The Role of Transverse Faults in Great Basin Extension: Transfer Faults Or N-S Extension?

Total Page:16

File Type:pdf, Size:1020Kb

The Role of Transverse Faults in Great Basin Extension: Transfer Faults Or N-S Extension? UNLV Retrospective Theses & Dissertations 1-1-2005 The role of transverse faults in Great Basin extension: Transfer faults or N-S extension? Tandis S Bidgoli University of Nevada, Las Vegas Follow this and additional works at: https://digitalscholarship.unlv.edu/rtds Repository Citation Bidgoli, Tandis S, "The role of transverse faults in Great Basin extension: Transfer faults or N-S extension?" (2005). UNLV Retrospective Theses & Dissertations. 1820. http://dx.doi.org/10.25669/5ag1-zwwy This Thesis is protected by copyright and/or related rights. It has been brought to you by Digital Scholarship@UNLV with permission from the rights-holder(s). You are free to use this Thesis in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you need to obtain permission from the rights-holder(s) directly, unless additional rights are indicated by a Creative Commons license in the record and/ or on the work itself. This Thesis has been accepted for inclusion in UNLV Retrospective Theses & Dissertations by an authorized administrator of Digital Scholarship@UNLV. For more information, please contact [email protected]. INFORMATION TO USERS This manuscript has been reproduced from the microfilm master. UMI films the text directly from the original or copy submitted. Thus, some thesis and dissertation copies are in typewriter face, while others may be from any type of computer printer. The quality of this reproduction is dependent upon the quality of the copy submitted. Broken or indistinct print, colored or poor quality illustrations and photographs, print bleedthrough, substandard margins, and improper alignment can adversely affect reproduction. In the unlikely event that the author did not send UMI a complete manuscript and there are missing pages, these will be noted. Also, if unauthorized copyright material had to be removed, a note will indicate the deletion. Oversize materials (e.g., maps, drawrings, charts) are reproduced by sectioning the original, beginning at the upper left-hand comer and continuing from left to right in equal sections with small overlaps. ProQuest Information and Learning 300 North Zeeb Road. Ann Arbor, Ml 48106-1346 USA 800-521-0000 UMI’ Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. THE ROLE OF TRANSVERSE FAULTS IN GREAT BASIN EXTENSION: TRANSFER FAULTS OR N-S EXTENSION? by Tandis S. Bidgoli Bachelor of Science San Francisco State University 2002 A thesis submitted in partial fulfillment of the requirements for Master of Science Degree in Geoscience Department of Geoscience College of Sciences Graduate College University of Nevada, Las Vegas August 2005 Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. UMI Number: 1429694 UMI Microform 1429694 Copyright 2006 by ProQuest Information and Learning Company. All rights reserved. This microform edition is protected against unauthorized copying under Title 17, United States Code. ProQuest Information and Learning Company 300 North Zeeb Road P.O. Box 1346 Ann Arbor, Ml 48105-1346 Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. Thesis Approval IJNTV The Graduate College University of Nevada, Las Vegas Jung—24- ,20_o§ The Thesis prepared by Tandis S. Bidgoli Entitled The Role of Transverse Faults in Great Basin Kytrensinn; TrangfpT Faults or N-S Extension? is approved in partial fulfillment of the requirements for the degree of Master of Science in Geoscience Examination Committee Chair Dean of the Graduate College . I Examination Committee Member Examination Committee Member Graduate College Facidty Representative 11 Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. ABSTRACT The Role of Transverse Faults in Great Basin Extension: Transfer Faults or N-S Extension? by Tandis S. Bidgoli Dr. Wanda J. Taylor, Examination Committee Chair Professor of Geology University of Nevada, Las Vegas New geologic map data (1:24,000 scale), geometric analyses, and kinematic analyses in the vicinity of the Crescent Spring fault zone (CSFZ), an E-W-striking fault zone in eastern Nevada, allow the recognition of four distinct extensional episodes. The episodes are pre-volcanic (pre-27 Ma), syn-volcanic (-27-18 Ma), Miocene (?) post-volcanic, and Miocene (?) - Pliocene or Quaternary post-volcanic extension. This extensional pattern, which is consistent with other fault studies along the broadly defined Timpahute lineament, has several important aspects. (I) Transverse faults of the CSFZ are normal faults that accommodated a distinct N-S extensional event. (2) The strain field within this part of the Great Basin reoriented at least twice during the Tertiary, from E-W extension to N-S extension and back to E-W extension. (3) The dominantly south- dipping, transverse normal faults moved crustal material southward, which may explain N-S shortening during large-magnitude E-W extension at the latitude of Las Vegas. (4) The eastern part of the Timpahute lineament is a regional transfer fault system that accommodated changes in the magnitude, timing, location, and direction of extension. Ill Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. TABLE OF CONTENTS ABSTRACT.................................................................................................................. ni LIST OF FIGURES....................................................................................................... vi ACKNOWLEDGEMENTS.......................................................................................... vii CHAPTER 1 INTRODUCTION................................................................................... 