Borehole Stress Orientation  MIN  MAX Top View Drilling Induced Fracture Borehole Breakout Courtesy of Steve Hansen, Schlumberger.

Slides:



Advertisements
Similar presentations
Announcements EXAM 3 is TOMORROW! NO New Homework Office hours…
Advertisements

Polarization of Light Waves
Earth is constantly moving in two ways.
Distribution of Microcracks in Rocks Uniform As in igneous rocks where microcrack density is not related to local structures but rather to a pervasive.
Climate and The Ocean Chapter 17.
(The figures in this section of your text are especially important)
Lecture 13 Electromagnetic Waves Ch. 33 Cartoon Opening Demo Topics –Electromagnetic waves –Traveling E/M wave - Induced electric and induced magnetic.
Models of the Earth.
Fracture Spacing in Miss. Madison Ls
Stereonets Solving geometerical problems – displays geometry and orientation os lines and planes. It is a three-dimensional protractor. With a normal protractor,
Earth Study 360 Technology overview
Field trip this Saturday! We will leave from the loading dock at 7:30 AM sharp! HYDRATE... or else! BRING >1 GALLON OF WATER!
Reading Activity Questions? IB Assessment Statements Topic Polarization: Describe what is meant by polarized light Describe polarization.
Lecture 13 Electromagnetic Waves Ch. 33 Cartoon Opening Demo Topics –Electromagnetic waves –Traveling E/M wave - Induced electric and induced magnetic.
THE PARTS OF A BRUNTON COMPASS
Vectors and Scalars AP Physics C.
GEOREFERENCING SYSTEMS
Weighted Stacking of 3-D Converted-wave Data for Birefringent Media Richard Bale.
Silicon chip birefringence
Electromagnetic Waves
Spatial Variations in Microseismic Focal Mechanisms, Yibal Field, Oman A. AL-Anboori 1, M. Kendall 2, D. Raymer 3, R. Jones 3 and Q. Fisher 1 1 University.
Unit 3 Lesson 1 Earth’s Days, Years, and Seasons Copyright © Houghton Mifflin Harcourt Publishing Company.
Air Pressure and Winds. Atmospheric Pressure  What causes air pressure to change in the horizontal?  Why does the air pressure change at the surface?
Mechanics of Materials – MAE 243 (Section 002) Spring 2008 Dr. Konstantinos A. Sierros.
Lecture 7 Mechanical Properties of Rocks
Option A - Wave Phenomena Standing Waves, Resonance, Doppler Effect, Diffraction, Resolution, Polarization.
EXPLORATION GEOPHYSICS THE EXPLORATION TASK PLAN EXPLORATION APPROACH FOR A MATURE TREND GATHER DATA FOR A MATURE TREND DEVELOP PLAY PROSPECT FRAMEWORK.
PHYSICS 222 EXAM 2 REVIEW SI LEADER: ROSALIE DUBBERKE.
Field notes by Kelsey Wagner. Seismic Anisotropy of the mid to lower crust is very difficult to measure in field by seismologists. Using a scanning electron.
SI leader: Rosalie Dubberke
5. Magnetic forces on current
Cutnell/Johnson Physics 8th edition Reading Quiz Questions
9.2 Latitude and longitude
Introduction to Shear Wave Splitting Erin Elliott Guofeng Yuan February 26, 2010.
Motion at Angles Life in 2-D Review of 1-D Motion  There are three equations of motion for constant acceleration, each of which requires a different.
Chapter 20 Magnetism Conceptual Quiz 20 Conceptual Quiz Questions.
Presentation on Terminology and different types of Faults
3280 East Foothill Boulevard Pasadena, California USA (626) Fax (626) World Wide Web:
5. Magnetic forces on current
Breakout analysis using Fullbore Formation MicroImager images
Introduction to Seismology
STRUCTURAL GEOLOGY LAB. STEREOGRAPHIC PROJECTION Dr. Masdouq Al-Taj
Announcements EXAM 3 is TOMORROW! NO New Homework Office hours…
Polarized Microscope Q.1 What does it mean for the light to be “Polarized” ? Natural sunlight and almost every other form of artificial illumination transmits.
Look at the block diagram below.
GY403 Structural Geology Laboratory
Force on an Electric Charge Moving in a Magnetic Field
Force on an Electric Charge Moving in a Magnetic Field
Latitude and Longitude
Shear alignment of olivine crystals
$$$ DEAL OR NO DEAL $$$.
Angles. Angles Angles Angles The distance from rotary table to Point B as measured along the wellbore is called a measured depth. The vertical distance.
Ch. 2: Fundamental of Structure
Introduction to Shear Wave Splitting
Latitude and Longitude
Announcements I should have exams back to you on Fri.
Latitude and Longitude
CHAPTER THREE DISCONTINUITIES
Dr. Steven Danyluk/Stephen Zagarola
Attitude of Beds Attitude: A general term for the orientation of a line or plane. Attitude refers to the three dimensional orientation of planar and linear.
In-class problem For maximum and minimum stresses of 600 and 200 mega-pascals (MPa) oriented as a vertical vector and a horizontal, E-W striking vector.
The Mohr Stress Diagram
Attitudes of Planes and Lines
Aim: What other details can be discussed about vectors?
by John D. O. Williams, Mark W. Fellgett, and Martyn F. Quinn
Unit 9 Review.
Latitude and Longitude
Conceptual MC Questions
HF Signal Propagation Bill Leonard N0CU 1 June 2019
A B C c b a c A B H= a(sinB) B = drill plunge a =(cSinA/SinC)
Presentation transcript:

