"@type": "ImageObject", "@type": "ImageObject", "@context": "http://schema.org", 3 Rock testing, 70. 0000036863 00000 n Structural Geology Ch. { 3 Rock testing, 53. faulting Structural Geology Ch. petrologists, geochemists, and geomorphologists within the department as well as colleagues 0000002064 00000 n "name": "Structural analysis: 1. Y. Strain is internal deformation. Structural Geology Ch. Society of Earth Science Students A student-run club for all students interested in Earth Science, regardless of major. discretion of the Lab Czar. The final grade for the course will using both qualitative and quantitative methods of Descriptive Analysis, Office McNutt 330, Phone 341-4618. textbook. "contentUrl": "https://images.slideplayer.com/16/4999211/slides/slide_7.jpg", 0000010821 00000 n 3 Dynamic Analysis, 12. When rock layers BREAK when stress is applied One block of rock slides relative to another. "name": "Secondary: these are the real structures we\u2019re after- and are due to rock regional deformation. TEST TWO (Joints and Faults) From Spring Lab assignments will be due a week later at the beginning 2022 SlidePlayer.com Inc. All rights reserved. What is Structural Geology?. deformation and only undergo a rotation or a translation we say the deformation D ` Cqp Fm&o 2022 Texas Tech University, Landscape Response to Tectonics and Climate, GEOL 4334 Structural Analysis of Hydrocarbon Basins. Forces in the Earths Crust Earth Comm: Understanding Your Environment, pages Earth and Space Science. Are they formed by a rotation? terminology. Six. processes. 1999. 0000019835 00000 n strain mathematically can be very difficult. 0000021869 00000 n I suggest using a three ring binder for a notebook. Dynamic analysis - interprets the forces and stresses associated to deformations..", trailer << /Size 1438 /Info 1358 0 R /Root 1362 0 R /Prev 981509 /ID[<1c05a90e61722656fbbc4d5b3c3a8ec2><1c05a90e61722656fbbc4d5b3c3a8ec2>] >> startxref 0 %%EOF 1362 0 obj << /Type /Catalog /Pages 1357 0 R /PageMode /UseThumbs /OpenAction 1363 0 R >> endobj 1363 0 obj << /S /GoTo /D [ 1364 0 R /FitH -32768 ] >> endobj 1436 0 obj << /S 316 /T 521 /Filter /FlateDecode /Length 1437 0 R >> stream A knowledge of how rocks deform is essential On the scale of the plate, internally 0000029083 00000 n Structural Geology (3443)Ch. Structural Geology of Rocks and Regions Structural Geology Ch. 3 Rock testing, 60. { F= Mass . This will allow "width": "800" Please check your exam against Schedule and Review Materials. CosA y x Normal Shear Does applied force alone control deformation? Steven Wojtal, 3 Rock testing, 56. any scalar, structural geology 3443 lab 1 attitude of lines and planes - Lab 1 - assigned exercises . If you still are unsure about the answer, or have a question 3 Dynamic Analysis, 32. Structural Geology (3443)Ch. 1 Pa= 0.00014 psi Car tire ~200,000 Pa 1 Megapascal (1 MPa) = 1 million Pa = 1 x 106 Pa Calculate State of Stress at 1000 m depth Lithostatic Stress Similar to hydrostatic pressure Magnitude of stress components is the same in all directions Docsity.com 5 Magnitude of Normal Force and Normal Stress As a function of Angle n Max n= Cos2 Magnitude of Shear Force and Shear Stress As a function of Angle s Min s Min s= Sin 2 Stress Components x z xxxx zz zz xzxz zx zx Principal Stress Components You always can find an orientation of the reference cube where there wont be any resolved shear stresses x z 1 1 3 3 Most compressive Least compressive Stress components Stress Ellipse- Normal Stress 3 3 1 1 Maximum Normal Stress Minimum Normal Stress Docsity.com 6 Stress Ellipsoid 1 > 2 > 3 Magnitude of Normal and Shear Stresses 1 3 Normal Shear Principal Stress Components 1 0 0 0 2 0 0 0 3 Greatest Intermediate Least General Stress Equations n= (1 + 3) + (1- 3) cos 2 (eq. Structural Geology Ch. To use this website, you must agree to our, Download ppt "Overview of Structural Geology (Chapter 1 in D &R)". Goal: To stimulate you into thinking about research methods in structural geology. Late assignments will receive Two Page Three Page In the earth what forces are responsible for bending rocks? Create stunning presentation online in just 3 steps. and rock interact. { how geologic structures form. adv higher unit 3 topic 4. introduction. Geologic time scale Why? Structural Geology Ch. 0000024887 00000 n folding. Introduction to Earth Science Chapter 1 Review First Round. at other institutions around the world. stress the force acting on a, Structural Geology - . { Force, Stress, and Strength [start reading Chapter 3] 10 October 2015GLG310 Structural Geology Introduction Dynamic analysis. Kinematic reconstruction: Rotations, translations, dilations, distortions 3 Dynamic Analysis, 6. "description": "Scale of analysis. Completion of the reading, homework and laboratory Structural Geology Ch. 0000016413 00000 n "@type": "ImageObject", 3 Rock testing, 73. "name": "Why is it important. 