1 CHAPTER 2 REGIONAL GEOLOGY......................................................................... 6 Structural and Tectonic Background ......................................................................... 6 East-West-Trending Lineaments ............................................................................. 10 CHAPTERS STRATIGRAPHY................................................................................. 13 Paleozoic Stratigraphy ............................................................................................. 13 Sub-Tertiary Unconformity ..................................................................................... 14 Tertiary Stratigraphy ................................................................................................14 CHAPTER 4 METHODS............................................................................................16 CHAPTER 5 FAULT DESCRIPTIONS......................................................................18 -East-West-Striking Faults ...................................................................................... 18 -North-South-Striking Faults ..................................................................................21 CHAPTER 6 FOLD DESCRIPTIONS........................................................................ 24 CHAPTER 7 STRUCTURAL AND TECTONIC INTERPRETATIONS ................... 25 Mesozoic Contraction ..............................................................................................25 Prevolcanic Extension ..............................................................................................26 Synvolcanic Extension .............................................................................................30 Postvolcanic Miocene (?) Extension ........................................................................ 32 Postvolcanic Miocene (?) to Pliocene or Quaternary Extension ...............................35 CHAPTERS DISCUSSION........................................................................................37 Regional Transverse Zone .......................................................................................37 Implications of N-S Extension .................................................................................42 CHAPTER 9 SUMMARY AND CONCLUSIONS.....................................................51 IV Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. APPENDIX I METHODS................................................................................................... 83 APPENDIX II ANALYTICAL DATA.............................................................................. 89 REFERENCES....................................................................................................................... 98 VITA...................................................................................................................................... 110 Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. LIST OF FIGURES Figure 1 Tectonic Setting of Nevada..................................................................................54 Figure 2 Transverse Structure Models ............................................................................... 56 Figure 3 Location Map with Major Structural Elements .................................................. 57 Figure 4 Major Elements of a Collapsed Caldera ..............................................................59 Figure 5 Tectonomagmatic
Recommended publications
  • Progressive Deformation of a Zone of Magma Transfer in a Transpressional Regime: the Variscan Me´Rens Shear Zone (Pyrenees, France)
    Journal of Structural Geology 30 (2008) 1138–1149 Contents lists available at ScienceDirect Journal of Structural Geology journal homepage: www.elsevier.com/locate/jsg Progressive deformation of a zone of magma transfer in a transpressional regime: The Variscan Me´rens shear zone (Pyrenees, France) Yoann Dene`le, Philippe Olivier*,Ge´rard Gleizes LMTG, Universite´ de Toulouse, CNRS, IRD, OMP, 14 Avenue Edouard Belin, 31400 Toulouse, France article info abstract Article history: The EW-striking Variscan Me´rens shear zone (MSZ), located on the southern border of the Aston dome Received 19 November 2007 (Pyrenees), corresponds to variously mylonitized gneisses and plutonic rocks that are studied using the Received in revised form 30 April 2008 Anisotropy of Magnetic Susceptibility (AMS) technique. The plutonic rocks form EW-striking bands with, Accepted 15 May 2008 from south to north, gabbro-diorites, quartz diorites and granodiorites. The MSZ underwent a mylonitic Available online 28 May 2008 deformation with an intensity progressively increasing from the mafic to the more differentiated rocks. The foliations are EW to NW–SE striking and subvertical. A first set of lineations shows a moderate WNW plunge, with a dextral reverse kinematics. More recent subvertical lineations correspond to an uplift of Keywords: Mylonitic shear zone the northern compartment. To the east, the MSZ was cut by a N120 E-striking late shear band, separating Granite the MSZ from the Que´rigut pluton. The different stages of mylonitization relate to Late Variscan dextral AMS analysis transpression. This regime allowed the ascent of magmas along tension gashes in the middle crust. We Transpression interpret the MSZ as a zone of magma transfer, which fed a pluton now eroded that was similar to the Variscan Que´rigut and Millas plutons located to the east.
