APPENDIX D FAULT SLIP DATA AND SENSE OF SHEAR DETERMINED IN FOLIATED AND MYLONITIC ROCKS FROM THE WILD ROGUE WILDERNESS, SW OREGON

Figure 4.1 Undeformed diabase dike cutting mylonitized gabbro of Shear Zone VII. 44 Figure 4.5 Typical shear zone boundary. Unfoliated gabbro to the left, strongly foliated mylonite

lecture 8 Shear zones Kristallingeologie Summary lecture on foliations Faults and shear zones Strength of the crust

Kristallingeologie lecture 8 Shear zones Summary lecture on foliations Rocks can contain foliations and lineations Some important foliations Primary foliation (S 0 ), Axial planar & crenulation cleavage

Shear Zones and Mylonites

Shear Zones and Mylonites A shear zone is a tabular zone in which strain is notably higher than in the surrounding rock. Simplified model of the connection between faults, which normally form in the upper

Hand specimen descriptions of metamorphic rocks

Hand specimen descriptions of metamorphic rocks Hand specimen descriptions for metamorphic rocks are like those for igneous rocks. The objective is to tell someone looking at it everything they need to

APPENDIX 2 Table 2. Sample descriptions

Table 2. descriptions 225 Felsic gneiss, fine-grained and very light-gray. From the upper part of the lower of the two layers, which connect. 226 Amphibolite, even-grained, fine-grained, medium-gray, little

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

Supplement of Pinch and swell structures: evidence for strain localisation by brittle viscous behaviour in the middle crust

Supplement of Solid Earth, 6, 1045 1061, 2015 http://www.solid-earth.net/6/1045/2015/ doi:10.5194/se-6-1045-2015-supplement Author(s) 2015. CC Attribution 3.0 License. Supplement of Pinch and swell structures:

Testing the transpression hypothesis in the western part of the Cheyenne belt, Medicine Bow Mountains, southeastern Wyoming

Testing the transpression hypothesis in the western part of the Cheyenne belt, Medicine Bow Mountains, southeastern Wyoming W. A. Sullivan 1*, R. J. Beane 2, E. N. Beck 1, W. H. Fereday 1, A. M. Roberts-Pierel

Zone" Microstructures and

Textures and Microstructures, 1982, Vol. 5, pp. 33-61 0730-3300/82/0501-0033 $06.50/0 (C) Gordon and Breach Science Publishers Inc., 1982 Printed in Great Britain Fault Rocks of the Moine Thrust Zone"

A-13R-CC (24-25 cm) No. 38 OBSERVER: SKE, RUB, MAN, BES ROCK NAME: Amphibolite. GRAIN SIZE: Medium-grained. TEXTURE: Elongated amphibole

173-1067A-13R-CC (24-25 cm) No. 38 OBSERVER: SKE, RUB, MAN, BES ROCK NAME: Amphibolite. TEXTURE: Elongated amphibole grains displaying preferred orientation. NAME MODE (%) SIZE (mm) SHAPE COMMENTS Amphibole

Provided by Tasa Graphic Arts, Inc. for An Introduction to Structural Methods DVD-ROM

Provided by Tasa Graphic Arts, Inc. for An Introduction to Structural Methods DVD-ROM http://www.tasagraphicarts.com/progstruct.html AN INTRODUCTION TO STRUCTURAL METHODS - DETAILED CONTENTS: (Navigate

Strength variation and deformational behavior in anisotropic granitic mylonites under high-temperature and -pressure conditions An experimental study

Strength variation and deformational behavior in anisotropic granitic mylonites under high-temperature and -pressure conditions An experimental study Gui Liu, Yongsheng Zhou, Yaolin Shi, Sheqiang Miao,

UNIVERSITY OF PRETORIA Department of Geology STRUCTURAL GEOLOGY -GLY 254 SEMESTER EXAM

UNIVERSITY OF PRETORIA Department of Geology STRUCTURAL GEOLOGY -GLY 254 SEMESTER EXAM Copyright reserved 6 th June 2006 Time: 3 hours Internal examiner: Dr A.J. Bumby External examiner: Dr R. van der

