Journal of Mechanics of Materials and Structures Vol 1 Issue 2, Feb 2006
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326-97 Lab Final S.D
Geol 326-97 Name: KEY 5/6/97 Class Ave = 101 / 150 Geol 326-97 Lab Final s.d. = 24 This lab final exam is worth 150 points of your total grade. Each lettered question is worth 15 points. Read through it all first to find out what you need to do. List all of your answers on these pages and attach any constructions, tracing paper overlays, etc. Put your name on all pages. 1. One way to analyze brittle faults is to calculate and plot the infinitesimal shortening and extension directions on a lower hemisphere, stereographic projection. These principal axes lie in the “movement plane”, which contains the pole to the fault plane and the slickensides, and are at 45° to the pole. The following questions apply to a single fault described in part (a), below: (a) A fault has a strike and dip of 250, 57 N and the slickensides have a rake of 63°, measured from the given strike azimuth. Plot the orientations of the fault plane and the slickensides on an equal area projection. (b) Bedding in the vicinity of the fault is oriented 37, 42 E. Assuming that the fault formed when the bedding was horizontal, determine and plot the original geometry of the fault and the slickensides. (c) Determine the original (pre-rotation)orientation of the infinitesimal shortening and extension axes for fault. 2. All of the following questions apply to the map shown on the next page. In all of the rocks with cleavage, you may assume that both cleavage and bedding strike 024°. -
Geologic Map of the Yellow Pine Quadrangle, Valley County, Idaho
IDAHO GEOLOGICAL SURVEY IDAHOGEOLOGY.ORG DIGITAL WEB MAP 190 MOSCOW AND BOISE STEWART AND OTHERS present in exposures in the southern part of the map. Quartzite is feldspar The Johnson Creek shear zone is a major regional structure (Lund, 2004). To PIONEER GROUP (CH0776) poor. Thickness unknown because of complex internal folding and the the south of the quadrangle it can be traced as a series of faults (Fisher and 19DS16 GEOLOGIC MAP OF THE YELLOW PINE QUADRANGLE, VALLEY COUNTY, IDAHO The Pioneer group is a prospected area located northeast of the mouth of presence of a foliation that may or may not be transposed bedding. Likely others, 1992; Stewart and others, 2018), none of which appear to be as equivalent to the quartzite and schist unit in the Stibnite roof pendant silicified as in the Yellow Pine area. One splay likely connects to the Dead- Riordan Creek. One Defense Minerals Administration (DMA) application Cambrian y CORRELATION OF MAP UNITS and one Defense Minerals Exploration Administration (DMEA) loan appli- t i mapped by Stewart and others (2016). wood fault, which is locally mineralized at and southwest of the Deadwood l i lower cation were made in the 1950s for claims in this area, details of which are b Mine (Kiilsgaard and others, 2006). To the north, north of the Red Mountain a b Zmsm Marble of Moores Station Formation (Neoproterozoic)—Discontinuous lenses available in Frank (2016). Prospects at slightly lower elevation were termed o qtzite David E. Stewart, Reed S. Lewis, Eric D. Stewart, and Zachery M. Lifton stockwork, the fault zone is intruded by voluminous Eocene dikes (Lund, r p of buff to light-gray marble and lesser amounts of millimeter- to the Syringa Group (DMA Docket 1036). -
Along Strike Variability of Thrust-Fault Vergence
Brigham Young University BYU ScholarsArchive Theses and Dissertations 2014-06-11 Along Strike Variability of Thrust-Fault Vergence Scott Royal Greenhalgh Brigham Young University - Provo Follow this and additional works at: https://scholarsarchive.byu.edu/etd Part of the Geology Commons BYU ScholarsArchive Citation Greenhalgh, Scott Royal, "Along Strike Variability of Thrust-Fault Vergence" (2014). Theses and Dissertations. 