    [Show full text]
  • Subseismic Deformation in the Vaza-Barris Transfer Zone in the Cretaceous Recôncavo-Tucano-Jatobá Rift System, NE Brazil T
    Journal of Structural Geology 117 (2018) 81–95 Contents lists available at ScienceDirect Journal of Structural Geology journal homepage: www.elsevier.com/locate/jsg Subseismic deformation in the Vaza-Barris Transfer Zone in the Cretaceous Recôncavo-Tucano-Jatobá rift system, NE Brazil T ∗ Cleber Peralta Gomes Jr.a, Haakon Fossenb, , Renato Paes de Almeidaa, Bruno Salmonia a Instituto de Geociências, Universidade de São Paulo, Rua do Lago, 562, Cidade Universitária, CEP 05508-080, São Paulo, SP, Brazil b Museum of Natural History/Department of Earth Science, University of Bergen, Allégaten 41, N-5007, Bergen, Norway ARTICLE INFO ABSTRACT Keywords: We investigate the subseismic structural expression of the major Vaza-Barris Transfer Zone in the Early Subseismic structures Cretaceous Tucano rift basin, NE Brazil based on field observations. Subseismic structures in the Tucano rift fill Deformation bands encompass cataclastic deformation bands, deformation band clusters and deformation band faults. In general, Rift transfer zone these subseismic structures indicate a ∼120° extension direction and document oblique extension across the N-S Tucano basin Tucano Rift, consistent with the movement direction inferred from plate-scale reconstructions. The transfer zone itself is dominated by a large population of NE-SW trending deformation band structures that developed into deformation band faults making a high angle to the transfer zone. The deformation band faults are quite evenly distributed along the transfer zone, which we attribute to extension related to its arcuate cross-sectional shape with flanks dipping toward the rift margins. Additional subordinate structures, many of which are oriented parallel to the transfer zone, show strike-slip dominated motion, and indicate that the finite strain field in the transfer zone involves a component of NNW-SSE shortening in addition to the main extension along the transfer zone.
    [Show full text]
  • Foreland-Forearc Collisional Granitoid and Mafic Magmatism Caused By
    Foreland-forearc collisional granitoid and ma®c magmatism caused by lower-plate lithospheric slab breakoff: The Acadian of Maine, and other orogens A. Schoonmaker Department of Geology, University of Vermont, Burlington, Vermont 05405, USA W.S.F. Kidd Earth and Atmospheric Sciences, University at Albany, Albany, New York 12222, USA D.C. Bradley U.S. Geological Survey, 4200 University Drive, Anchorage, Alaska 99508, USA ABSTRACT canic belt. This model (Fig. 1) was elaborated on in Bradley et al. During collisional convergence, failure in extension of the lith- (1996), Robinson et al. (1998), Bradley and Tucker (2002), and Begeal osphere of the lower plate due to slab pull will reduce the thickness et al. (2004). Similarly, Sacks and Secor (1990) suggested lithospheric or completely remove lower-plate lithosphere and cause decom- necking to explain early granitic magmatism in the lower plate of the pression melting of the asthenospheric mantle; magmas from this southern Appalachian system during the Alleghenian orogeny. These source may subsequently provide enough heat for substantial par- models propose detachment of sections of the underthrust lower plate tial melting of crustal rocks under or beyond the toe of the colli- during the early orogenic stages of the subduction of a passive margin, sional accretionary system. In central Maine, United States, this rather than later, as proposed by Bird (1978) for the Himalaya, when type of magmatism is ®rst apparent in the Early Devonian West signi®cant lithospheric thickening and overthrusting has occurred. Branch Volcanics and equivalent ma®c volcanics, in the slightly younger voluminous ma®c/silicic magmatic event of the Moxie ACADIAN OF CENTRAL MAINEÐGEOLOGY OF THE Gabbro±Katahdin batholith and related ignimbrite volcanism, and CHESUNCOOK DOME in other Early Devonian granitic plutons.