Core Photo. Site 1111 Hole A Core 2R Rec. 0.73% mbsf

VISUAL CORE DESCRIPTIONS, SITE 1111 1 1111A-2R message openfile IMAGES/1111A2R.PDF 1111A-1R NO RECOVERY Site 1111 Hole A Core 2R Rec. 0.73% 10.1-19.7 mbsf GRAIN SIZE METERS 1 SECTION granule very coarse

An unusual 'crack--seal' vein geometry

Journal of Structural Geology, Vol. 6, No. 5, pp. 593 to 597, 1984 0191--8141/84 $3.00 + 0.00 Printed in Great Britain Pergamon Press Ltd. An unusual 'crack--seal' vein geometry BEN A. VAN DER PLUJM Department

Lithology: Olivine-rich gabbro medium grained Observer: Texture: granular Ave. grain size: medium grained [345] Shape Habit Comments

THIN SECTION LABEL ID: 179-1105A-1R-2-W 88/91-TSB-TSS Piece no.: #02 TS no.: Igneous Medium-grained olivine gabbronorite; plagioclase chadacryst within orthopyroxene oikocryst; rims of olivine and clinopyroxene

Structural Geology and Geology Maps Lab

Structural Geology and Geology Maps Lab Mesa College Geology 101 Lab Ray Rector: Instructor Structural Geology Lab Pre-Lab Resources Pre-Lab Internet Links 1) Fundamentals of Structural Geology 2) Visualizing

Faults. Strike-slip fault. Normal fault. Thrust fault

Faults Strike-slip fault Normal fault Thrust fault Fault any surface or narrow zone with visible shear displacement along the zone Normal fault Strike-slip fault Reverse fault Thrust fault

12. MYRMEKITE IN THE SANTA ROSA MYLONITE ZONE, PALM SPRINGS, CALIFORNIA

1 ISSN 1526-5757 12. MYRMEKITE IN THE SANTA ROSA MYLONITE ZONE, PALM SPRINGS, CALIFORNIA Lorence G. Collins email: lorencec@sysmatrix.net February 15, 1997 Introduction Myrmekite, containing tiny quartz

Answer sheet for question 1 Answer question 1 as soon as the sample arrives at your desk.

EAS 233 Geologic structures. Final test. April 2012. 3 hours. Answer question 1 and 2 and three other questions. If you start more than the required number of questions, clearly delete the answers you

Geology 3120: Fault Rocks. Brittle shear zone, CO Natl Mon

Geology 3120: Fault Rocks Brittle shear zone, CO Natl Mon Outline Fault rocks and strength Fault zone processes Fault rocks Example from Death Valley Fault Rocks and Strength Brittle Fault Zone Processes

EESC 4701: Igneous and Metamorphic Petrology METAMORPHIC ROCKS LAB 8 HANDOUT

Sources: Caltech, Cornell, UCSC, TAMIU Introduction EESC 4701: Igneous and Metamorphic Petrology METAMORPHIC ROCKS LAB 8 HANDOUT Metamorphism is the process by which physical and chemical changes in a

Question 1: Examine the following diagram:

Question 1: Examine the following diagram: 1a.) Which of the illustrated faults is a left-handed strike-slip fault? = a 1b.) Which of the illustrated faults is a normal-slip fault? = e 1c.) Which of the

Deformation mechanisms in mylonites at Fletcher Peak, Washington County, ME

Colby College Digital Commons @ Colby Honors Theses Student Research 2014 Deformation mechanisms in mylonites at Fletcher Peak, Washington County, ME Ariana S. Boyd Colby College Follow this and additional

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,

Lecture 6 Folds, Faults and Deformation Dr. Shwan Omar

Fold: A fold is a bend or wrinkle of rock layers or foliation; folds form as a sequence of ductile deformation. Folding is the processes by which crustal forces deform an area of crust so that layers of

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

Chapter - IV PETROGRAPHY. Petrographic studies are an integral part of any structural or petrological studies in

Chapter - IV PETROGRAPHY 4.1. Introduction Petrographic studies are an integral part of any structural or petrological studies in identifying the mineral assemblages, assigning nomenclature and identifying