4095. https://scholarsarchive.byu.edu/etd/4095 This Thesis is brought to you for free and open access by BYU ScholarsArchive. It has been accepted for inclusion in Theses and Dissertations by an authorized administrator of BYU ScholarsArchive. For more information, please contact [email protected], [email protected]. Along Strike Variability of Thrust-Fault Vergence Scott R. Greenhalgh A thesis submitted to the faculty of Brigham Young University in partial fulfillment of the requirements for the degree of Master of Science John H. McBride, Chair Brooks B. Britt Bart J. Kowallis John M. Bartley Department of Geological Sciences Brigham Young University April 2014 Copyright © 2014 Scott R. Greenhalgh All Rights Reserved ABSTRACT Along Strike Variability of Thrust-Fault Vergence Scott R. Greenhalgh Department of Geological Sciences, BYU Master of Science The kinematic evolution and along-strike variation in contractional deformation in over- thrust belts are poorly understood, especially in three dimensions. The Sevier-age Cordilleran overthrust belt of southwestern Wyoming, with its abundance of subsurface data, provides an ideal laboratory to study how this deformation varies along the strike of the belt. We have per- formed a detailed structural interpretation of dual vergent thrusts based on a 3D seismic survey along the Wyoming salient of the Cordilleran overthrust belt (Big Piney-LaBarge field). -
Folds & Folding
Folds and Folding Earth Structure (2nd Edition), 2004 W.W. Norton & Co, New York Slide show by Ben van der Pluijm © WW Norton; unless noted otherwise Folds Maryland Appalachians Swiss Alps 9/18/2010 © EarthStructure (2nd ed) 2 Fold Classification fold shape in profile interlimb angle similar/parallel symmetry/vergence fold size amplitude wavelength fold facing upward/downward fold orientation axis/hinge line axial surface fold in 3D cylindrical/non-cylindrical presence of secondary features foliation lineation DePaor, 2002 9/18/2010 © EarthStructure (2nd ed) 3 Fold terminology 9/18/2010 © EarthStructure (2nd ed) 4 Fold facing (a) upward facing antiform or anticline (b) upward facing synform or syncline (c) downward-facing antiform or antiformal syncline (d) downward-facing synform or synformal anticline (e) profile view; (f) map view 9/18/2010 © EarthStructure (2nd ed) 5 Fold Shape parallel fold similar fold ptygmatic folds 9/18/2010 © EarthStructure (2nd ed) 6 Fold shape a. Parallel fold b. Similar fold t is layer-perpendicular thickness; T is axial trace-parallel thickness 9/18/2010 © EarthStructure (2nd ed) 7 Dip isogons In Class 1A (a) the construction of a single dip isogon is shown, which connects the tangents to upper and lower boundary of folded layer with equal angle (α) relative to a reference frame; dip isogons at 10° intervals are shown for each class. Class 1 folds (a– c) have convergent dip isogon patterns; dip isogons in Class 2 folds (d) are parallel; Class 3 folds (e) have divergent dip isogon patterns. In this classification, parallel (b) and similar (d) folds are labeled as Class 1B and Class 2, respectively. -
Anticline and Adjacent Areas Grand County, Utah
Please do not destroy or throw away this publication. If you have no further use for it write to the Geological Survey at Washington and ask for a frank to return it UNITED STATES DEPARTMENT OF THE INTERIOR Harold L. Ickes, Secretary GEOLOGICAL, SURVEY W. C. Mendenhall, Director Bulletin 863 GEOLOGY OF THE SALT VALLEY ANTICLINE AND ADJACENT AREAS GRAND COUNTY, UTAH BY C. H. DANE UNITED STATES GOVERNMENT PRINTING OFFICE WASHINGTON : 1935 For sale by the Superintendent of Documents, Washington, D. C. - - Price $1.00 (Paper cover) CONTENTS Abstract.____________________________________________________ 1 .Introduction____________________________________________ 2 Purpose and scope of the work_____________________________ 2 Field work.____________________________________________________ 4 Acknowledgments....-___--____-___-_--_-______.__________ 5 Topography, drainage, and water supply. ______ 5 Climate_._.__..-.-_--_-______- _ ____ 11 Vegetation. ____________________________ 14 Fuel.._____________________________________ 15 Population, accessibility, routes of travel___--______..________ 15 Previous publications......--.-.-.---.-...__---_-__-___._______ 17 Stratigraphy __ ____.____-__-_---_--____---______--___________.__ 18 Pre-Cambrian complex___---_-_-_-_-_-_-_--__ __--______ 20 Carboniferous system..______--__--_____-_-_-_-_-___-___.______ 24 Pennsylvanian (?) series.__________________________________ 24 Unnamed conglomerate--_______-._____________________ 24 Pennsylvanian series..--____-_-_-_-_-_-______--___.________ 25 Paradox formation.____-_-___---__-_____-__-__-__..__. -
Evolution of the Guerrero Composite Terrane Along the Mexican Margin, from Extensional Fringing Arc to Contractional Continental Arc