    [Show full text]
  • Stratigraphy and Structure of the Seaman Range and Fox Mountain, Lincoln and Nye Counties, Nevada
    Stratigraphy and Structure of the Seaman Range and Fox Mountain, Lincoln and Nye Counties, Nevada U.S. GEOLOGICAL SURVEY BULLETIN 1988-B I 1 r^Hr-~"r-^S »:-«>'°-;>-.'; '£ '. -"* °-"^^io-'oO;ol!i-..e>L ^? :^~ty-":- o\: s--b>^.'d- .? " ? o..bTvo-r» ?:.-!:.»:-. "o'.-o'-o .- *^-o?.°:.--o : : ° o£\*>: ^-°:* '.« - "o-o- .-o - ^-.o.*'. ^» ' - 1 .". '. O- ' "" "- "* -" no: ^--'*^-o.yvo:»-c)^ - *>- : p.-by :o.;--p-/.-'o."-',c>-( 0 = ?.o'VO -V "±« -* «?'.<?o-oi ^ .. «- .*».-:»: -* ^^»-^ Chapter B Stratigraphy and Structure of the Seaman Range and Fox Mountain, Lincoln and Nye Counties, Nevada By DONLON O. HURTUBISE and EDWARD A. DU BRAY A multidisciplinary approach to research studies of sedimentary rocks and their constituents and the evolution of sedimentary basins, both ancient and modern U.S. GEOLOGICAL SURVEY BULLETIN 1988 EVOLUTION OF SEDIMENTARY BASINS EASTERN GREAT BASIN HARRY E. COOK AND CHRISTOPHER J. POTTER, Project Coordinators U.S. DEPARTMENT OF THE INTERIOR MANUEL LUJAN, JR., Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government UNITED STATES GOVERNMENT PRINTING OFFICE: 1992 For sale by Book and Open-File Report Sales U.S. Geological Survey Federal Center, Box 25286 Denver, CO 80225 Library of Congress Cataloging-in-Publication Data Hurtubise, D.O. Stratigraphy and structure of the Seaman Range and Fox Mountain, Lincoln and Nye Counties, Nevada / by Donlon O. Hurtubise and Edward A. du Bray, p. cm. (Evolution of sedimentary basins Eastern Great Basin ; ch. B) (U.S. Geological Survey bulletin ; 1988-B) Includes bibliographical references.
    [Show full text]
  • The Evolution of an Exposed Mid-Lower Crustal Attachment Zone in Fiordland, New Zealand
    The evolution of an exposed mid-lower crustal attachment zone in Fiordland, New Zealand Keith A. Klepeis1 and Geoffrey L. Clarke2 1Department of Geology, University of Vermont, Burlington, VT, 05405-0122, USA 2School of Geosciences, Division of Geology and Geophysics, University of Sydney, NSW 2006, Australia Abstract. Studies of convergent margins suggest that large subhorizontal shear zones in the lower crust help regulate how displacements are transferred horizontally and vertically through the lithosphere. We present structural data from the Fiordland belt of southwest New Zealand that illustrate the progressive evolution of a 25 km thick section of exhumed, Early Cretaceous middle and lower crust. The data show that the mechanisms by which displacements were relayed through the crust during a 25 Ma cycle of arc-related magmatism, high-grade metamorphism and contraction changed repeatedly. During the period 126-116 Ma, a ≥10 km batholith composed of gabbroic-dioritic magma was emplaced into the lower crust. Melt-enhanced shear zones evolved at the upper and lower contacts of the batholith where magma and steep temperature gradients created strength contrasts. By ~120 Ma, partial melting of mafic-intermediate lower crust resulted in the formation of high-pressure (14-16 kbar) migmatite and steep, regionally extensive vein networks up to 10 km below the batholith. Melt segregation and transfer through and out of the lower crust was aided by melt-induced fracture arrays and in ductile deformation in shear zones. During the period 116-108 Ma, differential shortening of the crust produced a network of subhorizontal and subvertical shear zones at different crustal depths.