Metamorphism (means changed form

Metamorphism (means changed form) is recrystallization without melting of a previously existing rock at depth in response to a change in the environment of temperature, pressure, and fluids. Common minerals

Learning goals - January 16, Describe the geometry of a fault (1) orientation of the plane (strike and dip) (2) slip vector

Learning goals - January 16, 2012 You will understand how to: Describe the geometry of a fault (1) orientation of the plane (strike and dip) (2) slip vector Understand concept of slip rate and how it is

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

Lab 7: STRUCTURAL GEOLOGY FOLDS AND FAULTS

Lab 7: STRUCTURAL GEOLOGY FOLDS AND FAULTS This set of labs will focus on the structures that result from deformation in earth s crust, namely folds and faults. By the end of these labs you should be able

Figure 1. Regional map from Roure and Blanchet (1983), Blake et al. (1982, 1985a), and G. Harper and M. Giaramita (unpublished mapping). Mineral Hill and Saddle Mountain greenstone blocks are blocks in

EAS FINAL EXAM

EAS 326-03 FINAL EXAM This exam is closed book and closed notes. It is worth 150 points; the value of each question is shown at the end of each question. At the end of the exam, you will find two pages

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

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

Satulinmäki Au Prospect Structural Mapping

M19/2024/2003/1/10 Juhani Ojala Satulinmäki Au Prospect Structural Mapping V. Juhani Ojala Geological Survey of Finland 1 Table of Contents Introduction...2 Local geology...2 Structures...2 Discussion...2

Part 2: Metamorphic features. Foliation, cleavage, lineation. Chapter 15

Part 2: Metamorphic features Chapter 15 Foliation, cleavage, lineation The terms foliation and cleavage in metamorphic rocks have formal definitions, but their colloquial use in the field is commonly haphazard

Table 5.1 Recognised senses of shear from locations in SE NPHM & Dichil/E. Astor

Table 5.1 Table 5.1 Recognised senses of shear from locations in SE NPHM & Dichil/E. Astor 200 Table 5.1 Recognised senses of shear from locations in SE NPHM & Dichil/E. Astor Area / loction no. Sinistral

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

DETAILED STRUCTURAL ANALYSIS OF THE JOHNSON SHEAR ZONE IN THE WEST GEMMELL LAKE AREA (NTS 64C/11) by C.J. Beaumont-Smith and C.D.

GS-13 DETAILED STRUCTURAL ANALYSIS OF THE JOHNSON SHEAR ZONE IN THE WEST GEMMELL LAKE AREA (NTS 64C/11) by C.J. Beaumont-Smith and C.D. Edwards 1 Beaumont-Smith, C.J. and Edwards, C.D. 2000: Detailed structural

shear zones Ductile shear zones can develop as a results of shearing (simple shear strain) or "squeezing" (pure shear strain).

shear zones Ductile shear zones can develop as a results of shearing (simple shear strain) or "squeezing" (pure shear strain). Shear Zones Mylonite, or mylonitic zone is the central part of the shear zone

STRUCTURE AND METAMORPHISM

STRUCTURE AND METAMORPHISM STRUCTURE The area contains a single regional foliation that is inhomogeneously developed. Within the Lushs Bight Group the foliation is restricted to tuffaceous units, pillow

Thermal evolution of the Sisters shear zone, southern New Zealand: Formation of the Great South Basin and onset of Pacific-Antarctic spreading

Click Here for Full Article Thermal evolution of the Sisters shear zone, southern New Zealand: Formation of the Great South Basin and onset of Pacific-Antarctic spreading Joseph Kula, 1,2 Andy J. Tulloch,

G 3. AN ELECTRONIC JOURNAL OF THE EARTH SCIENCES Published by AGU and the Geochemical Society

Geosystems G 3 AN ELECTRONIC JOURNAL OF THE EARTH SCIENCES Published by AGU and the Geochemical Society Article Volume 11, Number 4 3 April 2010 Q04002, doi: ISSN: 1525-2027 Click Here for Full Article