Evolution of the Guerrero composite terrane along the Mexican margin, from extensional fringing arc to contractional continental arc Elena Centeno-García1,†, Cathy Busby2, Michael Busby2, and George Gehrels3 1Instituto de Geología, Universidad Nacional Autónoma de México, Avenida Universidad 3000, Ciudad Universitaria, México D.F. 04510, México 2Department of Geological Sciences, University of California, Santa Barbara, California 93106-9630, USA 3Department of Geosciences, University of Arizona, Tucson, Arizona 85721, USA ABSTRACT semblage shows a Callovian–Tithonian (ca. accreted to the edge of the continent during 163–145 Ma) peak in magmatism; extensional contractional or oblique contractional phases The western margin of Mexico is ideally unroofing began in this time frame and con- of subduction. This process can contribute sub- suited for testing two opposing models for tinued into through the next. (3) The Early stantially to the growth of a continent (Collins, the growth of continents along convergent Cretaceous extensional arc assemblage has 2002; Busby, 2004; Centeno-García et al., 2008; margins: accretion of exotic island arcs by two magmatic peaks: one in the Barremian– Collins, 2009). In some cases, renewed upper- the consumption of entire ocean basins ver- Aptian (ca. 129–123 Ma), and the other in the plate extension or oblique extension rifts or sus accretion of fringing terranes produced Albian (ca. 109 Ma). In some localities, rapid slivers these terranes off the continental margin by protracted extensional processes in the subsidence produced thick, mainly shallow- once more, in a kind of “accordion” tectonics upper plate of a single subduction zone. We marine volcano-sedimentary sections, while along the continental margin, referred to by present geologic and detrital zircon evidence at other localities, extensional unroofing of Collins (2002) as tectonic switching. -
Thesis-Reproduction (Electronic)
A synopsis of the geologic and structural history of the Randsburg Mining District Item Type text; Thesis-Reproduction (electronic) Authors Morehouse, Jeffrey Allen, 1953-1985 Publisher The University of Arizona. Rights Copyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author. Download date 27/09/2021 08:53:56 Link to Item http://hdl.handle.net/10150/558085 Call No. BINDING INSTRUCTIONS INTERUBRARY INSTRUCTIONS Dept. E9791 Author: Morehouse, J. 1988 245 Title: RUSH___________________ PERMABIND____________ PAMPHLET._____________ GIFT____________________ COLOR: M,S* POCKET FOR MAP______ COVERS Front_______Both Special Instructions - Bindery or Repair REFERENCE____ i________ O th er--------------------------- 3 /2 /9 0 A SYNOPSIS OF THE GEOLOGIC AND STRUCTURAL HISTORY OF THE RANDSBURG MINING DISTRICT by Jeffrey Allen Morehouse A Thesis Submitted to the Faculty of the DEPARTMENT OF GEOSCIENCES In Partial Fulfillment of the Requirements For the Degree of MASTER OF SCIENCE In the Graduate College THE UNIVERSITY OF ARIZONA 19 8 8 THE UNIVERSITY OF ARIZONA TUCSON, ARIZONA 85721 DEPARTMENT OF GEOSCIENCES BUILDING *77 GOULD-SIMPSON BUILDING TEL (602) 621-6024 To the reader of Jeff Morehouse's thesis: Jeff Morehouse's life was lamentably cut short by a hiking-rock climbing accident in the Santa Catalina Mountains near Tucson, Arizona, on March 24, 1985. Those who knew Jeff will always regret that accident, not only because it abbreviated what would certainly have been an uncommonly productive geological career but also because it snuffed an effervescent, optimistic,, charming personality. -
Development of a Dilatant Damage Zone Along a Thrust Relay in a Low-Porosity Quartz Arenite
Journal of Structural Geology 28 (2006) 776–792 www.elsevier.com/locate/jsg Development of a dilatant damage zone along a thrust relay in a low-porosity quartz arenite Jennie E. Cook a, William M. Dunne a,*, Charles M. Onasch b a Department of Earth and Planetary Sciences, University of Tennessee, Knoxville, TN 37996-1410, USA b Department of Geology, Bowling Green State University, Bowling Green, OH 43403, USA Received 12 August 2005; received in revised form 26 January 2006; accepted 15 February 2006 Available online 18 April 2006 Abstract A damage zone along a backthrust fault system in well-cemented quartz arenite in the Alleghanian foreland thrust system consists of a network of NW-dipping thrusts that are linked by