35TH INTERNATIONAL GEOLOGICAL CONGRESS
|
|
|
- Marianna Lamb
- 6 years ago
- Views:
Transcription
1 35TH INTERNATIONAL GEOLOGICAL CONGRESS T Rock Deformation and Structural Geology Date Thursday, 01 September 2016 Time 08:00 to 10:00 08:00 08: Pseudotachylytes: towords a depth of origin Prof. Uwe Altenberger 08:15 08: Microstructural and chemical heterogeneity of pseudotachylytes from Indian craton, and its implications for frictional Professor Anupam Chattopadhyay melting process along seismic faults 08:30 09: Interpreting continuous-discontinuous deformation structures considering a continuum of fault slip styles: The Dr. Ake Fagereng example of flexural-slip folds Keynote 09:00 09: Structural analysis of Jwaneng Mine, Botswana Dr. Ian Basson 09:15 09: Structural analysis of the Steenkampskraal Monazite Deposit, Western Cape, South Africa Dr. Ian Basson 09:30 09: Interactive Structural Analysis of Virtual Geological Outcrops Dr. Michael Roach Page: 1/7
2 T Rock Deformation and Structural Geology Date Thursday, 01 September 2016 Time 10:30 to 12:00 10:30 10: Structural Development of the Potchefstroom Thrust and Fault System, Witwatersrand Basin, South Africa. Mr. Matt Terracin 10:45 11: The Time that Geology Forget What Dykes in the Sydney Basin tell us about the Volcanic Evolution of the East Ms. Helen Baxter Australian Continental Margin. 11:00 11: A comparative study between magmatic and magnetic fabrics with flow indicators to infer magma flow in sills. Dr. Lauren Hoyer 11:15 11: Interpreting earthquake-triggered mass transport and soft sediment deformation in Lake Lisan, Dead Sea Basin Prof. Shmuel Marco 11:30 11: Micro-structural analysis to identify micro-scale deformation mechanisms and their effects on fault sealing capacity: Dr. Yangwen Pei an example from the Lenghu5 thrust-fold belt, Qaidam Basin, NE Tibetan Plateau 11:45 12: The architecture of buried reverse fault zone in sedimentary basin: A case from the northwest margin of Junggar Dr. Liu Yin Basin, China Page: 2/7
3 T Rock Deformation and Structural Geology Date Thursday, 01 September 2016 Time 14:00 to 15:30 14:00 14: Deformation characteristics of iron-ore-bodies in Xinyu iron deposit, Central Jiangxi Province and its implication for Dr. Zhengle Chen ore-prospecting 14:15 14: Pseudo mega ring structure in Waterberg sandstone Ms. Carike Pretorius 14:30 14: Carbon Release In Italy Through Volcanic, Tectonic And Other Styles Of Degassing : Implication For Carbon Dioxide Ms. Sabina Bigi Sequestration And Storage. 14:45 15: Gas Bearing faults: how do they work? Ms. Sabina Bigi 15:00 15: The brittle evolution of the Critical Zone across South Africa: Implications for sustainable transformation Mr. Taufeeq Dhansay 15:15 15: Paleomagnetism of the Permian and the Jurassic rocks of the Velebit Mt. and its implication for tectonic history of the Prof. Marek Lewandowski Karst Dinarides (Croatia) Page: 3/7
4 T Rock Deformation and Structural Geology Date Thursday, 01 September 2016 Time 16:00 to 17:45 16:00 16: Intracontinental deformation and reactivation, South Wales Coalfield, UK Dr. Thomas Blenkinsop Keynote 16:30 16: Soft-sediments deformation structures of the Niger River right bank alluviums at Bamako, Mali, and their Mr. N'dji dit Jacques DEMBELE paleoseismic significance 16:45 17: Crustal deformtion characteristics revealed by GPS observations in Guangdong area Dr. Xing Yan 17:00 17: The Trans-European Suture Zone: origin and tectonomagmatic events in late Variscan times Prof. Andrzej Zelazniewicz 17:15 17: Geometry and kinematics of Moyar-Bhavani shear zone (central part), Tamil Nadu India: Characterising a Mr. Siddhartha Karmakar Neoproterozoic oblique transpression 17:30 17: Structural characterization and its implication of deformation timing of the Daerbute strike slip fault Dr. Kongyou Wu Dr. Yangwen Pei Page: 4/7
