Thrust faults (continued) Cross sections Importance to oil exploration.

Slides:



Advertisements
Similar presentations
Geologic Time, Unconformities and Relative Dating Uniformitarianism Appendix A.
Advertisements

The Siwalik Fold Belt along the Himalayan piedmont 10 km Main Frontal Thrust Main Boundary Thrust.
Lab 7 – Structural Geology Chapter 10 Turn In: Lab 6 Pre-Lab 7 EC 2 Handouts: Quiz 6 Lab 7 Pre-Lab 8.
Section 6.1 – Volume using Cross-sections – Disks and Washers Copyright  2010 Pearson Education, Inc. Volume of the disk r.
Deformation of the Crust
Forces in Earth’s Crust
Steno’s Laws of Stratigraphy
Classroom presentations to accompany Understanding Earth, 3rd edition prepared by Peter Copeland and William Dupré University of Houston Chapter 21 Deformation.
Chapter-11 Mountain Building
Dip-slip faults Goal: To interpret dip-slip faults on seismic sections and to build on your interpretations to understand normal-fault and thrust-fault.
Jaime Toro West Virginia University
Relative Dating The Law of Superposition
1 Lab 08 ONLINE LESSON. 2 If viewing this lesson in Powerpoint Use down or up arrows to navigate.
Chapter 5 pages Warm up Define deformation Exit
Announcements Talk This Thurs. 4 pm, Rm. Haury Bldg. Rm 216, "Tertiary structural and stratigraphic evolution of the Greater Tucson area", by Jon Spencer.
Magnetic Expression of Buried and Obscured Anticlines in South America An HRAM survey flown over a tropical forest in Guatemala reveals the presence of.
II. Basic Techniques in Structural Geology Field measurements and mapping Terminology on faults and folds Stereographic projections From maps to cross-sections.
Section 1: Forces in Earth’s Crust
Chapter 20 Geologic structures.
Geologic Maps and Structures Lab 2a Geology 208. Geologic Maps: Snoqualmie Pass.
Plate Puzzle Plate Motions This PPT:
Normal faults -rifted continental margins -form in extension -typical for continental and oceanic lithosphere -jargon (horsts, grabens, listric, detachment)
Announcements Field trip this Saturday to Cottonwood Canyon area 7:30 AM at loading dock. We will map some really cool stuff! Please review map symbols.
Announcements Field trip during lab today/tomorrow Field trip this Saturday to Collosal Cave area 7:30 AM at loading dock. We will map some really cool.
Unit 5 Topic 7 - Mountains 1. Mountains! Mountain building takes many years Cordillera is Spanish for mountain range 2.
Instruction: View full-screen images in the Slide Show mode of display. Read the explanatory notes in the Normal View mode of display.
Key Ideas State the principle of uniformitarianism.
mountains, mountain building, & growth of continents
Newton ’ s Law of Universal Gravitation Dan Li SUNY-Stony Brook 12/09/2002.
PASSIVE MODE SALT DOES NOT ACTIVELY DEFORM SEDIMENT. MOST FEATURES ARE ATTRIBUTED TO SALT WITHDRAWAL. ACTIVE MODE SALT ACTIVELY PUSHES SEDIMENT COVER OUT.
EARS 5131 STUCTURE AND HYDROCARBON PROSPECTIVITY OF BASIN.
1 THRUST FAULTS: ASSOCIATED STRUCTURES AND IMPLICATIONS IN HYDROCARBONS TRAPS James Moore Alex Nyombi Christian Hidalgo Adekunle Odutola STRUCTURE AND.
Interpreting Earth’s Rocks to Determine Its Past History.
Faults and Folds Normal Fault In normal faulting, the hanging wall block moves down relative to the footwall block. The fault plane.
Unit 2: Tectonic Process Ms. Thind.   Rocks under pressure or tension fracture under strain  If movement takes place along a fracture a rift is formed.
Exploring the Earth’s Surface Landforms
II. Basic Techniques in Structural Geology
Lecture 22 By thought and dint of hammering, Is the good work done whereof I sing, And a jollier crowd you´ll rarely find, than the men who chip on earth´s.
Volume Prisms and Cylinders. Volume of a Prism A prism is a solid object with: identical ends flat sides and the same Cross Section all along its length.
Recognizing and mapping faults using lidar, Google Earth, and field data Anne E. Egger Central Washington University Teaching Structural Geology, Geophysics,
Structure labs/drawing Recent labs often “sloppy” Not taking time to draw contacts properly –Units must maintain thickness –Contacts should be parallel.
Folds Read Davis and Reynolds, Chapter 7 Why is it important? fundamental to deformation of the Earth’s crust; structural traps for oil ore deposits.
Science 7: Unit E: Planet Earth Topic 7: Mountains.
July 2, 2016July 2, 2016July 2, 2016 AF Carpinelli 1 Mountains and Mountain Building.
Room: 407 Tel: Patrice Rey.
Topic 7: Mountains. Mountain building takes many years. Himalayas, Nepal.
Offshore Oil Formation  The formation of oil takes a tremendously long time. Millions of years ago plants and animals of the oceans died & settled on.
Eric H Christiansen.
Fold-thrust belts Goonyella coal mine, Australia, courtesy Steve Marshak/Scott Wilkerson.
Chapter 5 pages Warm up Explain what a thrust fault is? Exit
Lecture Outlines Physical Geology, 10/e
Find the common denominator. Make equivalent fractions.
Reading Displacement chapter, in library (not available online). Read plus Concept map due Wednesday. Davis and Reynolds “ Structural.
Fold Thrust Belts.
II. Basic Techniques in Structural Geology
Relative Dating Notes.
Relative Age Dating What is it?
Chapter 4: Plate Tectonics.
Chapter 10.
PASSIVE MODE ACTIVE MODE
Earth Systems 3209 Unit 2: Relative Dating.
Outline Terminology Ramp and Flat thrusts Animations
EARTH AND SPACE SCIENCE
Chapter 8 section 1 RELATIVE AGE.
Chapter 6 Section 1: Forces in Earth’s crust
Relative- Age Dating.
Fractures, Faults, & Friction
What exactly is an earthquake?
Mountains.
Relative Dating Notes.
Presentation transcript:

Thrust faults (continued) Cross sections Importance to oil exploration

Cross-sections Thrust faults cut up-section only! (or section-parallel) Every flat or ramp in the FW should correspond to an equivalent flat or ramp in the WH Bed thickness is preserved (conservation of volume and mass) Other than that - it’s all interpretation!

A trip along the Athabasca River

Roche Ronde More Canadian Cordillera

Boulle Range

Roche Ronde Boulle Range

Other types of shortening-high angle; typical reactivate older structures (“inversion tectonics”)

Thrust belts contain a significant fraction of the Earth’s oil deposits- typically form in anticlinal traps