multiple higher-order faults and bound a zone of intense extensional fractures and breccias. The damage zone developed at an extensional step-over between two independent, laterally propagating backthrusts. The zone is unusual because it preserves porous brittle fabrics despite formation at O5 km depth. The presence of pervasive, late-stage fault-normal joints in a fault-bounded horse in the northwestern damage zone indicates formation between two near-frictionless faults. This decrease in frictional resistance was likely a result of increased fluid pressure. In addition to physical effects, chemical effects of fluid also influenced damage zone development. Quartz cements, fluid inclusion data, and Fourier Transform Infrared analysis indicate that both aqueous and methane-rich fluids were present within the damage zone at different times. The backthrust network likely acted as a fluid conduit system, bringing methane-rich fluids up from the underlying unit and displacing resident aqueous fluids. -
Thick-Skinned, South-Verging Backthrusting in the Felch and Calumet Troughs Area of the Penokean Orogen, Northern Michigan
Thick-Skinned, South-Verging Backthrusting in the Felch and Calumet Troughs Area of the Penokean Orogen, Northern Michigan U.S. GEOLOGICAL SURVEY BULLETIN 1904-L AVAILABILITY OF BOOKS AND MAPS OF THE U.S. GEOLOGICAL SURVEY Instructions or. ordering publications of the U.S. Geological Survey, along with the last offerings, are given in the current-year issues of the monthly catalog "New Publications of the U.S. Geological Survey." Prices of available U.S. Geological Survey publications released prior to the current year are listed in the most recent annual "Price and Availability List" Publications that are listed in various U.S. Geological Survey catalogs (see back inside cover) but not listed in the most recent annual "Price and Availability List" are no longer available. Prices of reports released to the open files are given in the listing "U.S. Geological Survey Open-File Reports," updated monthly, which is for sale in microfiche from the USGS ESIC-Open-File Report Sales, Box 25286, Building 810, Denver Federal Center, Denver, CO 80225 Order U.S. Geological Survey publications by mail or over the counter from the offices given below. BY MAIL OVER THE COUNTER Books Books Professional Papers, Bulletins, Water-Supply Papers, Tech Books of the U.S. Geological Survey are available over the niques of Water-Resources Investigations, Circulars, publications counter at the following U.S. Geological Survey offices, all of of general interest (such as leaflets, pamphlets, booklets), single which are authorized agents of the Superintendent of Documents. copies of periodicals (Earthquakes & Volcanoes, Preliminary De termination of Epicenters), and some miscellaneous reports, includ ANCHORAGE, Alaska-4230 University Dr., Rm. -
A N–S-Trending Active Extensional Structure, the Fiuhut (Afyon) Graben
Turkish Journal of Earth Sciences (Turkish J. Earth Sci.), Vol. 16, 2007, pp. 391–416. Copyright ©TÜB‹TAK A N–S-trending Active Extensional Structure, the fiuhut (Afyon) Graben: Commencement Age of the Extensional Neotectonic Period in the Isparta Angle, SW Turkey AL‹ KOÇY‹⁄‹T & fiULE DEVEC‹ Middle East Technical University, Department of Geological Engineering, Active Tectonics and Earthquake Research Laboratory, TR–06531 Ankara, Turkey (E-mail: [email protected]) Abstract: The fiuhut graben is an 8–11-km-wide, 24-km-long, N–S-trending, active extensional structure located on the southern shoulder of the Akflehir-Afyon graben, near the apex of the outer Isparta Angle. The fiuhut graben developed on a pre-Upper Pliocene rock assemblage comprising pre-Jurassic metamorphic rocks, Jurassic–Lower Cretaceous platform carbonates, the Lower Miocene–Middle Pliocene Afyon stratovolcanic complex and a fluvio- lacustrine volcano-sedimentary sequence. The eastern margin of the fiuhut graben is dominated by the Afyon volcanics and their well-bedded fluvio- lacustrine sedimentary cover, which is folded into a series of NNE-trending anticlines and synclines. This volcano- sedimentary sequence was deformed during a phase of WNW–ESE contraction, and is overlain with angular unconformity by nearly horizontal Plio–Quaternary graben infill. Palaeostress analyses of slip-plane data recorded in the lowest unit of the modern graben infill and on the marginal active faults indicate that the fiuhut graben has been developing as a result of ENE–WSW extension since the latest Pliocene. The extensional neotectonic period in the Isparta Angle started in the latest Pliocene. All margins of the fiuhut graben are determined and controlled by a series of oblique-slip normal fault sets and isolated fault segments. -