5 T43.P4 - Rock Deformation and Structural Geology Date Thursday, 01 September 2016 Time 17:45 to 19:00 Chair Room Exhibition 5039 Structural Mapping and Identification of Hydrothermal Alteration Zones Trhough SRTM and ASTER Images in Mr. Manuel Nopeia Macossa, Mozambique 3302 The difference of fracture density and fluid flow characteristics between footwall and hanging wall of a high angle Mr. Taehyung Kim fault 2296 Phyllosilicate occurrence along extensional faults in carbonate rocks and implications for seismic rupture Dr. Luca Smeraglia propagation: case studies from the central Apennines, Italy 1090 The metamorphic basement from the Santander Massif (Colombian Eastern Cordillera): a new stratigraphic Dr. Luis Carlos Mantilla Figueroa framework Dr. Carlos Alberto García Ramirez Dr. Víctor Valencia 5076 En-echelon quartz vein arrays in a progressive dextral transpressional system, Storms River, Eastern Cape, South Dr. Matthew Brayshaw Africa 3341 ANOTHER LOOK AT GEOLOGICAL STRUCTURES OF PART OF THE NANGODI BELT, NORTHEASTERN Ms. Elikplim Dzikunoo GHANA: AN INTEGRATED STRUCTURAL AND GEOPHYSICAL APPROACH 2088 Geophysical Evidence on the Origin of the Caldas Novas Dome Dr. Detlef Walde 3000 Origin of Pseudotachylyte: A case study from the fault zone between the Mangalwar and Sand Mata plutons, central Dr. Gautam Deb Rajasthan, India 2111 A Comparison Between Modeling and Field Observations of Off-Fault Strain around Pseudotachylyte Fault Veins, Ms. Catherine Ross Norumbega Shear Zone, southern Maine 1069 The elusive Rayton Formation in the Khayakhulu area; western Transvaal basin of the North West Province, South Ms. Refilwe Shelembe Africa 2830 Age of folding and relationships of Pai-Hoi Novaya Zemlya and Urals orogenic belts. Dr. Mikhal Shishkin 2672 The effects of tectonic and stratigraphic inherited discontinuities on fault development and their surface evidences Prof. Silvio Seno through analogue models 19 Geological Mapping, Structural Setting and Petrographic Description Of The Archean Volcanic Rocks Of Mnanka Mr. Ezra Kavana Area, North Mara, Tanzania Hydraulic fracturing for plaster under brittle-ductile transition condition Dr. Akihisa KIZAKI 5325 Series of China s metallogenic geological setting maps Mrs. Yanfang Feng Page: 5/7
6 T Rock Deformation and Structural Geology Date Friday, 02 September 2016 Time 08:00 to 10:00 08:00 08: Deformation patterns in the Bagalkot Group of rocks in the intracratonic Kaladgi basin, south western India: A case Dr. Mrinal Kanti Mukherjee of Mesoproterozoic gravity gliding of the cover over the basement during basin uplift 08:15 08: Stress rotation, scale invariance and the locked in stress Dr. Gerrie van Aswegen Keynote 08:45 09: Three Pagoda Fault Zone of the Kanchanaburi region interpreted from airborne geophysical data Dr. Dhiti Tulyatid 09:00 09: D microfabric analysis of progressive, polyphase subglacial deformation beneath the late Weichselian Baltic Ice Dr. Heiko Huneke Stream (Scandinavian Ice Sheet, Europe) Page: 6/7
7 T Rock Deformation and Structural Geology Date Friday, 02 September 2016 Time 10:30 to 12:00 10:30 10: Structural Analysis and Implicit 3D Modelling of High-Grade Host Rocks to the Venetia Kimberlite Diatremes, Central Dr. Ian Basson Zone, Limpopo Belt, South Africa 10:45 11: UPPER CRETACEOUS-TERTIAY STRIKE-SLIP TECTONICS IN NE LIBYA: EVOLUTION WITHIN DEXTRAL Dr. Maher El Amawy SPLAY DUPLEX STRUCTURE 11:00 11: The Record of Subduction and Collision along the Southern Marginal Zone of the Damara Orogen Mr. Michael Hartnady 11:30 11: Caledonides to Cascades Connections: Tectonic evolution of Paleozoic terranes in NW Washington, USA Dr. Elizabeth Schermer Page: 7/7
TECTONIC AND STRUCTURAL CONTROLS ON INTRUSION- RELATED DEPOSITS IN THE NORTHERN PART OF SREDNA GORA ZONE, BULGARIA NIKOLAY PETROV & KAMELIA NEDKOVA
TECTONIC AND STRUCTURAL CONTROLS ON INTRUSION- RELATED DEPOSITS IN THE NORTHERN PART OF SREDNA GORA ZONE, BULGARIA NIKOLAY PETROV & KAMELIA NEDKOVA INVESTIGATED AREA Praveshka Lakavica deposit Elatsite
Global Tectonics. Kearey, Philip. Table of Contents ISBN-13: Historical perspective. 2. The interior of the Earth.
Global Tectonics Kearey, Philip ISBN-13: 9781405107778 Table of Contents Preface. Acknowledgments. 1. Historical perspective. 1.1 Continental drift. 1.2 Sea floor spreading and the birth of plate tectonics.
