Lecture 17 Structural geology and tectonics Hor 1

Lecture 17 Structural geology and tectonics Hor. 1 Hor. 2 Hor. 3 Courtesy of Exxon. Mobil FWS 04 L 10 – Structural Analysis

Geologic Framework Structural analysis is part of the entire geologic framework. Using all available data (wells, seismic, outcrop, regional studies, gravity, magnetics, etc. ), build a framework of present-day structure and stratigraphy Ø Structural Interpretation • Faults & Folds • Subsidence & Uplift • Structural Trends • Structural Features Ø Stratigraphic Interpretation • Unconformities • Stratal Packages • Environments / Facies / Lithologies • Ages Courtesy of Exxon. Mobil FWS 04 L 9 – Overview

Structural Analysis - What is it? The analysis of all of the significant processes that formed a basin and deformed its sedimentary fill from basin-scale processes (e. g. , plate tectonics) to centimeter-scale processes (e. g. , fracturing) Some Major Elements: • Basin Formation • Fault Network Mapping • Stratigraphic Deformation • Present-Day Trap Definition • Timing of Trap Development Courtesy of Exxon. Mobil FWS 04 L 10 – Structural Analysis

Role of Seismic Interpretation • Identify and map faults, folds, uplifts, and other structural elements • Interpret structural settings and structural styles • Ensure 3 D geometric consistency in an interpretation - is it structurally valid? • Determine timing relationships, especially the timing of trap formation • Check if the interpretation is admissible Courtesy of Exxon. Mobil FWS 04 L 10 – Structural Analysis

A Caution about Seismic Images Most seismic data are displayed in 2 way TIME, which can distort geometric relationships V: H is 1. 3: 1 At 1900 m/s V: H is 1: 1 At 2500 m/s V: H is 0. 9: 1 At 3000 m/s Watch the vertical exaggeration It changes with depth V: H is 0. 8: 1 At 3500 m/s 1 km Courtesy of Exxon. Mobil FWS 04 L 10 – Structural Analysis

The STRENGTHS of Seismic Data • Inherently 3 -D (even if a 2 -D grid) • Able to image trap-scale structures • Able to image stratigraphy, to identify reservoir, seal, and for use on structural markers, e. g. , to constrain fault offsets • Provides a 3 -D context for understanding other data – surface geology – well data – potential field data Courtesy of Exxon. Mobil FWS 04 L 10 – Structural Analysis

The WEAKNESSES of Seismic Data • Limited resolution: can’t resolve “small” features • Steep dips can be difficult to image • Acquisition can be difficult, e. g. in areas of: variable topography, variable surface geology, or “hard” water bottom • Vertical axis is typically (migrated) time, not depth – Velocity variations distort geometries • Display scales are commonly not V: H=1: 1, which results in distortions of geometries • Typically we can’t “see” hydrocarbons Courtesy of Exxon. Mobil FWS 04 L 10 – Structural Analysis

A ‘Synergistic’ Relationship You can not get all of the stratigraphic information without working the structure You can not get all of the structural information without working the stratigraphy Courtesy of Exxon. Mobil FWS 04 L 10 – Structural Analysis

Basic Observations: Profile View We can recognize moderate- to large-scale faults on seismic profiles by: • Termination of reflections • Offset in stratigraphic markers • Abrupt changes in dip • Abrupt changes in seismic patterns • Fault plane reflections • Associated folding or sag • Discontinuities Courtesy of Exxon. Mobil FWS 04 L 10 – Structural Analysis

Fault Identification: Time Slice View Do you see evidence for faults? 1856 ms Courtesy of Exxon. Mobil FWS 04 L 10 – Structural Analysis

Coherency Data Also known as Discontinuity or Variance A derivative data volume based on trace-to-trace correlation Data range from 0 to 1, (1 = neighboring traces are identical) Amplitude Data Discontinuity 1856 ms Courtesy of Exxon. Mobil 1856 ms FWS 04 L 10 – Structural Analysis

Corendering of Data 1. The amplitude data is displayed (red-blue) 2. The coherency data below user-defined thresholds is over-posted in black (very low values ) and gray (low values) Opacity for the Continuity Data Black Gray Transparent 1856 ms Courtesy of Exxon. Mobil FWS 04 L 10 – Structural Analysis

Fault Identification: Profile Views A B A C B N Faults must tie on lines that intersect or the interpretation is not internally consistent Courtesy of Exxon. Mobil S W C E tie FWS 04 L 10 – Structural Analysis

Interpreting Faults Structural Observations Courtesy of Exxon. Mobil Structural Concepts FWS 04 L 10 – Structural Analysis

Interpreting Faults Structural Observations Structural Concepts • Tectonic Setting – Divergent zones – Convergent zones – Strike-slip zones – Mobile substrate • How Structures Evolve – Fault-bend folds – Fault-propagation folds – Salt movement – etc. • Fault segments on seismic lines • Fault plane orientation • Sense of motion • Magnitude of offset • Range of depths • Relative timing – when faults moved – when structures grew Courtesy of Exxon. Mobil FWS 04 L 10 – Structural Analysis

Structural Styles Matrix EXTENSION CONTRACTION LATERAL UPLIFT, SUBSIDENCE BASEMENT INVOLVED extensional fault blocks contractional fault blocks strike-slip or wrench faulting basement warps BASEMENT DETACHED detached normal faulting fold-andthrust belts tear faults (detached) salt, shale diapirism Courtesy of Exxon. Mobil FWS 04 L 10 – Structural Analysis

Extensional Faults basement involved basement detached 1 mile Courtesy of Exxon. Mobil FWS 04 L 10 – Structural Analysis

Diapirs Can Provide Good Traps Salt and shale layers can become mobile when subjected to differential loading Imaging beneath salt is very difficult, but the rewards can be great! Many oil and gas fields have been found associated with salt & shale diapirs Courtesy of Exxon. Mobil FWS 04 L 10 – Structural Analysis

Is the Interpretation Admissible? We can check the kinematic admissibility of a thrust fault interpretation by means of a 2 -D sequential restoration Courtesy of Exxon. Mobil FWS 04 L 10 – Structural Analysis

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