GEOLOGY 470 FIELD EXERCISE 3, SPRING SKETCHING, DESCRIBING, AND MAPPING EXPOSURES

GEOLOGY 470 FIELD EXERCISE 3, SPRING 2009 -- SKETCHING, DESCRIBING, AND MAPPING EXPOSURES 1 OBJECTIVES: To develop and refine your field skills in: 1. observation and rock and sediment description 2. sketching

Blocks Module Content Guide

Blocks Module Content Guide This guide covers the basics of the content within the Interactive 3D Geologic Blocks Module. The content guide is intended to assist you, the teacher, in creating effective

Metamorphic Petrology. Jen Parks ESC 310, x6999

Metamorphic Petrology Jen Parks ESC 310, x6999 jeparks@sciborg.uwaterloo.ca Definition of Metamorphism The IUGS-SCMR SCMR definition of metamorphism: Metamorphism is a subsolidus process leading to changes

Fault Rocks. EARS5136 slide 1

Fault Rocks EARS5136 slide 1 Fault rocks Fault rock types Examples of deformation features in cores Microstructures Porosity and permeability Lithological and lithification control EARS5136 slide 2 Deformation

1-6 Figure 1.3. View of the field area, looking south-southwest. Left side of the picture shows the steep flank of the Green Mountain massif. The Vermont Valley and the Tinmouth Valley are separated by

Controls on Strain Partitioning in the White Horse Creek Mylonite, West Coast, New Zealand Michelle Gavel

1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 Controls on Strain Partitioning in the White Horse Creek Mylonite, West Coast, New Zealand Michelle Gavel Abstract The White Horse Creek Mylonites (WHC)

Michael J Kalczynski. Alexander E Gates

Hydrothermal Mass Transfer and Magnetite Mineralization in Dilational Shear Zones, western Hudson Highlands, NY Michael J Kalczynski & Alexander E Gates Introduction Bedrock geology Shear zones & mineralized

PETROGRAFI BATUAN METAMORF

PETROGRAFI BATUAN METAMORF OLEH : AGUS HENDRATNO Laboratorium Geologi Optik Jurusan Teknik Geologi Fakultas Teknik Universitas Gadjah Mada Yogyakarta Quartz metamorf As deformation increases, the quartz

Report of Activities 2003 Published by: Manitoba Industry, Economic Development and Mines Manitoba Geological Survey, 2003.

Report of Activities 2003 Published by: Manitoba Industry, Economic Development and Mines Manitoba Geological Survey, 2003. ERRATA: The publisher/department name in the bibliographic reference cited immediately

MICROSTRUCTURAL STUDY ON NEOGENE ROCKS OF LOWER WEST KAMENG DISTRICT, ARUNACHAL PRADESH, INDIA

MICROSTRUCTURAL STUDY ON NEOGENE ROCKS OF LOWER WEST KAMENG DISTRICT, ARUNACHAL PRADESH, INDIA PANKAJ JYOTI DUTTA IIT Kharagpur, West Bengal (Email: pankajdutta86@gmail.com) Journal of Frontline Research

10 cm. 5 cm. 10 cm. glacial striae. glacial striae

GSA DATA REPOSITORY Druguet et al. Supplementary Photographs All photographs are vertical shots of sub-horizontal outcrops. All contacts are sub-vertical except for DR7 (dips indicated on picture). quartzitic

The movement history and fault rock evolution of a reactivated crustal-scale strike-slip fault: the Walls Boundary Fault Zone, Shetland

Journal of the Geological Society, London, Vol. 164, 2007, pp. 1037 1058. Printed in Great Britain. The movement history and fault rock evolution of a reactivated crustal-scale strike-slip fault: the Walls

GEOLOGY 435 FIELD EXERCISE 2, SPRING SKETCHING, DESCRIBING, AND MAPPING EXPOSURES OBJECTIVES:

OBJECTIVES: GEOLOGY 435 FIELD EXERCISE 2, SPRING 2016 -- SKETCHING, DESCRIBING, AND MAPPING EXPOSURES To develop and refine your field skills in: 1. observation and rock and sediment description 2. sketching

P Forsmark site investigation. Detailed fracture mapping of the outcrops Klubbudden, AFM and Drill Site 4, AFM001097