Deformation of Rocks. Orientation of Deformed Rocks
Deformation of Rocks Folds and faults are geologic structures caused by deformation. Structural geology is the study of the deformation of rocks and its effects. Fig. 7.1 Orientation of Deformed Rocks
KEY CHAPTER 12 TAKE-HOME QUIZ INTERNAL STRUCTURES AND PROCESSES Score Part B = / 55 PART B
GEOLOGY 12 KEY CHAPTER 12 TAKE-HOME QUIZ INTERNAL STRUCTURES AND PROCESSES Score Part B = / 55 PART B CHAPTER 12 Isostacy and Structural Geology 1. Using the terms below, label the following diagrams and
Earth Science, (Tarbuck/Lutgens) Chapter 10: Mountain Building
Earth Science, (Tarbuck/Lutgens) Chapter 10: Mountain Building 1) A(n) fault has little or no vertical movements of the two blocks. A) stick slip B) oblique slip C) strike slip D) dip slip 2) In a(n) fault,
Chapter 15 Structures
Chapter 15 Structures Plummer/McGeary/Carlson (c) The McGraw-Hill Companies, Inc. TECTONIC FORCES AT WORK Stress & Strain Stress Strain Compressive stress Shortening strain Tensional stress stretching
Directed Reading. Section: How Mountains Form MOUNTAIN RANGES AND SYSTEMS. Skills Worksheet
Skills Worksheet Directed Reading Section: How Mountains Form 1. How high is Mount Everest? a. about 1980 km above sea level b. more than 8 km below sea level c. more than 8 km above sea level d. more
Strike-Slip Faults. ! Fault motion is parallel to the strike of the fault.
Strike-Slip Faults! Fault motion is parallel to the strike of the fault.! Usually vertical, no hanging-wall/footwall blocks.! Classified by the relative sense of motion. " Right lateral opposite block
Regional GIS based exploration targeting studies in data poor environments
Regional GIS based exploration targeting studies in data poor environments A case study of gold prospectivity mapping in Nigeria Matthew Greentree, Mathieu Lacorde and Bert De Waele Acknowledgements Australian
Mountains and Mountain Building: Chapter 11
Mountains and Mountain Building: Chapter 11 Objectives: 1)Explain how some of Earth s major mountain belts formed 2) Compare and contrast active and passive continental margins 3) Explain how compression,
EXISTING GEOLOGICAL INFORMATION
CHAPER 3 EXISTING GEOLOGICAL INFORMATION 3-1 General Geology of the Surrounding Area (1) General geology and ore deposits in Mongolia Geographically, Mongolia is a country located between Russia to the
FINAL EXAM Crustal Deformation CONVERGE DIVERGENT PLATES MANTLE PLUMES FLUX BASALTIC GRANITIC
Crustal Deformation Reading: Chapter 10 Pages 283-304 Review Questions 4, 6, 7, 10, 12, 15, 18, 20 FINAL EXAM NOON TO 2 PM, TUESDAY DEC. 5 HERE: Natural Science 101 BRING A SCAN TRON TURN IN YOUR REVIEW
11.1 Rock Deformation
Tarbuck Lutgens Mountain Building 11.1 Rock Deformation Factors Affecting Deformation Factors that influence the strength of a rock and how it will deform include temperature, confining pressure, rock
GLY 155 Introduction to Physical Geology, W. Altermann. Press & Siever, compressive forces. Compressive forces cause folding and faulting.
Press & Siever, 1995 compressive forces Compressive forces cause folding and faulting. faults 1 Uplift is followed by erosion, which creates new horizontal surface. lava flows Volcanic eruptions cover
Structural Geology of the Mountains
Structural Geology of the Mountains Clinton R. Tippett Shell Canada Limited, Calgary, Alberta clinton.tippett@shell.ca INTRODUCTION The Southern Rocky Mountains of Canada (Figure 1) are made up of several
Topics Laramide Orogeny: Late Cretaceous to Early Eocene Reading: GSA DNAG volume 3, Ch. 6
Topics Laramide Orogeny: Late Cretaceous to Early Eocene Reading: GSA DNAG volume 3, Ch. 6 Late Cretaceous to early Eocene New patterns developed 5 main regions Tectonic interpretations Post-Laramide events
Essentials of Geology, 11e
Essentials of Geology, 11e Crustal Deformation and Mountain Building Chapter 17 Instructor Jennifer Barson Spokane Falls Community College Geology 101 Stanley Hatfield Southwestern Illinois College Jennifer
GY111 Earth Materials Practice Final Exam
I. True/False Questions: circle a T for true or F for false (10% total -or- 0.5 per) 1. (T F) The Uranium used in nuclear power plants may explode if not controlled properly. 2. (T F) Natural Gas is an
TS Tectonics & Structural Geology Orals Monday, 28 April
TS Tectonics & Structural Geology Orals Monday, 28 April MO1, 08:30 10:00 MO2, 10:30 12:00 MOL, 12:15 13:15 MO3, 13:30 15:00 MO4, 15:30 17:00 GD3.2/TS9.7, Recent advances in computational geodynamics (co-organized),
TS Tectonics & Structural Geology Orals and PICOs Monday, 08 April
TS Tectonics & Structural Geology Orals and PICOs Monday, 08 April MO1, 08:30 10:00 MO2, 10:30 12:00 MOL, 12:15 13:15 MO3, 13:30 15:00 MO4, 15:30 17:00 GD3.3/GM3.3/GMPV16/TS4.7, The evolution of plate
Deformation of the Crust
Deformation of the Crust Review Choose the best response. Write the letter of that choice in the space provided. 1. The state of balance between the thickness of the crust and the depth at which it rides
Mountain Building. Mountain Building
Mountain Building Mountain building has occurred during the recent geologic past American Cordillera the western margin of the Americas from Cape Horn to Alaska Includes the Andes and Rocky Mountains Alpine
Chapter 10: Deformation and Mountain Building. Fig. 10.1
Chapter 10: Deformation and Mountain Building Fig. 10.1 OBJECTIVES Describe the processes of rock deformation and compare and contrast ductile and brittle behavior in rocks. Explain how strike and dip
Preface and Overview. Folded strata in the mountains of Italy (ca AD), Leonardo da Vinci
Preface and Overview Folded strata in the mountains of Italy (ca. 1500 AD), Leonardo da Vinci Models of Mountain Building and Associated Deformation as represented by G.P. Scrope Deformation Feature: Scales
Learning Objectives (LO) What we ll learn today:!
