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Geophysical Inversion×تفسیر لرزه‌ای بازتابی×
حوزهعلوم زمینعلوم زمین
خانوادهProcess / pipelineProcess / pipeline
سال پیدایش19631960s
پدیدآورTikhonov and TarantolaDobrin and Savit
نوعdata assimilation pipelinegeophysical imaging pipeline
منبع بنیادینTarantola, A. (1987). Inverse Problem Theory: Methods for Data Fitting and Model Parameter Estimation. Elsevier. link ↗Yilmaz, Ö. (2001). Seismic Data Analysis: Processing, Inversion, and Interpretation of Seismic Data. Society of Exploration Geophysicists. DOI ↗
نام‌های دیگرinverse problem solving, parameter estimation, model-data fittingseismic interpretation, seismic data analysis
مرتبط35
خلاصهGeophysical inversion is the process of using observed geophysical data to estimate subsurface properties and structures. Formalized by Tikhonov (1963) and expanded by Tarantola (1987), this mathematical framework solves the inverse problem: given measurements (gravity, magnetics, seismic, electrical), what subsurface model produced them? Inversion is central to all quantitative geophysics and enables extraction of detailed subsurface information from surface or borehole measurements.Seismic reflection interpretation is the process of extracting meaningful geological information from seismic survey data, which is collected by recording elastic waves reflected from rock layers beneath the surface. Developed and systematized in the mid-20th century, this method is foundational in petroleum exploration and engineering geology. It enables geoscientists to image subsurface structures, identify hydrocarbon prospects, and assess hazards without drilling.
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ScholarGateمقایسهٔ روش‌ها: Geophysical Inversion · Seismic Reflection Interpretation. بازیابی‌شده در 2026-06-17 از https://scholargate.app/fa/compare