghassemi Research Institute for Earth Sciences - Geological Survey of Iran - Tehran , Alireza، Golalzadeh National Iranian South Oil Company - Tehran
كليدواژه :
In situ stress , Breakouts , Induce fractures , Dezful embayment , Lali , Zeloi , Stress regime
چكيده لاتين :
This paper analyzes in-situ stress field in the Asmari formation with in the complex structures
of the Zeloi and Lali oilfields located in the Dezful embayment, SW Iran. The orientation of
the maximum horizontal stress, SHmax is determined on the basis of compressive borehole
breakouts and drilling-induced tensile fractures observed in eight oil wells, in which we
focus on well-log based methods and drilling data to estimate stress magnitudes. In situ stress
magnitude in studied fields obtained from 1D mechanical earth modeling in key wells. The
maximum horizontal stress trend in this area is NE–SW in accordance with the World Stress
Map however a stress perturbation has been recognized in some wells of the Lali field which
is approximately perpendicular to the expected direction of the maximum horizontal stress.
In situ stress magnitudes in the Lali oil wells are consistent with a strike-slip regime, while
in the Zeloi oilfield, normal faulting regime is estimated. The observed strike-slip and normal
faulting regime in the Lali and Zeloi wells respectively, Supports the idea that the role of
overburden stress magnitude is higher than the horizontal stresses. Undoubtedly, the structural
position of the wells, structural framework, faults location, fold geometry, pore pressure
changes and mechanical properties of rocks are main factors and have played an important
role in stress condition and in situ stress regime in these two hydrocarbon structure.