Learning Objectives (LO) Lecture 13: Mountain Building Read: Chapter 10 Homework #11 due Tuesday 12pm What we ll learn today:! 1. Define the types of stress that are present in the crust! 2. Define the
Evolution of Continents Chapter 20
Evolution of Continents Chapter 20 Does not contain complete lecture notes. Mountain belts Orogenesis the processes that collectively produce a mountain belt Includes folding, thrust faulting, metamorphism,
TECHNICAL REPORT: REGIONAL GEOLOGY AND TECTONICS Resume. Huachon Project, Cerro de Pasco departments, Peru. By: AFC Logistic SAC
TECHNICAL REPORT: REGIONAL GEOLOGY AND TECTONICS Resume Huachon Project, Cerro de Pasco departments, Peru By: AFC Logistic SAC December 2016 1. INTRODUCTION GPM Metals Peru, in its portfolio of generating
NATURAL ENVIRONMENT. Geophysics
NATURAL ENVIRONMENT Geophysics Geodynamics Alpine, Carpathian and Dinaric mountain belts surround the Pannonian (Carpathian) Basin, of Neogene through Quaternary in age. The Cenozoic evolution of the Alpine-Pannonian
Chapter 16. Mountain Building. Mountain Building. Mountains and Plate Tectonics. what s the connection?
Chapter 16 Mountains and Plate Tectonics what s the connection? Mountain Building Most crustal deformation occurs along plate margins. S.2 Active Margin Passive Margin Mountain Building Factors Affecting
Answers: Internal Processes and Structures (Isostasy)
Answers: Internal Processes and Structures (Isostasy) 1. Analyse the adjustment of the crust to changes in loads associated with volcanism, mountain building, erosion, and glaciation by using the concept
Description of faults
GLG310 Structural Geology Description of faults Horizontal stretch Crustal thickness Regional elevation Regional character Issues Normal Thrust/reverse Strike-slip >1 1 in one direction and < 1 in
Copyright McGraw-Hill Education. All rights reserved. No reproduction or distribution without the prior written consent of McGraw-Hill Education
Copyright McGraw-Hill Education. All rights reserved. No reproduction or distribution without the prior written consent of McGraw-Hill Education Tibetan Plateau and Himalaya -southern Asia 11.00.a VE 10X
Crags, Cracks, and Crumples: Crustal Deformation and Mountain Building
Crags, Cracks, and Crumples: Crustal Deformation and Mountain Building Updated by: Rick Oches, Professor of Geology & Environmental Sciences Bentley University Waltham, Massachusetts Based on slides prepared
Chapter. Mountain Building
Chapter Mountain Building 11.1 Rock Deformation Factors Affecting Deformation Factors that influence the strength of a rock and how it will deform include temperature, confining pressure, rock type, and
Geology 15 West Valley College. Exam IV: Sierra Nevada
Geology 15 West Valley College Name Exam IV: Sierra Nevada 1) On the diagram above, where is the Arc- Trench Gap? a. 1 and 3 c. 7 and 8 d. 6 e. 5 and 10 2) On the diagram above, where is the subduction
Stress and Strain. Stress is a force per unit area. Strain is a change in size or shape in response to stress
Geologic Structures Geologic structures are dynamically-produced patterns or arrangements of rock or sediment that result from, and give information about, forces within the Earth Produced as rocks change
GOLD IN MANITOBA SHORT COURSE
November 20-22 GOLD IN MANITOBA SHORT COURSE D. Lentz Developing the Orogenic Gold Deposit Model: Insights from R&D for Exploration Success View Abstract B. Lafrance Structural Controls on Hydrothermal
UNIVERSITY OF PRETORIA Department of Geology HISTORICAL GEOLOGY - GLY 161 SEMESTER EXAM
UNIVERSITY OF PRETORIA Department of Geology HISTORICAL GEOLOGY - GLY 161 SEMESTER EXAM Internal examiner: Dr A.J. Bumby. External examiner: Prof. P.G. Eriksson Copyright Reserved 20 th November 2009 Time:
Course Title: Discipline: Geology Level: Basic-Intermediate Duration: 5 Days Instructor: Prof. Charles Kluth. About the course: Audience: Agenda:
Course Title: Structural Geology Discipline: Geology Level: Basic-Intermediate Duration: 5 Days Instructor: Prof. Charles Kluth About the course: This course covers the basic ideas of structural geometry
NAME HOMEWORK ASSIGNMENT #4 MATERIAL COVERS CHAPTERS 19, 20, 21, & 2
NAME HOMEWORK ASSIGNMENT #4 MATERIAL COVERS CHAPTERS 19, 20, 21, & 2 Assignment is due the beginning of the class period on December 14, 2004. Mark answers on a scantron sheet, which will be provided.