P-03-115 Forsmark site investigation Detailed fracture mapping of the outcrops Klubbudden, AFM001098 and Drill Site 4, AFM001097 Jan Hermanson, Lars Hansen, Jon Vestgård, Peter Leiner Golder Associates

CHAPTER 3.3: METAMORPHIC ROCKS

CHAPTER 3.3: METAMORPHIC ROCKS Introduction Metamorphism - the process of changes in texture and mineralogy of pre-existing rock due to changes in temperature and/or pressure. Metamorphic means change

Structure and history of the Kern Canyon fault system: introduction and thesis overview

1 Chapter 1 Structure and history of the Kern Canyon fault system: introduction and thesis overview Exposures of fault zones from the surface to deep levels afford an opportunity to study the transition

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.

Petrographic Data. Appendix C. Edward F. Stoddard

Appendix C Petrographic Data Edward F. Stoddard Standard size (27 46 mm) petrographic thin sections (30 m) of all rock and artifact samples were examined with a binocular Zeiss polarizing microscope using

Faults and Faulting. Processes in Structural Geology & Tectonics. Ben van der Pluijm. WW Norton+Authors, unless noted otherwise 2/2/ :47

Faults and Faulting Processes in Structural Geology & Tectonics Ben van der Pluijm WW Norton+Authors, unless noted otherwise 2/2/2017 14:47 We Discuss Faults Types and Geometries Systems Fault bends Dimensions

Chapter 7 Metamorphism, Metamorphic Rocks, and Hydrothermal Rocks

Chapter 7 Metamorphism, Metamorphic Rocks, and Hydrothermal Rocks Copyright The McGraw-Hill Companies, Inc. Permission required for reproduction or display. Metamorphism What happens to rocks that are

Deformation: Modification of Rocks by Folding and Fracturing

CHAPTER 7 Deformation: Modification of Rocks by Folding and Fracturing Chapter Summary A geologic map is a scientific model of rock formations that are exposed on the Earth s surface showing outcrops,

Thermomechanical evolution of the crust during convergence and deep crustal pluton emplacement in the Western Province of Fiordland, New Zealand

TECTONICS, VOL. 21, NO. 4, 10.1029/2001TC001282, 2002 Thermomechanical evolution of the crust during convergence and deep crustal pluton emplacement in the Western Province of Fiordland, New Zealand Nathan

Received 5 February 2003; received in revised form 30 July 2003; accepted 4 September 2003

Journal of Structural Geology 26 (2004) 793 805 www.elsevier.com/locate/jsg Development of shape- and lattice-preferred orientations of amphibole grains during initial cataclastic deformation and subsequent

LAB 1: ORIENTATION OF LINES AND PLANES

LAB 1: ORIENTATION OF LINES AND PLANES Read the introductory section, chapter 1, pages 1-3, of the manual by Rowland et al (2007) and make sure you understand the concepts of bearing, strike, dip, trend,

INSIGHTS INTO EARTHQUAKE RUPTURE AND RECOVERY FROM STUDIES OF PALEOSEISMIC FAULTS CHRISTIE ROWE, MCGILL UNIVERSITY

INSIGHTS INTO EARTHQUAKE RUPTURE AND RECOVERY FROM STUDIES OF PALEOSEISMIC FAULTS CHRISTIE ROWE, MCGILL UNIVERSITY DEFINITION OF AN EARTHQUAKE 1.Fast fault slip (~1 m/s) generates heat 2.Slip propagates

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

Preliminary Structural Study of the Gold-bearing Shear Zone System at the Seabee Mine, Northern Saskatchewan

Preliminary Structural Study of the Gold-bearing Shear Zone System at the Seabee Mine, Northern Saskatchewan Ghislain Tourigny Tourigny, G. (2003): Preliminary structural study of the gold-bearing shear

Figure 23-2 a. Highest strain in areas near grain contacts (hatch pattern). b. High-strain areas dissolve and material precipitates in adjacent

Textures Textures Reading: Winter, Chapter 23 Textures are small-scale scale penetrative features Relict Textures Inherited from original rock Blasto- = relict Any degree of preservation Pseudomorphs of

