Stress and Fluid Control on De Collement Within Competent Limestone
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Significance of Brittle Deformation in the Footwall
Journal of Structural Geology 64 (2014) 79e98 Contents lists available at SciVerse ScienceDirect Journal of Structural Geology journal homepage: www.elsevier.com/locate/jsg Significance of brittle deformation in the footwall of the Alpine Fault, New Zealand: Smithy Creek Fault zone J.-E. Lund Snee a,*,1, V.G. Toy a, K. Gessner b a Geology Department, University of Otago, PO Box 56, Dunedin 9016, New Zealand b Western Australian Geothermal Centre of Excellence, The University of Western Australia, 35 Stirling Highway, Crawley, WA 6009, Australia article info abstract Article history: The Smithy Creek Fault represents a rare exposure of a brittle fault zone within Australian Plate rocks that Received 28 January 2013 constitute the footwall of the Alpine Fault zone in Westland, New Zealand. Outcrop mapping and Received in revised form paleostress analysis of the Smithy Creek Fault were conducted to characterize deformation and miner- 22 May 2013 alization in the footwall of the nearby Alpine Fault, and the timing of these processes relative to the Accepted 4 June 2013 modern tectonic regime. While unfavorably oriented, the dextral oblique Smithy Creek thrust has Available online 18 June 2013 kinematics compatible with slip in the current stress regime and offsets a basement unconformity beneath Holocene glaciofluvial sediments. A greater than 100 m wide damage zone and more than 8 m Keywords: Fault zone wide, extensively fractured fault core are consistent with total displacement on the kilometer scale. e Fluid flow Based on our observations we propose that an asymmetric damage zone containing quartz carbonate Hydrofracture echloriteeepidote veins is focused in the footwall. -
GEO 2008 Conference Abstracts, Bahrain GEO 2008 Conference Abstracts
GEO 2008 conference abstracts, Bahrain GEO 2008 Conference Abstracts he abstracts of the GEO 2008 Conference presentations (3-5 March 2008, Bahrain) are published in Talphabetical order based on the last name of the first author. Only those abstracts that were accepted by the GEO 2008 Program Committee are published here, and were subsequently edited by GeoArabia Editors and proof-read by the corresponding author. Several names of companies and institutions to which presenters are affiliated have been abbreviated (see page 262). For convenience, all subsidiary companies are listed as the parent company. (#117804) Sandstone-body geometry, facies existing data sets and improve exploration decision architecture and depositional model of making. The results of a recent 3-D seismic reprocessing Ordovician Barik Sandstone, Oman effort over approximately 1,800 square km of data from the Mediterranean Sea has brought renewed interest in Iftikhar A. Abbasi (Sultan Qaboos University, Oman) deep, pre-Messinian structures. Historically, the reservoir and Abdulrahman Al-Harthy (Sultan Qaboos targets in the southern Mediterranean Sea have been the University, Oman <[email protected]>) Pliocene-Pleistocene and Messinian/Pre-Messinian gas sands. These are readily identifiable as anomalousbright The Lower Paleozoic siliciclastics sediments of the amplitudes on the seismic data. The key to enhancing the Haima Supergroup in the Al-Haushi-Huqf area of cen- deeper structure is multiple and noise attenuation. The tral Oman are subdivided into a number of formations Miocene and older targets are overlain by a Messinian- and members based on lithological characteristics of aged, structurally complex anhydrite layer, the Rosetta various rock sequences. -
Deformation Mechanisms, Rheology and Tectonics Geological Society Special Publications Series Editor J