Parts of the Sevier/ Laramide Orogeny
Parts of the Sevier/ Laramide Orogeny AA. Accretionary Prism BB. Forearc Basin Sediment scraped off of subducting plate Sediment derived from the volcanic arc CC. Volcanic Arc Magmatic intrusion into the
The continental lithosphere
Simplicity to complexity: The continental lithosphere Reading: Fowler p350-377 Sampling techniques Seismic refraction Bulk crustal properties, thickness velocity profiles Seismic reflection To image specific
Contractional Tectonics: Convergence and Collision
Contractional Tectonics: Convergence and Collision Processes in Structural Geology & Tectonics Ben van der Pluijm WW Norton+Authors, unless noted otherwise 4/12/2017 5:21 PM We Discuss Contractional Tectonics
Section 2: How Mountains Form
Section 2: How Mountains Form Preview Objectives Mountain Ranges and Systems Plate Tectonics and Mountains Types of Mountains Objectives Identify the types of plate collisions that form mountains. Identify
GEOL 321 Structural Geology and Tectonics
GEOL 321 Structural Geology and Tectonics Geology 321 Structure and Tectonics will be given in Spring 2017. The course provides a general coverage of the structures produced by brittle and ductile rock
Study the architecture and processes responsible for deformation of Earth s crust. Folding and Faulting
Crustal Deformation AKA Structural geology (adapted from Brunkel, 2012) Study the architecture and processes responsible for deformation of Earth s crust. Folding and Faulting How Rocks Deform: 4 Controls
Orphan Basin, Offshore Newfoundland: New seismic data and hydrocarbon plays for a dormant Frontier Basin
Orphan Basin, Offshore Newfoundland: New seismic data and hydrocarbon plays for a dormant Frontier Basin Jerry Smee* G&G Exploration Consulting, 301 400-3rd Avenue SW, Calgary, AB, T2P 4H2 Sam Nader, Paul
Continental Margin Geology of Korea : Review and constraints on the opening of the East Sea (Japan Sea)
Continental Margin Geology of Korea : Review and constraints on the opening of the East Sea (Japan Sea) Han-Joon Kim Marine Satellite & Observation Tech. Korea Ocean Research and Development Institute
COMPOSITION and PHYSICAL PROPERTIES GENERAL SUBJECTS. GEODESY and GRAVITY
COMPOSITION and PHYSICAL PROPERTIES Composition and structure of the continental crust Composition and structure of the core Composition and structure of the mantle Composition and structure of the oceanic
Before Plate Tectonics: Theory of Continental Drift
Before Plate Tectonics: Theory of Continental Drift Predecessor to modern plate tectonics Shape and fit of the continents was the initial evidence Snider-Pelligrini (1858) Taylor (1908) Wegner (1915) Fig.
Cretaceous Tertiary Contraction, Shear and Inversion in the Western Barents Sea
Cretaceous Tertiary Contraction, Shear and Inversion in the Western Barents Sea Roy H. Gabrielsen,* Jan Inge Faleide*, Karen A. Leever*,** * Department of Geosciences, University of Oslo GeoForschungZentrum
Geologic Structures. Changes in the shape and/or orientation of rocks in response to applied stress
Geologic Structures Changes in the shape and/or orientation of rocks in response to applied stress Figure 15.19 Can be as big as a breadbox Or much bigger than a breadbox Three basic types Fractures >>>
GY111 Earth Materials Practice Final Exam
I. True/False Questions: circle a T for true or F for false (10% total -or- 0.5 per) (Correct answer in red) 1. (T F) The Uranium used in nuclear power plants may explode if not controlled properly. 2.
Section 10.1 The Nature of Volcanic Eruptions This section discusses volcanic eruptions, types of volcanoes, and other volcanic landforms.
