Impact of Irregularities of 3D Seismic Geometry on Subsurface Imaging

نویسندگان

  • Singh U. P
  • Ram Kumar
چکیده

3D seismic data acquisition brought a sea change in subsurface imaging. The bridge between geology and seismic is P/S wave velocity of different subsurfaces/lithology. The technique has acquired prime importance due to its inherent strength of determining seismic velocity/amplitudes of the different medium. Lithological variations estimations is possible due to proper Vp/Vs ratio or either velocity alone. Success of advance seismic studies solely depends on accurate subsurface mapping. 3D seismic subsurface image is biased to a great extent by the acquisition geometry, as it affects lateral & vertical velocities. Thus a proper evaluation of the influence of the acquisition geometry on image quality, in areas with complex geology, needs to be carried out. The acquisition geometry footprint is the cumulative effect of azimuthal fold variations across the near offsets, source-receiver directivity, and subsurface illumination irregularities. The ideal 3D acquisition geometry called “full 3D” is the one in which the whole sub-surface area should be covered with regular source positions, and recorded in receiver positions covering the whole acquisition area. Each receiver position is to be covered by source position as well. In 3D seismic survey the choices of acquisition geometry is governed by geological objectives. The optimization of acquisition geometry arises out of resource constraints / cost. The impact of offsets, azimuths, inherent acquisition footprint needs to be understood while optimizing these acquisition parameters/geometry. Obstructions, environmental objectives, economic constraints and many other factors cause irregularity and sparse data sampling. This needs to be studied before geometry optimization as demography is altering at a rapid pace with urbanization. The irregularities are observed in the form of variations in the fold coverage, irregular offset which can manifest itself as an acquisition footprint on pre-stack data or even the stacked image. This study deals with the various irregularities introduced by the choice of geometry. Thus assessing the environmental / logistic /economic resource constraints, design of geometry should not sacrifice the basic objective of the 3D survey.

برای دانلود متن کامل این مقاله و بیش از 32 میلیون مقاله دیگر ابتدا ثبت نام کنید

ثبت نام

اگر عضو سایت هستید لطفا وارد حساب کاربری خود شوید

منابع مشابه

Optimizing design of 3D seismic acquisition by CRS trace interpolation

Land seismic data acquisition in most of cases suffers from obstacles in fields which deviates geometry of the real acquired data from what was designed. These obstacles will cause gaps, narrow azimuth and offset limitation in the data. These shortcomings, not only prevents regular trace distribution in bins, but also distorts the subsurface image by reducing illumination of the target formatio...

متن کامل

Analyzing the Illumination and Resolution in Seismic Survey Designing

Seismic modeling aids the geophysicists to have a better understanding of the subsurface image before the seismic acquisition, processing, and interpretation. In this regard, seismic survey modeling is employed to make a model close to the real structure and to obtain very realistic synthetic seismic data. The objective of this study is to analyze the resolution and illumination of the fault by...

متن کامل

Subsurface modeling of mud volcanoes, using density model and analysis of seismic velocity

Detection of subsurface structures by means of gravity method can be used to determine mass distribution and density contrast of rock units. This distribution could be detected by different geophysical methods, especially gravity method. However, gravity techniques have some drawbacks and can't be always successful in distinguishing subsurface structures. Performance of the gravity technique co...

متن کامل

2610588 Volumetric Fault Imaging based on Seismic Geometry Analysis

Computer-aided fault imaging and interpretation is a fundamental tool for subsurface structure characterization and modeling, and the existing methods are primarily based on seismic discontinuity analysis (e.g., coherence and semblance) that evaluates the lateral variation of waveform and/or amplitude. However, such attributes have a limited resolution on subtle faults without apparent displace...

متن کامل

Fault-controlled fluid flow inferred from hydrothermal vents imaged in 3Dseismic reflection data, offshore NWAustralia

Fluid migration pathways in the subsurface are heavily influenced by pre-existing faults. Although studies of active fluid-escape structures can provide insights into the relationships between faults and fluid flow, they cannot fully constrain the geometry of and controls on the contemporaneous subsurface fluid flow pathways. We use 3D seismic reflection data from offshore NW Australia to map 1...

متن کامل

ذخیره در منابع من


  با ذخیره ی این منبع در منابع من، دسترسی به آن را برای استفاده های بعدی آسان تر کنید

برای دانلود متن کامل این مقاله و بیش از 32 میلیون مقاله دیگر ابتدا ثبت نام کنید

ثبت نام

اگر عضو سایت هستید لطفا وارد حساب کاربری خود شوید

عنوان ژورنال:

دوره   شماره 

صفحات  -

تاریخ انتشار 2006