Deformation Mechanisms, Rheology and Tectonics Geological Society Special Publications Series Editor J. BROOKS J/iLl THIS VOLUME IS DEDICATED TO THE WORK OF HENDRIK JAN ZWART GEOLOGICAL SOCIETY SPECIAL PUBLICATION NO. 54 Deformation Mechanisms, Rheology and Tectonics EDITED BY R. J. KNIPE Department of Earth Sciences Leeds University UK & E. H. RUTTER Department of Geology Manchester University UK ASSISTED BY S. M. AGAR R. D. LAW Department of Earth Sciences Department of Geological Sciences Leeds University Virginia University UK USA D. J. PRIOR R. L. M. VISSERS Department of Earth Sciences Institute of Earth Sciences Liverpool University University of Utrceht UK Netherlands 1990 Published by The Geological Society London THE GEOLOGICAL SOCIETY The Geological Society of London was founded in 1807 for the purposes of 'investigating the mineral structures of the earth'. It received its Royal Charter in 1825. The Society promotes all aspects of geological science by means of meetings, speeiat lectures and courses, discussions, specialist groups, publications and library services. It is expected that candidates for Fellowship will be graduates in geology or another earth science, or have equivalent qualifications or experience. Alt Fellows are entitled to receive for their subscription one of the Society's three journals: The Quarterly Journal of Engineering Geology, the Journal of the Geological Society or Marine and Petroleum Geology. On payment of an additional sum on the annual subscription, members may obtain copies of another journal. Membership of the specialist groups is open to all Fellows without additional charge. Enquiries concerning Fellowship of the Society and membership of the specialist groups should be directed to the Executive Secretary, The Geological Society, Burlington House, Piccadilly, London W1V 0JU. -
Lithology and Internal Structure of the San Andreas Fault at Depth Based
1 1 Lithology and Internal Structure of the San Andreas Fault at depth based on 2 characterization of Phase 3 whole-rock core in the San Andreas Fault Observatory at 3 Depth (SAFOD) Borehole 4 By Kelly K. Bradbury1, James P. Evans1, Judith S. Chester2, Frederick M. Chester2, and David L. Kirschner3 5 1Geology Department, Utah State University, Logan, UT 84321-4505 6 2Center for Tectonophysics and Department of Geology and Geophysics, Texas A&M University, College Station, 7 Texas 77843 8 3Department of Earth and Atmospheric Sciences, St. Louis University, St. Louis, Missouri 63108 9 10 Abstract 11 We characterize the lithology and structure of the spot core obtained in 2007 during 12 Phase 3 drilling of the San Andreas Fault Observatory at Depth (SAFOD) in order to determine 13 the composition, structure, and deformation processes of the fault zone at 3 km depth where 14 creep and microseismicity occur. A total of approximately 41 m of spot core was taken from 15 three separate sections of the borehole; the core samples consist of fractured arkosic sandstones 16 and shale west of the SAF zone (Pacific Plate) and sheared fine-grained sedimentary rocks, 17 ultrafine black fault-related rocks, and phyllosilicate-rich fault gouge within the fault zone 18 (North American Plate). The fault zone at SAFOD consists of a broad zone of variably damaged 19 rock containing localized zones of highly concentrated shear that often juxtapose distinct 20 protoliths. Two zones of serpentinite-bearing clay gouge, each meters-thick, occur at the two 21 locations of aseismic creep identified in the borehole on the basis of casing deformation. -
24. Anelastic Strain Recovery and Elastic Properties of Oceanic Basaltic Rocks1
Gradstein, F. M., Ludden, J. N., et al., 1992 Proceedings of the Ocean Drilling Program, Scientific Results, Vol. 123 24. ANELASTIC STRAIN RECOVERY AND ELASTIC PROPERTIES OF OCEANIC BASALTIC ROCKS1 N. R. Brereton,2 P. N. Chroston,3 C. J. Evans,2 J. A. Hudson,4 and R. B. Whitmarsh5 ABSTRACT A knowledge of rock stress is fundamental for improving our understanding of oceanic crustal mechanisms and lithospheric dynamic processes. However, direct measurements of stress in the deep oceans, and in particular stress magnitudes, have proved to be technically difficult. Anelastic strain recovery measurements were conducted on 15 basalt core samples from Sites 765 and 766 during Leg 123. Three sets of experiments were performed: anelastic strain recovery monitoring, dynamic elastic property measure- ments, and thermal azimuthal anisotropy observations. In addition, a range of other tests and observations were recorded to characterize each of the samples. One common feature of the experimental results and observations is that apparently no consistent orientation trend exists, either between the different measurements on each core sample or between the same sets of measurements on the various core samples. However, some evidence of correspondence between velocity anisotropy and anelastic strain recovery exists, but this is not consistent for all the core samples investigated. Thermal azimuthal anisotropy observations, although showing no conclusive correlations with the other results, were of significant interest in that they clearly exhibited anisotropic behavior. The apparent reproducibility of this behavior may point toward the possibility of rocks that retain a "memory" of their stress history, which could be exploited to derive stress orientations from archived core. -