Chapter 10 Section 10.1 The Nature of Volcanic Eruptions This section discusses volcanic eruptions, types of volcanoes, and other volcanic landforms. Reading Strategy Previewing Before you read the section,
08GSA, James McLelland Symposium
Ben van der Pluijm and Eric Tohver with Eric Essene, and Jay Busch, Michael Cosca, James Cureton, Katherine Carlson, Jerry Magloughlin, Klaus Mezger, Mark Rathmell, Margaret Streepey, Mary Ellen Tuccillo.
Exam Deformatie en Metamorfose van de Korst Educatorium zaal ALFA
Naam Studentnummer... Exam Deformatie en Metamorfose van de Korst Educatorium zaal ALFA Do not forget to put your name and student number on each of the question and answer sheets and to return both of
Questions and Topics
Plate Tectonics and Continental Drift Questions and Topics 1. What are the theories of Plate Tectonics and Continental Drift? 2. What is the evidence that Continents move? 3. What are the forces that
December 21, Chapter 11 mountain building E.notebook. Feb 19 8:19 AM. Feb 19 9:28 AM
Mountains form along convergent plate boundaries. Typically (usually) if you look at a mountain range, you know that it is at a plate boundary (active continental margin) or has been some time in the past
Chapter 3. Geology & Tectonics
Chapter 3 Geology & Tectonics 3.1 Geology The general geological features of Indonesia are shown in Figure 3.1. The basement formation is metamorphic and it is intruded with plutonic formations. They are
FINAL EXAM Crustal Deformation CONVERGE DIVERGENT PLATES MANTLE PLUMES FLUX BASALTIC GRANITIC
Crustal Deformation Reading: Chapter 10 Pages 283-294 FINAL EXAM 8 to 10 AM, THURSDAY DEC. 6 HERE: Natural Science 101 BRING A SCAN TRON TURN IN YOUR REVIEW QUESTIONS BEFORE THE TEST, PICK UP WHEN YOU
Fault Architecture, Associated Structures and Uranium Mineralization, Eastern Athabasca Basin: A Provisional Empirical Classification
December 2014 Fault Architecture, Associated Structures and Uranium Mineralization, Eastern Athabasca Basin: A Provisional Empirical Classification David Thomas, Alex Aubin, Dan Brisbin, Joshua Mukwakwami,
What Causes Rock to Deform?
Crustal Deformation Earth, Chapter 10 Chapter 10 Crustal Deformation What Causes Rock to Deform? Deformation is a general term that refers to all changes in the shape or position of a rock body in response
HIGH GRADE GOLD-BEARING QUARTZ VEIN DISCOVERED AT MIAREE, KARRATHA AREA WESTERN AUSTRALIA
17 November 2010 Company Announcements Office Australian Stock Exchange Limited 20 Bridge Street SYDNEY NSW 2000 HIGH GRADE GOLD-BEARING QUARTZ VEIN DISCOVERED AT MIAREE, KARRATHA AREA WESTERN AUSTRALIA
3. GEOLOGY. 3.1 Introduction. 3.2 Results and Discussion Regional Geology Surficial Geology Mine Study Area
3. GEOLOGY 3.1 Introduction This chapter discusses the baseline study of the geology and mineralization characteristics of the mine study area. The study consolidates existing geological data and exploration
University of Leeds 3GP Geophysics Field Trip Lake Balaton, Hungary
University of Leeds 3GP Geophysics Field Trip Lake Balaton, Hungary September 1-15, 2007 geological background and logistics Staff: Greg Houseman, Graham Stuart The Alpine-Carpathian-Pannonian System Elevation
Hints of active deformation in the southern Adriatic foreland: Holocene tectonics along the Apulia offshore (Italy)
Hints of active deformation in the southern Adriatic foreland: Holocene tectonics along the Apulia offshore (Italy) Domenico Ridente^, Umberto Fracassi*, Daniela Di Bucci, Fabio Trincardi^ ^ & Gianluca
Lecture Outlines PowerPoint. Chapter 10 Earth Science, 12e Tarbuck/Lutgens
Lecture Outlines PowerPoint Chapter 10 Earth Science, 12e Tarbuck/Lutgens 2009 Pearson Prentice Hall This work is protected by United States copyright laws and is provided solely for the use of instructors
History of Earth. Chapter 9: HISTORY OF EARTH. The Solar System. Early Earth: A Giant Impact! Early Earth. Formation of the Solar System
Chapter 9: HISTORY OF EARTH The Essential Earth, 2 nd Edition Thomas H. Jordan & John Grotzinger History of Earth Earth is 4.56 Billion Years Old Earth has experienced a rich and diverse history that we
The Tectonic Setting of New Zealand
The Tectonic Setting of New Zealand we are here Subduction-driven tectonics The New Zealand continent Papua New Guinea Australia 3,000,000 sq km micro-continent back-arc basin trench volcanism faults accretionary
Lecture Outline Friday March 2 thru Wednesday March 7, 2018
Lecture Outline Friday March 2 thru Wednesday March 7, 2018 Questions? Lecture Exam Friday March 9, 2018 Same time, Same room Bring Pencils and WSU ID 50 question Multiple Choice, Computer Graded Interlude
(1) Identify 5 major principles of relative dating? For each principle, describe how you tell what is younger and what is older.