Parasitic Folds with Wrong Vergence: How Pre-Existing Geometrical Asymmetries Can Be Inherited During Multilayer Buckle Folding
Journal of Structural Geology 87 (2016) 19e29 Contents lists available at ScienceDirect Journal of Structural Geology journal homepage: www.elsevier.com/locate/jsg Parasitic folds with wrong vergence: How pre-existing geometrical asymmetries can be inherited during multilayer buckle folding * Marcel Frehner , Timothy Schmid Geological Institute, ETH Zurich, Switzerland article info abstract Article history: Parasitic folds are typical structures in geological multilayer folds; they are characterized by a small Received 20 October 2015 wavelength and are situated within folds with larger wavelength. Parasitic folds exhibit a characteristic Received in revised form asymmetry (or vergence) reflecting their structural relationship to the larger-scale fold. Here we 2 March 2016 investigate if a pre-existing geometrical asymmetry (e.g., from sedimentary structures or folds from a Accepted 5 April 2016 previous tectonic event) can be inherited during buckle folding to form parasitic folds with wrong Available online 9 April 2016 vergence. We conduct 2D finite-element simulations of multilayer folding using Newtonian materials. The applied model setup comprises a thin layer exhibiting the pre-existing geometrical asymmetry Keywords: Parasitic folds sandwiched between two thicker layers, all intercalated with a lower-viscosity matrix and subjected to Buckle folds layer-parallel shortening. When the two outer thick layers buckle and amplify, two processes work Fold vergence against the asymmetry: layer-perpendicular flattening between the two thick layers and the rotational Asymmetric folds component of flexural flow folding. Both processes promote de-amplification and unfolding of the pre- Structural inheritance existing asymmetry. We discuss how the efficiency of de-amplification is controlled by the larger-scale Finite-element method fold amplification and conclude that pre-existing asymmetries that are open and/or exhibit low amplitude are prone to de-amplification and may disappear during buckling of the multilayer system. -
Geodynamic Emplacement Setting of Late Jurassic Dikes of the Yana–Kolyma Gold Belt, NE Folded Framing of the Siberian Craton
minerals Article Geodynamic Emplacement Setting of Late Jurassic Dikes of the Yana–Kolyma Gold Belt, NE Folded Framing of the Siberian Craton: Geochemical, Petrologic, and U–Pb Zircon Data Valery Yu. Fridovsky 1,*, Kyunney Yu. Yakovleva 1, Antonina E. Vernikovskaya 1,2,3, Valery A. Vernikovsky 2,3 , Nikolay Yu. Matushkin 2,3 , Pavel I. Kadilnikov 2,3 and Nickolay V. Rodionov 1,4 1 Diamond and Precious Metal Geology Institute, Siberian Branch, Russian Academy of Sciences, 677000 Yakutsk, Russia; [email protected] (K.Y.Y.); [email protected] (A.E.V.); [email protected] (N.V.R.) 2 A.A. Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch, Russian Academy of Sciences, 630090 Novosibirsk, Russia; [email protected] (V.A.V.); [email protected] (N.Y.M.); [email protected] (P.I.K.) 3 Department of Geology and Geophysics, Novosibirsk State University, 630090 Novosibirsk, Russia 4 A.P. Karpinsky Russian Geological Research Institute, 199106 St. Petersburg, Russia * Correspondence: [email protected]; Tel.: +7-4112-33-58-72 Received: 30 September 2020; Accepted: 8 November 2020; Published: 11 November 2020 Abstract: We present the results of geostructural, mineralogic–petrographic, geochemical, and U–Pb geochronological investigations of mafic, intermediate, and felsic igneous rocks from dikes in the Yana–Kolyma gold belt of the Verkhoyansk–Kolyma folded area (northeastern Asia). The dikes of the Vyun deposit and the Shumniy occurrence intruding Mesozoic terrigenous rocks of the Kular–Nera and Polousniy–Debin terranes were examined in detail. The dikes had diverse mineralogical and petrographic compositions including trachybasalts, andesites, trachyandesites, dacites, and granodiorites.