Borehole Stress Orientation  MIN  MAX Top View Drilling Induced Fracture Borehole Breakout Courtesy of Steve Hansen, Schlumberger

Types of Directional Drilling for Fractures Courtesy of CSPE Nelson & Serra (1995)

PotentialDrillingDirections on Folds Courtesy of CSPE Nelson et.al. (1987a)

After Nolen-Hoeksema & Howard (1987) Fracture Spacing & Drilling Direction Courtesy of AAPG

Nolen-Hoeksema & Howard (1987) Drilling Direction Nomograph Courtesy of AAPG

High Intensity Fold-Related Fractures

Bedding/Fracture/Well Rotation unrotated rotated Joubert & Rice (1997)

UBIFMI UBI vs. FMI Courtesy of Steve Hansen, Schlumberger UBI Shows Topography FMI Shows Resistivity

Quantitative Fracture Analysis Polar projections of fold and fault related fractures with dip of 300 deg NW After removing structural bedding dip, fractures trend clearly NW-SE and to perpendicular to bedding.

Rotated Fracture Poles NN before bedding rotation after bedding rotation equal area, lower hemisphere, stereonets. fracture poles for all 9 wells ~ 1700 poles Joubert & Rice (1997)

Equation - Fracture Intercept Rate i th fracture - occurrence of i th fracture, The fracture frequency in any arbitrary direction is the sum of: - the cosine of the angle between the normal intercept rate direction of the i th fracture, over all fractures.

Occurrence Weighting (Lacazette 1990) Drill Hole Fracture 2 Fracture Fracture 2 is less likely to be intercepted by the drill hole than fracture 1 - as the angle of the normal approaches 90 deg. W increases. W1 < W2 Joubert & Rice (1997)

Occurrence Corrected Rose Diagrams occurrence weighted fracture planes rotated raw fracture planes Joubert & Rice (1997)

Intercept Rate NORTH EAST SOUTH WEST horizontal 15 deg. 30 deg. 45 deg. 60 deg. 75 deg. vertical Polar chart showing number of fractures intercepted per meter for different drilling directions - (bedding rotated flat). Well #1 Joubert & Rice (1997)

Aperture Variation on Rose Diagram N maximum aperture minimum aperture Joubert & Rice (1997)

Fracture Aperture Courtesy of Steve Hansen, Schlumberger

Equation - Flow Intercept Rate - fracture aperture of the i th fracture Joubert & Rice (1997)

Flow Intercept Rate HORZ. 15 DEG Joubert & Rice (1997)

Calculated Horizontal vs Vertical Drilling horz Vert. inclination angle relative to bedding % of maximum flow well # Triassic Carbonate Reservoirs, Northern British Columbia, Canada From Joubert & Rice (1997) Drilling at low angles to bedding makes a good well

Shear Anisotropy Preferential directional alignment of elastic properties due to regional stress fields Horizontal anisotropy - uniform laterally but not vertically (transversely isotropic with a vertical axis of symmetry) Vertical anisotropy - uniform vertically but not laterally (transversely isotropic with a horizontal axis of symmetry) Shear waves travel faster along axis of symmetry

Shear Wave Birefringence Fracture-induced elastic anisotropy can be detected through shear-wave splitting, or birefringence Shear waves split into fast and slow polarizations Data are analyzed for orientation and degree of anisotropy indicated by the amount of birefringence Fast shear polarization direction relates to fracture orientation