Suusamyr, Kyrgyzstan Structural-geological Report

Suusamyr, Kyrgyzstan Structural-geological Report by David Fossati fossatid@student.ethz.ch Contents 1 Introduction... 2 2 Field work area... 2 3 Field work methods... 5 4 Analysis methods... 7 5 Maps

Structural analysis of the Sopron Gneiss Formation (Sopron Mts., W-Hungary)

Structural analysis of the Sopron Gneiss Formation (Sopron Mts., W-Hungary) Zsolt BENKÓ a Éva BUGLEDITS a András RÉCSI a a Department of Physical Geography, University of West Hungary, Szombathely, Hungary

Cannat, M., Karson, J.A., Miller, D.J., et al., 1995 Proceedings of the Ocean Drilling Program, Initial Reports, Vol

Cannat, M., Karson, J.A., Miller, D.J., et al., 995 Proceedings of the Ocean Drilling Program, Initial Reports, Vol. 53 7. Shipboard Scientific Party 2 Date occupied: 4 January 994 Date departed: 6 January

Ductile Shear Zone ( 韌性剪切帶 ), Textures, and Transposition ( 移置作用 )

Ductile Shear Zone ( 韌性剪切帶 ), Textures, and Transposition ( 移置作用 ) Moine Thrust in Scotland http://www.uwsp.edu/geo/projects/geowe b/participants/dutch/vtrips/scot75may25-28.htm http://jaeger.earthsci.unimelb.edu.au/im

Sample photos and petrographic descriptions of core samples from the Norwegian continental margin basement

Sample photos and petrographic descriptions of core samples from the Norwegian continental margin basement Appendix 1 Petrophysical and thermal properties of pre-devonian basement rocks on the Norwegian

The geology of the Vermont Valley and the western flank of the Green Mountains between Dorset Mountain and Wallingford, Vermont

University at Albany, State University of New York Scholars Archive Geology Theses and Dissertations Atmospheric and Environmental Sciences 1992 The geology of the Vermont Valley and the western flank

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

Metamorphism occurs where equi P-T is disturbed

Metamorphism occurs where equi P-T is disturbed Steady-state geotherms are disturbed by a variety of processes including plate-tectonic transport of rocks and heat input by intrusion of magma active transport

Fig. Captions. Fig. 1. Generalized geologic map of eastern Nepal after Akiba et al. (1973), Carosi et al. (1993b),

41 Fig. Captions Fig. 1. Generalized geologic map of eastern Nepal after Akiba et al. (1973), Carosi et al. (1993b), Lombardo et al. (1993), and our field interpretations. The upper left inset shows the

Strain Localization on an Oceanic Detachment Fault System, Atlantis Massif, 30 Degrees N, Mid- Atlantic Ridge

University of Wyoming Wyoming Scholars Repository Geology and Faculty Publications Geology and 11-6-2004 Strain Localization on an Oceanic Detachment Fault System, Atlantis Massif, 30 Degrees N, Mid- Atlantic

Origin and mechanical significance of foliated cataclastic rocks in the cores of crustal-scale faults: Examples from the Median Tectonic Line, Japan

JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 111,, doi:10.1029/2005jb004205, 2006 Origin and mechanical significance of foliated cataclastic rocks in the cores of crustal-scale faults: Examples from the Median

Suzanne Picazo, Mathilde Cannat, Adelie Delacour, Javier Escartın, Stephane Roumejon, and Serguei Silantyev

Correction Volume 14, Number 8 16 August 2013 doi: ISSN: 1525-2027 Correction to Deformation associated with the denudation of mantle-derived rocks at the Mid- Atlantic Ridge 13 15 N: The role of magmatic

Introduction. Regional Geological Setting. Previous Work

Structural Geology of the Granite Lake Pit, Gibraltar Copper-Molybdenum Mine, South-Central British Columbia (NTS 093B/08, /09): Preliminary Observations N. Mostaghimi, University of British Columbia,

5/1/2017. Foliated Metamorphic Rocks. Classification of Metamorphic Rocks. Classification & Textures. Metamorphic Classification. Metamorphic Textures