    [Show full text]
  • Structure and Devonian Stratigraphy of the Timpahute Range, Nevada
    STRUCTURE AND DEVONIAN STRATIGRAPHY OF THE TIMPAHUTE RANGE, NEVADA Volume I by Alan K. Chamberlain © Copyright, 1999 A thesis submitted to the Faculty and Board of Trustees of the Colorado School of Mines in partial fulfillment of the requirements for the degree of Doctor of Philosophy (Geology). Golden, Colorado Date____________ Signed:__________________________ Alan K. Chamberlain Approved:__________________________ Dr. John E. Warme Professor and Thesis Advisor Golden, Colorado Date____________ ____________________________________ Dr. Roger Slatt, Professor and Head, Department of Geology and Geological Engineering ii ABSTRACT Sequences of Devonian rocks are advantageously exposed along a unique 40- mile-long east-west traverse in the greater Timpahute Range, southeastern Nevada. Study of these rocks casts light upon Devonian paleogeography, the Devonian Antler orogeny, an Upper Devonian cosmolite impact basin, this part of the Cretaceous Sevier fold-and- thrust belt, and the effects of Cenozoic extension. The greater Timpahute Range lies within the Timpahute Range 30' X 60' quadrangle and includes the region from Tempiute Mountain on the west to the Pahroc Range on the east. Concealed major north-south trending normal faults caused by Cenozoic extension have been proposed to disrupt the Paleozoic rocks of the region. However, a structural interpretation using a new geologic map of the quadrangle requires no major north-south striking normal faults. Furthermore, the greater Timpahute Range is interpreted as a salient of stacked thrust sheets within the Sevier fold-and-thrust belt. The range is bounded on the north and south by thrust tear faults that may be related to basement fractures caused by the cosmolite impact. Evidence for the Late Devonian cosmolite impact includes shocked quartz, iridium anomalies, ejecta spherules, and disturbed shallowing-upward sequences exhibiting intrasequence folding, brecciation, carbonate liquefaction, and graded bedding.
    [Show full text]
  • University of Nevada Reno Analysis of the White River Groundwater Flow System Using a Deuterium-Calibrated Discrete-State Compar
    MINIS lilR A ftt University of Nevada Reno Analysis of the White River Groundwater Flow System Using a Deuterium-Calibrated Discrete-State Compartment Model A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Hydrology and Hydrogeology Mines Library University of Nevada - Reno Reno, Nevada 89557-0044 by Stephen T. Kirk i' * July 1987 II WINtS UMARY " i i t S ' S The thesis of Stephen Thomas Kirk is approved: \AAjiC&OjJ C. Cr Thesis Advisor " University of Nevada Reno July 1987 ACNOWLED GEMENTS The author gratefully acknowledges the advice and guidance of Dr. Michael Cam- pana throughout this project. Additional advice was provided by Dr. W. Miller and Dr. D. Tibbitts. Special thanks go to Marcia Olson Kirk for her advice, en­ couragement, and patience. Financial support for this project was provided by the State of Nevada’s Carbonate Aquifers Studies Program and Desert Research Institute, Water Resources Center. IV ABSTRACT The White River Flow System (WRFS), a regional carbonate flow system in eastern Nevada, can be delineated with a discrete-state compartment model using environmental isotope (deuterium) data. Calibrated model results yield the following differences with an earlier conceptual model of WRFS: 1) minimum underflow out of the system along the Pahranagat Shear Zone is 4,000 acre feet per year; 2) minimum recharge from the Sheep Range to Coyote Springs Valley is 5,000 acre feet per year; and 3) minimum underflow from Meadow Valley Wash to Upper Moapa Valley is 4,500 acre feet per year. Calibration of the model using a paleoclimatically induced shift in re­ charge amounts (+35%) and deuterium concentrations (-8<5D) during the Pleistocene support these results.