Things to Know - Third GLG101Exam Page 1 Important Note: This is not everything you need to know or study. However, it provides you with a relatively comprehensive list of questions to help you study.
Chapter 10: Volcanoes and Other Igneous Activity Section 1: The Nature of Volcanic Eruptions I. Factors Affecting Eruptions Group # Main Idea:
Chapter 10: Volcanoes and Other Igneous Activity Section 1: The Nature of Volcanic Eruptions I. Factors Affecting Eruptions Group # A. Viscosity Group # B. Dissolved Gases Group # II. Volcanic Material
GENERAL GEOLOGY Fall Chapter 18: The Sea Floor. Partial Examination IV Study Guide Dr. Glen S. Mattioli
GENERAL GEOLOGY 1113-005 Fall 2008 Partial Examination IV Study Guide Dr. Glen S. Mattioli Note that these are NOT questions, but rather are a list of topics that we have covered either in class or are
Introduction to Prospecting. Session Two Geology
Introduction to Prospecting Session Two Geology The Earth Earth is 4.6 billion years old (Ba). Bacteria & algae +3.5 Ba. Microscopic animals ~2 Ba. Animals ~600 million years (Ma) old. Mankind about 100,000
RELINQUISHMENT REPORT. License P1546 Block April 2009
RELINQUISHMENT REPORT License P1546 Block 110-01 14 April 2009 Sherritt International Oil and Gas Limited 2000, 425-1 st street S.W., Calgary, Alberta Canada T2P 3L8 Telephone (403) 260-2900 Fax (403)
L.K. Carr 1, R.J. Korsch 1, A.J. Mory 2, R.M. Hocking 2, S.K. Marshall 1, R.D. Costelloe 1, J. Holzschuh 1, J.L. Maher 1. Australia.
STRUCTURAL AND STRATIGRAPHIC ARCHITECTURE OF WESTERN AUSTRALIA S FRONTIER ONSHORE SEDIMENTARY BASINS: THE WESTERN OFFICER AND SOUTHERN CARNARVON BASINS L.K. Carr 1, R.J. Korsch 1, A.J. Mory 2, R.M. Hocking
Geological & Geophysical Interpretation of ZTEM EM and Magnetic Survey. Kemess Project, BC. for AuRico Metals Inc. September, 2016 Nicole Pendrigh
Geological & Geophysical Interpretation of ZTEM EM and Magnetic Survey Kemess Project, BC for AuRico Metals Inc. September, 2016 Nicole Pendrigh SUMMARY REPORT Regional setting Located in North central
Activity Pacific Northwest Tectonic Block Model
Activity Pacific Northwest Tectonic Block Model The Cascadia tectonic margin is caught between several tectonic forces, during the relentless motions of the giant Pacific Plate, the smaller subducting
Crustal Deformation. Earth Systems 3209
Crustal Deformation Earth Systems 3209 Crustal Deformation pg. 415 Refers to all changes in the original form and/or size of a rock body. May also produce changes in the location and orientation of rocks.
Overview of the Seismic Source Characterization for the Palo Verde Nuclear Generating Station
Overview of the Seismic Source Characterization for the Palo Verde Nuclear Generating Station Scott Lindvall SSC TI Team Lead Palo Verde SSC SSHAC Level 3 Project Tuesday, March 19, 2013 1 Questions from
CHAPTER 5.0 STRUCTURAL GEOLOGY AND VEINS SYSTEM. Penjom is classified as orogenic gold (Flindell, 2003) after Groves et al.
CHAPTER 5.0 STRUCTURAL GEOLOGY AND VEINS SYSTEM 5.1 Introduction Penjom is classified as orogenic gold (Flindell, 2003) after Groves et al. (1999) and has many characteristics that are common with other
predictive mineral discovery*cooperative Research Centre A legacy for mineral exploration science Mineral Systems Q1 Architecture
Mineral Systems Q1 Architecture 1 Key Parameter Mineral System Exploration is reflected in scale-dependent translation A. Gradient in hydraulic potential B. Permeability C. Solubility sensitivity to P,
Mineral Systems modelling in the Mount Isa Inlier, and its use in identification of permissive tracts for copper and lead/zinc mineralisation.