Classification & Textures Metamorphic Classification Foliated Rocks Non-foliated Rocks Etc. Metamorphic Textures Relict textures Contact metamorphism Deformation & Recrystallization Dynamic/Regional metamorphism

Kinematic Investigation of Part of the Needle Falls Shear Zone 1

Kinematic Investigation of Part of the Needle Falls Shear Zone 1 M.R. Stautte? and J.F. Lewry 3 Stauffer, M.A. and Lewry, J.F. (1988): Kinematic investigation of part of the Needle Falls Shear Zone; in

material would flow extremely slowly similarly to a brittle material. The shear zone

GSA DATA REPOSITORY 21468 Hayman and Lavier Supplementary model description: Lavier et al. (213) showed that formation or reactivation of mixed mode fractures in ductile shear zones might generate variations

Accreted Terranes. Photos by Jim Cash Moscow High School

Accreted Terranes Photos by Jim Cash Moscow High School This unit contains photos from Hells Canyon, Rapid River, McCall to New Meadows, Kleinschmidt Grade, and Slate Creek Seven Devils Area: View of Seven

Geological sketch map of the Karkonosze granite and its metamorphic cover (after Aleksandrowski & Mazur, 2002). Study area - southern contact t zone

Brittle faulting in the southern contact zone of the Karkonosze granite near Karpacz Krzysztof Gaidzik, Jerzy Żaba Department of Fundamental Geology Faculty of Earth Sciences University of Silesia Aim

CHAPTER Va : CONTINUOUS HETEROGENEOUS DEFORMATION

Va-1 INTRODUCTION Heterogeneous deformation results from mechanical instabilities (folding and boudinage) within an heterogeneous material or from strain localization in an homogeneous material (shear

NMBGMR Geologic Map Symbols

NMBGMR Geologic Map Symbols LINES: Exposure Exposed Intermittent/Obscured Concealed Certain (or unspecified) Geologic contact, fault, or fold, exposed with high positional accuracy. Triangle shows location

Appendix 11. Geology. of the. I60 area

Appendix 11 Geology of the I60 area 1. Locality The locality of the I60 area is as follows; Northwestern corner; UTM_EW 530513, UTM_NS 7345741 Southwestern corner; UTM_EW 530418, UTM_NS 7301454 Northeastern

Igneous petrology EOSC 321

Igneous petrology EOSC 321 Laboratory 2: Determination of plagioclase composition. Mafic and intermediate plutonic rocks Learning Goals. After this Lab, you should be able: Determine plagioclase composition

lecture 8 Kristallingeologie This lecture Idioblastic porphyroblasts Porphyroblasts

Kristallingeologie lecture 8 Porphyroblasts This lecture Ductile deformation & metamorphic conditions New minerals grow: porphyroblasts with inclusions Inclusion trails can be used to define Pre-, syn-,

GG303 Lecture 29 9/4/01 1 FABRICS

GG303 Lecture 29 9/4/01 1 FABRICS I Main Topics A What are fabrics? B Planar fabrics C Linear fabrics D Penetrative vs. non-penetrative fabrics E Cleavage and folds F Comments on use of grain-scale observations

FIELD AND MICROSTRUCTURAL ANALYSIS OF A DIKE SWARM AND A DEFORMED COMPOSITE DIKE IN THE VINALHAVEN INTRUSIVE COMPLEX, MAINE

FIELD AND MICROSTRUCTURAL ANALYSIS OF A DIKE SWARM AND A DEFORMED COMPOSITE DIKE IN THE VINALHAVEN INTRUSIVE COMPLEX, MAINE OWEN MCKENNA Bowdoin College Sponsor: Rachel Beane INTRODUCTION The Vinalhaven

Structure and oxygen isotope analysis of Precambrian basement in the Cottonwood Creek Area, Black Mountain Quadrangle, Bighorn Mountains, Wyoming

Structure and oxygen isotope analysis of Precambrian basement in the Cottonwood Creek Area, Black Mountain Quadrangle, Bighorn Mountains, Wyoming Rashmi L. Becker Department of Forestry and Geology, The