Tectono-Metamorphic Evolution of the Northern Menderes Massif: Evidence from the Horst Between Gördes and Demirci Basins (West Anatolia, Turkey)
TECTONO-METAMORPHIC EVOLUTION OF THE NORTHERN MENDERES MASSIF: EVIDENCE FROM THE HORST BETWEEN GÖRDES AND DEMİRCİ BASINS (WEST ANATOLIA, TURKEY) A THESIS SUBMITTED TO THE GRADUATE SCHOOL OF NATURAL AND APPLIED SCIENCES OF MIDDLE EAST TECHNICAL UNIVERSITY BY ÇAĞRI BUĞDAYCIOĞLU IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE IN GEOLOGICAL ENGINEERING SEPTEMBER 2004 Approval of the Graduate School of Natural and Applied Sciences. I certify that this thesis satisfies all the requirements as a thesis for the degree of Master of Science. This is to certify that we have read this thesis and that in our opinion it is fully adequate, in scope and quality, as a thesis for the degree of Master of Science. Examining Committee Members Prof.Dr. Vedat Toprak (METU, GEOE) ___________________ Prof.Dr. Erdin Bozkurt (METU, GEOE) ___________________ Assoc.Prof.Dr. Bora Rojay (METU, GEOE) ___________________ Assoc.Prof.Dr. Kadir Dirik (HU, GEOE) ___________________ Assist.Prof.Dr. İsmail Ömer Yılmaz (METU, GEOE) ___________________ ii I hereby declare that all information in this document has been obtained and presented in accordance with academic rules and ethical conduct. I also declare that, as required by these rules and conduct, I have fully cited and referenced all material and results that are not original to this work. Name, Last name : Çağrı Buğdaycıoğlu Signature : iii ABSTRACT TECTONO-METAMORPHIC EVOLUTION OF THE NORTHERN MENDERES MASSIF: EVIDENCE FROM THE HORST BETWEEN GÖRDES AND DEMİRCİ BASINS (WEST ANATOLIA, TURKEY) Buğdaycıoğlu, Çağrı M.Sc., Department of Geological Engineering Supervisor : Prof.Dr. Erdin Bozkurt September 2004, 163 pages The Menderes Massif forms a large metamorphic culmination in western Turkey – an extensional province where continental lithosphere has been stretching following Palaeogene crustal thickening. -
Mechanical Stratigraphic Controls on Natural Fracture Spacing and Penetration
Journal of Structural Geology 95 (2017) 160e170 Contents lists available at ScienceDirect Journal of Structural Geology journal homepage: www.elsevier.com/locate/jsg Mechanical stratigraphic controls on natural fracture spacing and penetration * Ronald N. McGinnis a, , David A. Ferrill a, Alan P. Morris a, Kevin J. Smart a, Daniel Lehrmann b a Department of Earth, Material, and Planetary Sciences, Southwest Research Institute, 6220 Culebra Road, San Antonio, TX 78238-5166, USA b Geoscience Department, Trinity University, One Trinity Place, San Antonio, TX 78212, USA article info abstract Article history: Fine-grained low permeability sedimentary rocks, such as shale and mudrock, have drawn attention as Received 20 July 2016 unconventional hydrocarbon reservoirs. Fracturing e both natural and induced e is extremely important Received in revised form for increasing permeability in otherwise low-permeability rock. We analyze natural extension fracture 21 December 2016 networks within a complete measured outcrop section of the Ernst Member of the Boquillas Formation Accepted 7 January 2017 in Big Bend National Park, west Texas. Results of bed-center, dip-parallel scanline surveys demonstrate Available online 8 January 2017 nearly identical fracture strikes and slight variation in dip between mudrock, chalk, and limestone beds. Fracture spacing tends to increase proportional to bed thickness in limestone and chalk beds; however, Keywords: Mechanical stratigraphy dramatic differences in fracture spacing are observed in mudrock. A direct relationship is observed be- Natural fractures tween fracture spacing/thickness ratio and rock competence. Vertical fracture penetrations measured Fracture spacing from the middle of chalk and limestone beds generally extend to and often beyond bed boundaries into Fracture penetration the vertically adjacent mudrock beds. -
