Radon Transform In Geophysics | Tau P Transform for Seismic Data Reconstruction

In this lecture, the focus will remain on Radon Transform which is a mathematical technique that has been widely used in seismic data processing and image analysis. This will typically transform the data from the space-time domain (x, t) to the tau-p domain (τ, p), where it is modified and then transformed back to (x, t) space.
#GeophysicsInsight
#RadonTransformInGeophysics
#TauPTransformforSeismicDataReconstruction
…………………………………………………………………………………………………
To access comprehensive information regarding Geophysics courses, kindly go to the provided website. :
sites.google.com/view/geophys...
About Instructor:
sites.google.com/view/dryasir...
………………………………………………………………………………………………………
Further to study more about the new topics you can view and click on the links below.
Hilbert Transform | Time-Frequency Analysis in Seismic
• Hilbert Transform | Ti...
Seismic Data Modeling using Software | Tesseral Pro | Wave Propagation
• Seismic Data Modeling ...
AVO (Amplitude versus Offset) as a DHI (Direct Hydrocarbon Indicator)
• AVO (Amplitude versus ...
Thank you for taking the time to watch this video. I believe you want to learn how to process seismic data with sequence. So, you can either enroll in the course or watch the video below about a specific topic that interests you.
Course Link: www.openlearning.com/usmmooc/...
Chapter 1: Understanding Seismic: An Overview
1. Introduction to the Course
• Introduction to MOOC |...
2. Chapter Contents
• Introduction to Course...
Chapter 2: Data Processing in Geophysics
1. Scaling your Skills in Geophysics
• Seismic Data Processin...
2. Real Scenario and Motivation of Seismic
• Motivation of SDPI wit...
Chapter 3: Pre-processing Steps
1. Seismic Data Recording System
• Seismic Data Recording...
2. Demultiplexing and Reformatting Seismic Data
• Multiplex, De-multiple...
3. Muting, Trace Editing, Absorption
• Muting, Trace Editing,...
4. Seismic Filters and Types
• Seismic Filters and Ty...
5. Seismic Multiple & f-k Autonomy
• Seismic Multiples | MOOC
6. Seismic Gain, Types, and Usage
• Seismic Signal Gain | ...
Chapter 4: Main Seismic Processing Steps
1. Introduction to Main Processing
• Introduction to Main P...
2. Data and Sorting in Different Domains
• Data Sorting and Its U...
3. Understanding Seismic Velocities
• Understanding Seismic ...
4. Velocity Analysis & NMO Correction
• Velocity Analysis & NM...
5. Static Or Weathering Correction
• Seismic Static Correct...
6. Deconvolution
• Deconvolution | Correl...
Chapter 5: Seismic Migration & Imaging
1. Seismic Migration: An Overview
• Introduction to Seismi...
2. Classifications of Seismic Migration/Imaging
• Classification of Seis...
3. Seismic Diffraction: An Overview
• Seismic Diffraction: A...
4. Diffraction Imaging by Separation
• Diffraction Imaging by...
5. Over Vs Under Migration & 2D Vs 3D Data
• Over Vs Under Migratio...
6. Pre-stack Vs Post-Stack Time & Vs Depth Migration
• Pre-Stack Vs Post-Stac...
If you are interested in the topic of "Seismic Interpretation".
Introduction of Seismic Interpretation | Subsurface Interpretation | Deep Geological Interpretation
• Introduction of Seismi...
3D Seismic Interpretation | Data Loading | Visualization | Horizon | Attributes
• 3D Seismic Interpretat...
Global Seismic Interpretation Software Installation and License Request Guide | Paleoscan | Eliis
• Global Seismic Interpr...
AVO (Amplitude versus Offset) as a DHI (Direct Hydrocarbon Indicator)
• AVO (Amplitude versus ...
Also, some Guest Speaker talk on Seismic related topics.
Marine Seismic Exploration | From Acquisition, Processing to Interpretation | Guest Speaker at ITS
• Marine Seismic Explora...
Depth Imaging using least-squares RTM of short-streamer seismic data
• Depth Imaging using le...
Seismic Data Modeling using Software | Tesseral Pro | Wave Propagation
• Seismic Data Modeling ...
Radon Transform In Geophysics | Tau P Transform for Seismic Data Reconstruction
• Radon Transform In Geo...
Hilbert Transform | Time Frequency Analysis in Seismic
• Hilbert Transform | Ti...

[@peterkunbo1]

Thank you for your time and effort in making this lecture. It is very clear and informative

[@GeophysicsInsight]

Glad it was helpful! and thank you for your constructive comments.

[@gunjan6652]

Thank you for making video in this topic

[@GeophysicsInsight]

Hello Gunjan, Thank you for your comments.

[@lola-ye5cq]

Thanks for your helpful explanation 🌸appreciate your efforts

[@GeophysicsInsight]

Thank you, Lola for your comment.

[@jahongirxayrullaev108]

Great work, thank you. Keep going and good luck Sir.

[@GeophysicsInsight]

Thank you Jahongir for your comment.

[@jahongirxayrullaev108]

​@@GeophysicsInsight Four formulas are given on a slide on minute 6 of this video. All formulas use q (moveout) to calculate t. What is unit of q (moveout) and how is it difference than slowness?

[@samou9547]

Hello, in parabolic radon transform, why I can see the weak horizon events after inversion (in picture C). How they come from? Is this a inevitable problem?

[@GeophysicsInsight]

These weak horizon after in parabolic radon transform are because of overlapping the linear events with the non-linear events. So, Always there is new research going on to have optimum results of separation which gives an opportunity of finding solutions to these problems.

[@evilaquaman]

thanks great content but can you remove the music?

[@GeophysicsInsight]

Thank you and Noted!