Department of Natural Resources and Mines Mineral Systems modelling in the Mount Isa Inlier, and its use in identification of permissive tracts for copper and lead/zinc mineralisation. L.J.Hutton Geological
UNIT 10 MOUNTAIN BUILDING AND EVOLUTION OF CONTINENTS
UNIT 10 MOUNTAIN BUILDING AND EVOLUTION OF CONTINENTS ROCK DEFORMATION Tectonic forces exert different types of stress on rocks in different geologic environments. STRESS The first, called confining stress
SCIENCE CHINA Earth Sciences
SCIENCE CHINA Earth Sciences RESEARCH PAPER September 2011 Vol.54 No.9: 1386 1393 doi: 10.1007/s11430-011-4177-2 Crustal P-wave velocity structure of the Longmenshan region and its tectonic implications
Mark Legg COASTAL DEFORMATION AND TECTONIC EVOLUTION OFFSHORE SAN ONOFRE
COASTAL DEFORMATION AND TECTONIC EVOLUTION OFFSHORE SAN ONOFRE August 2013 Coastal Deformation and Tectonic Evolution Offshore San Onofre Mark R. Legg Legg Geophysical, Inc. The true sign of intelligence
USU 1360 TECTONICS / PROCESSES
USU 1360 TECTONICS / PROCESSES Observe the world map and each enlargement Pacific Northwest Tibet South America Japan 03.00.a1 South Atlantic Arabian Peninsula Observe features near the Pacific Northwest
Interaction between Faults and Igneous Intrusions in Sedimentary Basins: Insights from 3D Seismic Reflection Data*
Interaction between Faults and Igneous Intrusions in Sedimentary Basins: Insights from 3D Seismic Reflection Data* Craig Magee¹, Christopher A. Jackson¹, and Nick Schofield² Search and Discovery Article
Crystalline rocks in the Patterson Lake corridor: implications for uranium deposit genetic models. Colin D. Card
Crystalline rocks in the Patterson Lake corridor: implications for uranium deposit genetic models Colin D. Card Acknowledgements Forum Uranium Purepoint Uranium Fission Uranium Geological Survey of Canada
ANOTHER MEXICAN EARTHQUAKE! Magnitude 7.1, Tuesday Sept. 19, 2017
ANOTHER MEXICAN EARTHQUAKE! Magnitude 7.1, Tuesday Sept. 19, 2017 Why is there no oceanic crust older than 200 million years? SUBDUCTION If new oceanic crust is being continuously created along the earth
Composition of the earth, Geologic Time, and Plate Tectonics
Composition of the earth, Geologic Time, and Plate Tectonics Layers of the earth Chemical vs. Mechanical Chemical : Mechanical: 1) Core: Ni and Fe 2) Mantle: Mostly Peridotite 3) Crust: Many different
CRUSTAL DEFORMATION. Chapter 10
CRUSTAL DEFORMATION and dgeologic Structures t Chapter 10 Deformation Df Deformation involves: Stress the amount of force applied to a given area. Types of Stress: Confining Stress stress applied equally
Northern Tanzanian Earthquakes: Fault orientations, and depth distribution
Northern Tanzanian Earthquakes: Fault orientations, and depth distribution Stewart Rouse (NC A&T Physics) Penn State University SROP Mentors: Dr. Andy Nyblade & Dr. Rick Brazier July 27, 2005 1.0 Introduction
CHAPTER 8. TUVA AND WEST-SAYAN
169 CHAPTER 1. THEORY OF FAULTING AND EVALUATION OF TIMING OF FAULT MOVEMENTS: METHODOLOGY CHAPTER 2. NEOTECTONICS OF ALTAI-SAYAN CHAPTER 3. GEOLOGICAL AND GEODYNAMICAL SETTINGS CHAPTER 4. THE TELETSK
QUALITATIVE INTERPRETATION OF POTENTIAL FIELD PROFILES: SOUTHERN NECHAKO BASIN
QUALITATIVE INTERPRETATION OF POTENTIAL FIELD PROFILES: SOUTHERN NECHAKO BASIN By Melvyn E. Best Bemex Consulting International 5288 Cordova Bay Road Victoria, B.C. V8Y 2L4 KEYWORDS: potential fields,
The Building of the NYC Region
The Building of the NYC Region Definitions Fall Line marks the area where an upland region (continental bedrock) and a coastal plain meet Piedmont the plateau region of the eastern United States which
Structural geology and gold metallogeny of the New Britannia mine area, Snow Lake, Manitoba
Structural geology and gold metallogeny of the New Britannia mine area, Snow Lake, Manitoba Chris Beaumont-Smith Manitoba Geological Survey Boundary zone New Britannia Trans-Hudson Orogen 50 km 100 km
Quaternary clays alluvial sands of the Shepparton Formation overlie the basement rocks.
NAGAMBIE GOLDFIELD Regional Geological Setting The Nagambie Project is located within the Melbourne Structural Zone of Victoria. The lithologies range in age from the Upper Silurian Broadford Formation
How to Build a Mountain and other Geologic Structures. But first a short review
How to Build a Mountain and other Geologic Structures But first a short review Where do we see deep earthquakes? What is happening there? What can happen at a plate boundary? 1. Plates can move apart
Non-ideal Subduction
Subduction zone cross sections Earthquake locations : black = teleseismic est. gray = local-array est. red line = top of slab seismicity blue line = center of slab seismicity Non-ideal Subduction Oblique