The Role of Pressure Solution Seam and Joint Assemblages In
THE ROLE OF PRESSURE SOLUTION SEAM AND JOINT ASSEMBLAGES IN THE FORMATION OF STRIKE-SLIP AND THRUST FAULTS IN A COMPRESSIVE TECTONIC SETTING; THE VARISCAN OF SOUTHWESTERN IRELAND Filippo Nenna and Atilla Aydin Department of Geological and Environmental Sciences, Stanford University, Stanford, CA 94305 e-mail: [email protected] scale such as strike-slip faults and thrust-cored folds in Abstract various stages of their development. In this study we focus on the initiation and development of strike-slip The Ross Sandstone in County Clare, Ireland, was faults by shearing of the initial JVs and PSSs and deformed by an approximately north-south compression formation of thrust faults by exploiting weak shale during the end-Carboniferous Variscan orogeny. horizons and the strike-parallel PSSs in the adjacent Orthogonal sets of fundamental structures form the sandstone intervals. initial assemblage; mutually abutting arrays of 170˚ Development of faults from shearing of initial oriented set 1 joints/veins (JVs) and approximately 75˚ fundamental structural elements with either opening or pressure solution seams (PSSs) that formed under the closing modes in a wide range of structural settings has same stress conditions. Orientations of set 2 (splay) JVs been extensively reported. Segall and Pollard (1983), and PSSs suggest a clockwise remote stress rotation of Martel and Pollard (1989) and Martel (1990) have about 35˚ responsible for the contemporaneous described strike-slip faults formed by shearing of shearing of the set 1 arrays. Prominent strike-slip faults thermal fractures in granitic rocks. Myers and Aydin are sub-parallel to set 1 JVs and form by the linkage of (2004) and Flodin and Aydin (2004) reported strike-slip en-echelon segments with broad damage zones faulting formed by shearing of joints formed by an responsible for strike-slip offsets of hundreds of metres. -
Sedimentary Stylolite Networks and Connectivity in Limestone
Sedimentary stylolite networks and connectivity in Limestone: Large-scale field observations and implications for structure evolution Leehee Laronne Ben-Itzhak, Einat Aharonov, Ziv Karcz, Maor Kaduri, Renaud Toussaint To cite this version: Leehee Laronne Ben-Itzhak, Einat Aharonov, Ziv Karcz, Maor Kaduri, Renaud Toussaint. Sed- imentary stylolite networks and connectivity in Limestone: Large-scale field observations and implications for structure evolution. Journal of Structural Geology, Elsevier, 2014, pp.online first. <10.1016/j.jsg.2014.02.010>. <hal-00961075v2> HAL Id: hal-00961075 https://hal.archives-ouvertes.fr/hal-00961075v2 Submitted on 19 Mar 2014 HAL is a multi-disciplinary open access L'archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destin´eeau d´ep^otet `ala diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publi´esou non, lished or not. The documents may come from ´emanant des ´etablissements d'enseignement et de teaching and research institutions in France or recherche fran¸caisou ´etrangers,des laboratoires abroad, or from public or private research centers. publics ou priv´es. 1 2 Sedimentary stylolite networks and connectivity in 3 Limestone: Large-scale field observations and 4 implications for structure evolution 5 6 Laronne Ben-Itzhak L.1, Aharonov E.1, Karcz Z.2,*, 7 Kaduri M.1,** and Toussaint R.3,4 8 9 1 Institute of Earth Sciences, The Hebrew University, Jerusalem, 91904, Israel 10 2 ExxonMobil Upstream Research Company, Houston TX, 77027, U.S.A 11 3 Institut de Physique du Globe de Strasbourg, University of Strasbourg/EOST, CNRS, 5 rue 12 Descartes, F-67084 Strasbourg Cedex, France. -
The Central Zagros Fold-Thrust Bemt (Iran) : New Insights from Seismic Data Field Observation and Sandbox Modelling S
