glg 101 - physical geology bob leighty geologic structures
DESCRIPTION
If rocks are subjected to stress, they may be deformed (& show strain)stressstrain undeformed rocks deformed rocks (strain) (stress) compression Stress & Strain Structural GeologyTRANSCRIPT
GLG 101 - Physical GeologyGLG 101 - Physical Geology Bob LeightyBob Leighty
Geologic StructuresGeologic Structures
These lecture notes are very similar to the ones I use in my traditional classes. You’ll find they are loaded with imagery and streamlined text that highlight the most essential terms and concepts. The notes provide a framework for learning and, by themselves, are not meant to be a comprehensive source of information.To take advantage of the global knowledge base known as the Internet, I have included numerous hyperlinks to external web sites (like the Wikipedia, USGS, NASA, etc.). Follow the links and scan them for relevant info. The information from linked web sites is meant to supplement and reinforce the lecture notes – you won’t be responsible for knowing everything contained in them.
As a distance learning student, you need to explore and understand the content more independently than in a traditional class. As always, I will help guide you through this learning adventure. Remember, email Dr. Bob if you have any questions about today’s lecture ([email protected]).Leave no questions behind!Explore and have fun!Explore and have fun!
These notes and web links are your primary “lecture” content in this class. Additionally, various articles are assigned each week to supplement this “lecture” information. I believe you’ll have enough information to reference without having to purchase a costly textbook.
If rocks are subjected to stress, they may be deformed (& show strain)
undeformed rocks deformed rocks (strain)
(stress)compression
Stress & StrainStress & StrainStructuralStructuralGeologyGeology
Types of StressTypes of StressStress & StrainStress & StrainStructuralStructural
GeologyGeology
higher T (deeper)lower T (shallow)stronger rocks weaker rocks
Brittle Ductile(faulting) (folding)
fast strain rate slow strain rate
Types of StrainTypes of StrainStress & StrainStress & StrainStructuralStructural
GeologyGeology
Form under brittle conditions by any stress
Fractures with differential offset (vertical and/or horizontal)
FW
How to ID a fault with vertical offset
HW 1) Find matching features on either side of the faultHangingwall (HW): rocks above the fault plane
Footwall (FW): rocks below the fault plane
2) Which way does the HW move?
FaultsFaultsStructuralStructuralGeologyGeology
Normal faults – Tensional stress causes HW
HW
Reverse faults – Compressional stress causes HW
HW
Transform faults – Shear stress causes horizontal movement
FaultsFaultsStructuralStructuralGeologyGeology
FaultsFaultsStructuralStructuralGeologyGeology
Unnamed fault on AZ87(a high-angle normal fault) HW
FW
South Mountain detachment fault(a low-angle normal fault)
Thrust faults = low-angle (dip <45º) reverse faults
HWFW
FaultsFaultsStructuralStructuralGeologyGeology
The San Andreas transform fault (mostly horizontal movement)
FaultsFaultsStructuralStructuralGeologyGeology
Joint: a fracture where no offset has occurred
JointsJointsStructuralStructuralGeologyGeology
Form under ductile conditions by compressional stresses
FoldsFoldsStructuralStructuralGeologyGeology
Axial plane - splits the fold into two limbs
FoldsFoldsStructuralStructuralGeologyGeology
FoldsFoldsStructuralStructuralGeologyGeology
Strike & dip – describes orientation of bedding
dip
measuring strike & dip with a compass
strike dip
strik
e
FoldsFoldsStructuralStructuralGeologyGeology
limbs dip in toward axial plane
youngest beds in center of the fold
“point” downSynclinesSynclines
FoldsFoldsStructuralStructuralGeologyGeology
“point” up limbs dip away from axial plane oldest beds in center of the fold
AnticlinesAnticlinesFoldsFoldsStructuralStructural
GeologyGeology
Folds “plunge” when the fold axis is not horizontal
Form curving outcrop patterns
Plunging FoldsPlunging FoldsFoldsFoldsStructuralStructural
GeologyGeology
A one-limbed fold with horizontal beds on the top & bottom
MonoclinesMonoclinesFoldsFoldsStructuralStructural
GeologyGeology
Dome – A circular upwarp (a circular anticline)
Black Hills, SD
Structural DomesStructural DomesFoldsFoldsStructuralStructural
GeologyGeology
Basin – A circular downwarp (a circular syncline)
Michigan
Structural BasinsStructural BasinsFoldsFoldsStructuralStructural
GeologyGeology
WWW Links in this LectureWWW Links in this Lecture> Stress - http://en.wikipedia.org/wiki/Stress_%28physics%29> Strain - http://en.wikipedia.org/wiki/Strain_%28materials_science%29> Faults - http://en.wikipedia.org/wiki/Faults> Dip-slip fault - http://en.wikipedia.org/wiki/Geologic_fault#Dip-slip_faults> Strike-slip fault - http://en.wikipedia.org/wiki/Geologic_fault#Strike-slip_faults> Detachment fault - http://en.wikipedia.org/wiki/Detachment_fault> Thrust fault - http://en.wikipedia.org/wiki/Thrust_fault> San Andreas transform fault - http://en.wikipedia.org/wiki/San_Andreas_Fault> Joint - http://en.wikipedia.org/wiki/Joint_%28geology%29> Folds - http://en.wikipedia.org/wiki/Fold_%28geology%29> Strike and dip - http://en.wikipedia.org/wiki/Strike_and_dip> Syncline - http://en.wikipedia.org/wiki/Syncline> Anticline - http://en.wikipedia.org/wiki/Anticline> Dome - http://en.wikipedia.org/wiki/Dome_%28geology%29> Basin - http://en.wikipedia.org/wiki/Basin_%28geology%29
StructuralStructuralGeologyGeology