    [Show full text]
  • Structural Evolution and Regional Implications of the Arrowhead Mine Fault Within the Pahranagat Shear Zone, Nevada, USA Michael Dennis Evans [email protected]
    UNLV Theses, Dissertations, Professional Papers, and Capstones 5-15-2018 Structural Evolution and Regional Implications of the Arrowhead Mine Fault within the Pahranagat Shear Zone, Nevada, USA Michael Dennis Evans [email protected] Follow this and additional works at: https://digitalscholarship.unlv.edu/thesesdissertations Part of the Geology Commons Repository Citation Evans, Michael Dennis, "Structural Evolution and Regional Implications of the Arrowhead Mine Fault within the Pahranagat Shear Zone, Nevada, USA" (2018). UNLV Theses, Dissertations, Professional Papers, and Capstones. 3248. https://digitalscholarship.unlv.edu/thesesdissertations/3248 This Thesis is brought to you for free and open access by Digital Scholarship@UNLV. It has been accepted for inclusion in UNLV Theses, Dissertations, Professional Papers, and Capstones by an authorized administrator of Digital Scholarship@UNLV. For more information, please contact [email protected]. STRUCTURAL EVOLUTION AND REGIONAL IMPLICATIONS OF THE ARROWHEAD MINE FAULT WITHIN THE PAHRANAGAT SHEAR ZONE, NEVADA, USA By Michael Dennis Evans Bachelor of Science – Geology California Lutheran University 2013 A thesis submitted in partial fulfilment of the requirements for the Master of Science – Geoscience Department of Geoscience College of Sciences The Graduate College University of Nevada, Las Vegas May 2018 --------------------------------------------------------------- Copyright by Michael Evans, 2018 All Rights Reserved -------------------------------------------------------------- Thesis Approval The Graduate College The University of Nevada, Las Vegas May 10, 2018 This thesis prepared by Michael Dennis Evans entitled Structural Evolution and Regional Implications of the Arrowhead Mine Fault within the Pahranagat Shear Zone, Nevada, Usa is approved in partial fulfillment of the requirements for the degree of Master of Science – Geoscience Department of Geoscience Wanda Taylor, Ph.D.
    [Show full text]
  • The Dongying Anticline, Bohai Bay Basin, Eastern China
    Open Geosci. 2016; 8:612–629 Research Article Open Access Fei Tian*, Jianting Yang, Ming Cheng, Yuhong Lei, Likuan Zhang, Xiaoxue Wang, and Xin Liu Geometry, kinematics and dynamic characteristics of a compound transfer zone: the Dongying anticline, Bohai Bay Basin, eastern China DOI 10.1515/geo-2016-0053 riods of Neogene Guantao and Minghuazhen Formations, Received Feb 14, 2016; accepted Jul 18, 2016 and migrated along major faults from source kitchens to reservoirs. The secondary faults acted as barriers, result- Abstract: The Dongying anticline is an E-W striking com- ing in the formation of fault-bound compartments. The plex fault-bounded block unit which located in the central high points of the anticline and well-sealed traps near sec- Dongying Depression, Bohai Bay Basin. The anticline cov- ondary faults are potential targets. This paper provides a ers an area of approximately 12 km2. The overlying succes- reservoir formation model of the low-order transfer zone sion, which is mainly composed of Tertiary strata, is cut by and can be applied to the hydrocarbon exploration in normal faults with opposing dips. In terms of the general transfer zones, especially the complex fault block oilfields structure, the study area is located in a compound transfer in eastern China. zone with major bounding faults to the west (Ying 1 fault) and east (Ying -8 and -31 faults). Using three-dimensional Keywords: transfer zone; fault kinematics; stress proper- seismic data, wireline log and checkshot data, the geome- ties; petroleum migration; Dongying Depression; Bohai tries and kinematics of faults in the transfer zone were Bay Basin; China studied, and fault displacements were calculated.
    [Show full text]
  • New Insights on the Structural Geology of the Pacquet Harbour Group and Point Rousse Complex, Baie Verte Peninsula, Newfoundland
    Current Research (2009) Newfoundland and Labrador Department of Natural Resources Geological Survey, Report 09-1, pages 147-158 NEW INSIGHTS ON THE STRUCTURAL GEOLOGY OF THE PACQUET HARBOUR GROUP AND POINT ROUSSE COMPLEX, BAIE VERTE PENINSULA, NEWFOUNDLAND S. Castonguay1, T. Skulski2, C. van Staal3 and M. Currie2 1 Geological Survey of Canada, 490 rue de la Couronne, Québec, QC, G1K 9A9 2 Geological Survey of Canada, 601 Booth Street, Ottawa, ON, K1A 0E8 3 Geological Survey of Canada, 625 Robson Street, Vancouver, BC, V6B 5J3 ABSTRACT The Baie Verte Peninsula represents one of the classical areas to study the structural evolution of peri-Laurentian ophi- olite and arc complexes, before and following, their tectonic juxtaposition to the early Paleozoic Laurentian margin. Region- al structural data are presented that focus on the ophiolitic and cover rocks of the Pacquet Harbour Group (PHG) and Point Rousse complex (PRC) that have been affected by, at least, four phases of regional deformation. The D1 fabrics are poorly preserved and strongly overprinted in the ophiolitic rocks, but are locally preserved in the Fleur de Lys Supergroup (Humber Zone). The D1 phase is interpreted to be related to the obduction of ophiolites during the Ordovician Taconian Orogeny; D2 represents the main tectonometamorphic phase. In the PRC, D2 fabrics are mostly parallel to, and associated with, the west- trending south-directed reverse faults. Southward, these culminate with the Scrape fault, a ductile shear zone that juxtaposes serpentinized mantle of the PRC over amphibolitic gabbros and basalts of the PHG. The Scrape fault and D2 south-directed shear zones separating the PRC from the PHG are affected by penecontemporaneous transverse high-strain zones (D2b) inter- preted as lateral ramps.
