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Technical Content

Technical Abstract
EAGE - European Association of Geoscientists and Engineers | Xiaodong Wu, Yu Wang, Yi Xie, Joe Zhou, Dechun Lin, Casasanta Lorenzo © 2017 EAGE | June

The absorption effect caused by the anelastic nature of earth leads to attenuation of amplitudes and distortion of phases for seismic wave. The so-called Q factor has to be compensated for correct imaging. We propose least square Q-Kirchhoff migration (LSQPSDM) in which absorption is ...

Technical Abstract
EAGE - European Association of Geoscientists and Engineers | Gordon Poole © 2017 EAGE | June

2D deconvolution is an attractive approach for short period multiple prediction as it does not require direct recording of the multiple generator and can model multiples relating to more than one multiple generator at a time. One drawback, however, relates to an inherent over ...

Technical Abstract
EAGE - European Association of Geoscientists and Engineers | Jiang Liu (CNOOC), GuangYing Yu (CGG), Xinwei He (CGG), XiuPing Shi (CGG), Jiang Liu (CGG) © 2017 EAGE | June

Make a technical workflow including rockphysics, post-stack gestatistical inversion, seismic forward research and coal constrained pre-stack geostatistical inversion for the fine reservoir predictiong under coal interbedded. This work flow achieved huge success in the new development wells drilling.

Technical Abstract
EAGE - European Association of Geoscientists and Engineers | Carsten Scholl, Stephen Hallinan, Federico Miorelli, Don Watts © 2017 EAGE | June

A subsurface volume that can be reliably interpreted in terms of geologically-relevant attributes is a reasonable objective for products from depth inversion workflows. Commonly the field geophysics data available are inherently non-unique and deficient (noise, aliasing, etc.), so an implementation of some type of ...

Technical Abstract
EAGE - European Association of Geoscientists and Engineers | Anna Sedova, Gillian Royle, Olivier Hermant, Matthieu Retailleau, Gilles Lambare © 2017 EAGE | June

Standard reflection-based model building for land applications is challenging due to reduced data quality, near-surface heterogeneities, and the low-fold of reflection data at shallow depths. Broadband and large offset data acquisitions have been developed with the aim of investigating full waveform inversion (FWI) as ...

Technical Abstract
EAGE workshop/forum/local conference | Tran Thinh To, Shuhong Cao, Jason Sun, Joe Zhou © 2017 EAGE | June

In this paper, we discuss the deblending result of a penta-source marine towed streamer data. The small dithering time renders the cross-talk noise to be semi-coherent in all domains, making this dataset challenging for existing deblending techniques. To tackle this data, we propose a ...

Technical Abstract
EAGE - European Association of Geoscientists and Engineers | H. Puntous (Total), J.L. Boelle (Total), P. Ricarte (CGG), F. Adler (Total) © 2017 EAGE | June

3D elastic modelling was performed to compare two acquisition designs . Blind full processing sequence was applied to ensure unbiased conclusions and final quality. Final quality on stack sections are similar in quality for both flat and highly structured sub-surface. some major advantages of ...

Technical Abstract
EAGE - European Association of Geoscientists and Engineers | D. McCarthy (CGG), A. Berhaud (CGG), S. Mahrooqi (PDO), G. Henin (CGG), J. Shorter (PDO) © 2017 EAGE | June

Difficulties in processing land seismic data often arise due to insufficient sampling of the wavefield. Fully unconstrained simultaneous shooting offers a way to substantially increase productivity and hence source densities, leading to improved sampling of the wavefield. In order to achieve this we must ...

Technical Abstract
EAGE - European Association of Geoscientists and Engineers | Robert Soubaras, Bruno Gratacos © 2017 EAGE | June

Full waveform inversion (FWI) is a method of velocity estimation which minimizes the misfit between recorded and modeled data, the parameters of the minimization being the velocity model. If the velocity model is smooth, then only the refracted waves are modeled and used, if ...

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