چهل و دومین همایش ملی علوم زمین (نمایه ISC)

تاریخ برگزاری : 01 اسفند ماه 1402


برگزار شده توسط : سازمان زمین شناسی و اکتشافات معدنی کشور، مرکز پژوهشی زمین شناسی پارس آرین زمین

مدل سازی دوبعدی داده های میدان زمین گرمایی سبلان با استفاده از دو مجموعه برنامه REBOCC و MT2DInvMatlab

نویسندگان :

غلامعباس فنایی خیرآباد

چکیده

In this paper the modelling of Magnetotelluric (MT) data of Sabalan geothermal was undertaken to evaluate the resistivity models at the shallow depth and in the upper layers of thermal reservoir. Fo this purpose, a profile with the length of approximately 10 km include seven MT measuring stations selected and two-dimensional (2D) modelling source codes named the reduced based Occam (REBOCC) and the MT2DIinvMatlab inversion has been applied. The data points were carefully selected between frequency range 0.01- 132 Hz. In order to explain the mechanism of the geothermal reservoirs, some global conceptual model is presented that each of these models is valid for the interpretation of geothermal phenomena in a particular area. MT2DInvMatlab inversion source code prepared based on the finite elements (FEM) method for forward modelling. Inversion parameters as an Input file and appropriate mesh blocks design should prepared before starting the modelling and inversion. After setting up the model parameter, 2D inversion of the Sabalan magnetotelluric data has been performed using smoothness–constrained least square methods with a spatially regularization parameter estimation. The ACB (Active Constraint Balancing) algorithm employed to stabilize the model. Both apparent resistivity and phase data has been used to have model with minimum misfit for TM mode data. REBOCC is the second inversion program using for 2-D modeling. The resulting models reveal the presence of a resistive cover layer (Cap-rock) underlain by an anomalous conductive layer and other geological structures such as fluid-filled faults in about 500-1000 m below the ground surface. A very low resistivity (3-5 ohm-m) feature at the depths below 2000 m, bounded by two more resistive (100-500 ohm-m) features that interpreted as the main reservoir of the geothermal system in the area. At shallow depths, the resistivity model obtained from the MT data is consistent with the general conceptual resistivity model proposed for high-temperature geothermal systems.

کليدواژه ها

Magnetotellurics, Geothermal exploration, REBOCC, MT2DInvMatlab, Sabalan

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, 1402 , مدل سازی دوبعدی داده های میدان زمین گرمایی سبلان با استفاده از دو مجموعه برنامه REBOCC و MT2DInvMatlab , چهل و دومین همایش ملی علوم زمین (نمایه ISC)


چهل و دومین همایش ملی علوم زمین (نمایه ISC)
تاریخ برگزاری : 01 اسفند ماه 1402
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