    [Show full text]
  • Rifting, Seafloor Spreading, and Extensional Tectonics
    2917-CH16.pdf 11/20/03 5:21 PM Page 382 CHAPTER SIXTEEN Rifting, Seafloor Spreading, and Extensional Tectonics 16.1 Introduction 382 16.6.2 Igneous-Rock Assemblage of Rifts 397 16.2 Cross-Sectional Structure of a Rift 385 16.6.3 Active Rift Topography 16.2.1 Normal Fault Systems 385 and Rift-Margin Uplifts 399 16.2.2 Pure-Shear versus Simple-Shear 16.7 Tectonics of Midocean Ridges 402 Models of Rifting 389 16.8 Passive Margins 405 16.2.3 Examples of Rift Structure 16.9 Causes of Rifting 408 in Cross Section 389 16.10 Closing Remarks 410 16.3 Cordilleran Metamorphic Core Complexes 390 Additional Reading 410 16.4 Formation of a Rift System 394 16.5 Controls on Rift Orientation 396 16.6 Rocks and Topographic Features of Rifts 397 16.6.1 Sedimentary-Rock Assemblages in Rifts 397 16.1 INTRODUCTION phere undergoes regional horizontal extension. A rift or rift system is a belt of continental lithosphere that Eastern Africa, when viewed from space, looks like it is currently undergoing extension, or underwent exten- has been slashed by a knife, for numerous ridges, sion in the past. During rifting, the lithosphere bounding deep, gash-like troughs, traverse the land- stretches with a component roughly perpendicular to scape from north to south (Figure 16.1a and b). This the trend of the rift; in an oblique rift, the stretching landscape comprises the East African Rift, a region direction is at an acute angle to the rift trend. where the continent of Africa is quite literally splitting Geologists distinguish between active and inactive apart—land lying on the east side of the rift moves rifts, based on the timing of the extension.
    [Show full text]
  • Extension Parallel to the Rift Zone During Segmented Fault Growth: Application to the Evolution of the NE Atlantic
    Solid Earth, 8, 1161–1180, 2017 https://doi.org/10.5194/se-8-1161-2017 © Author(s) 2017. This work is distributed under the Creative Commons Attribution 4.0 License. Extension parallel to the rift zone during segmented fault growth: application to the evolution of the NE Atlantic Alodie Bubeck1, Richard J. Walker1, Jonathan Imber2, Robert E. Holdsworth2, Christopher J. MacLeod3, and David A. Holwell1 1Department of Geology, University of Leicester, Leicester, LE1 7RH, UK 2Department of Earth Sciences, Durham University, Durham, DH1 3LE, UK 3Department of Earth and Ocean Sciences, Cardiff University, Cardiff, CF10 3AT, UK Correspondence to: Alodie Bubeck ([email protected]) Received: 21 August 2017 – Discussion started: 24 August 2017 Revised: 15 October 2017 – Accepted: 17 October 2017 – Published: 22 November 2017 Abstract. The mechanical interaction of propagating normal 1 Introduction faults is known to influence the linkage geometry of first- order faults, and the development of second-order faults and The primary regional-scale segmentation of extensional ter- fractures, which transfer displacement within relay zones. ranes is controlled by the development of networks of normal Here we use natural examples of growth faults from two ac- fault systems and the partitioning of strain across them. Nor- tive volcanic rift zones (Koa‘e, island of Hawai‘i, and Krafla, mal faults comprise multiple discontinuous, non-collinear northern Iceland) to illustrate the importance of horizontal- segments, with overlaps and segment linkage forming char- plane extension (heave) gradients, and associated vertical acteristic stepping geometries on a broad range of scales (e.g. axis rotations, in evolving continental rift systems.
    [Show full text]