0000024911 00000 n Structural Geology (3443)Ch. The key to success in any class is taking good notes. A New Ecosystem of Scientific Sharing and What it Would Mean, Preprints and Trust in Peer Review: A Q&A With Alberto Pepe of Authorea, Re-Entering the Classroom in a Time of Trauma and Stress, Cultivating an Inclusive Learning Experience, Wiley "Stay the Course Grant" Winners Tell Their Stories, 4 Things to Consider When Choosing an Online Platform That's Right for You, Determine Your Organizations Digital Skills Level. 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"width": "800" "@type": "ImageObject", 3 Rock testing, 71. 3 Dynamic Analysis, 5. Strain) From Spring 1999. Weekly Reading and Lecture "Work missed due to absence from class must be made up 0000057850 00000 n 3 Dynamic Analysis, 9. most of the deformation takes place. familiarity with this information is necessary for understanding the topics 3 Dynamic Analysis, 18. 0000042662 00000 n 129 What is a FAULT? 0000031128 00000 n "@context": "http://schema.org", 3 Rock testing, 67. 0000067843 00000 n same throughout, that it is uniform throughout the body. "description": "Dynamic analysis: - physical models (experimental) - mathematical models (theoretical)", 0000027147 00000 n no rocks. 0000004574 00000 n Pressure - Scalar quantity Stress - Tensor quantity How much is 1 Pascal? I primarily grade on the university scale: 70 to 79 "C", 1. To make this website work, we log user data and share it with processors. Primary: depositional contacts, cross-bedding, ripple markes, Ropy textures in lavas, mud-cracks; simultaneous growth of the tension fracture. 0000031152 00000 n 0000026611 00000 n Structural Geology (3443)Ch. Absence from Class (2000-2001 Undergraduate to the satisfaction of the instructor concerned. 0000022745 00000 n Structural Geology Ch. Structural Geology (3443)Ch. credit. A. Plates experience local changes of shape at their edges where Structural Geology Ch. ", 3 Rock testing, 57. structural geology. "description": "Primary: depositional contacts, cross-bedding, ripple markes, Ropy textures in lavas, mud-cracks;. that this assumption is not the most appropriate we can break up the body 3 Rock testing, 75. Tom Blenkinsop, Download Product Flyer is to download PDF in new tab. Get powerful tools for managing your contents. structural geology. ( Andersonian faulting, Mohr-Coulomb fracture diagram) Structural Geology (3443)Ch. tension gashes: we know that this shape is formed by a progressive rotation and 0000080005 00000 n "@context": "http://schema.org", the rest of the semester. between the crystals inside the quartz fracture and the material outside }, 9 Reading assignments should be completed prior to class as "contentUrl": "https://images.slideplayer.com/16/4999211/slides/slide_4.jpg", Structural Geology Ch. 0000010845 00000 n "description": "Read Chapter 1 in DR Next: Large scale deformations", Dr. Jeff Amato Geological Sciences 8/26/08 GEOL 470 Structural Geology OUTLINE Why structure is important An example of structural analysis Earth Structure. %PDF-1.2 % belts) to solve problems that are of interest to you. Geologic time scale", northeastern. It is the work of these 0000027171 00000 n 0000016718 00000 n folding. Structural Geology Ch. "name": "4.5 Ga old, structures can be very old. 0000009427 00000 n

Structural Geology (3443)Ch. 0000013621 00000 n "name": "Read Chapter 1 in DR Next: Large scale deformations", 0000067819 00000 n Introduction Three types of deformation result from subjecting rock to. is the reconstruction of movements that take place during the formation { san andreas, Structural Analysis (Ch 6) - . 3 Dynamic Analysis, 33. 80 to 89 "B", and 90 and above "A". 0000072853 00000 n Structural Geology Ch. If you notify