The Central Zagros fold-thrust bemt (Iran) : New insights from seismic data field observation and sandbox modelling S. Sherkati, J. Letouzey, Dominique Frizon de Lamotte To cite this version: S. Sherkati, J. Letouzey, Dominique Frizon de Lamotte. The Central Zagros fold-thrust bemt (Iran) : New insights from seismic data field observation and sandbox modelling. Tectonics, American Geo- physical Union (AGU), 2006, 25 (4), pp.TC4007. 10.1029/2004TC001766. hal-00069591 HAL Id: hal-00069591 https://hal.archives-ouvertes.fr/hal-00069591 Submitted on 29 May 2021 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Copyright TECTONICS, VOL. 25, TC4007, doi:10.1029/2004TC001766, 2006 Central Zagros fold-thrust belt (Iran): New insights from seismic data, field observation, and sandbox modeling S. Sherkati,1 J. Letouzey,2 and D. Frizon de Lamotte3 Received 10 November 2004; revised 27 January 2006; accepted 29 March 2006; published 20 July 2006. [1] We present five generalized cross sections across levels are activated sequentially from deeper horizons the central Zagros fold-and-thrust belt (Iran). These to shallower ones. However, in one case (Gachsaran sections show that the fold geometry varies de´collement) a shallow de´collement is activated during significantly both horizontally and vertically. -
Gy403 Structural Geology Kinematic Analysis Kinematics
GY403 STRUCTURAL GEOLOGY KINEMATIC ANALYSIS KINEMATICS • Translation- described by a vector quantity • Rotation- described by: • Axis of rotation point • Magnitude of rotation (degrees) • Sense of rotation (reference frame; clockwise or anticlockwise) • Dilation- volume change • Loss of volume = negative dilation • Increase of volume = positive dilation • Distortion- change in original shape RIGID VS. NON-RIGID BODY DEFORMATION • Rigid Body Deformation • Translation: fault slip • Rotation: rotational fault • Non-rigid Body Deformation • Dilation: burial of sediment/rock • Distortion: ductile deformation (permanent shape change) TRANSLATION EXAMPLES • Slip along a planar fault • 360 meters left lateral slip • 50 meters normal dip slip • Classification: normal left-lateral slip fault 30 Net Slip Vector X(S) 40 70 N 50m dip slip X(N) 360m strike slip 30 40 0 100m ROTATIONAL FAULT • Fault slip is described by an axis of rotation • Rotation is anticlockwise as viewed from the south fault block • Amount of rotation is 50 degrees Axis W E 50 FAULT SEPARATION VS. SLIP • Fault separation: the apparent slip as viewed on a planar outcrop. • Fault slip: must be measured with net slip vector using a linear feature offset by the fault. 70 40 150m D U 40 STRAIN ELLIPSOID X • A three-dimensional ellipsoid that describes the magnitude of dilational and distortional strain. • Assume a perfect sphere before deformation. • Three mutually perpendicular axes X, Y, and Z. • X is maximum stretch (S ) and Z is minimum stretch (S ). X Z Y Z • There are unique directions -
Best Practices for Shale Core Handling: Transportation, Sampling and Storage for Conduction of Analyses
Journal of Marine Science and Engineering Review Best Practices for Shale Core Handling: Transportation, Sampling and Storage for Conduction of Analyses Sudeshna Basu 1,2,*, Adrian Jones 1 and Pedram Mahzari 1 1 Department of Earth Sciences, University College London, London WC1E 6BS, UK; [email protected] (A.J.); [email protected] (P.M.) 2 Department of Chemical Engineering, University College London, London WC1E 7JE, UK * Correspondence: [email protected] Received: 9 January 2020; Accepted: 12 February 2020; Published: 20 February 2020 Abstract: Drill core shale samples are critical for palaeoenvironmental studies and potential hydrocarbon reservoirs. They need to be preserved carefully to maximise their retention of reservoir condition properties. However, they are susceptible to alteration due to cooling and depressurisation during retrieval to the surface, resulting in volume expansion and formation of desiccation and micro fractures. This leads to inconsistent measurements of different critical attributes, such as porosity and permeability. Best practices for core handling start during retrieval while extracting from the barrel, followed by correct procedures for transportation and storage. Appropriate preservation measures should be adopted depending on the objectives of the scientific investigation and core coherency, with respect to consolidation and weathering. It is particularly desirable to maintain a constant temperature of 1 to 4 ◦C and a consistent relative humidity of >75% to minimise any micro fracturing and internal moisture movement in the core. While core re-sampling, it should be ensured that there is no further core compaction, especially while using a hand corer. Keywords: shale; drill core instability; micro fracture; clay minerals 1.