81. Geology (GEOL) Course Descriptions mechanisms of brittle and ductile deformation, and mechanics of folding,faulting, and salt tectonics. (Sp). G5130 Advanced Field geology. 1 to 6 hours. http://www.ou.edu/bulletins/courses/geology_courses.htm

Geology (GEOL) 1003 Volcanoes and Earthquakes. Prerequisite: high school chemistry and algebra. Worldwide distribution of volcanic and earthquake activity; types of volcanic eruptions and associated landforms and rocks; causes of and techniques for location of earthquakes; prediction of volcanic eruptions and earthquakes; social consequences of predictions and actual volcanic and earthquake activity. (F, Sp) [II-NL] Global Environmental Change. Past and present change on Earth from a global geologic perspective. Philosophy and methods of science, structure of the earth, plate tectonics, global catastrophes and geologic hazards, human impacts on the environment, global warming, pollution, ozone depletion, acid rain, resources, consumption, population growth, energy and technology. (Sp) [II-NL] 1024 The History of the Earth and Life. The origin of the Earth and solar system. Rocks and minerals; geologic time; plate tectonics and continental drift. The ocean-atmosphere system; climate change over time; biological evolution. The fossil record of early life; the "Cambrian Explosion" of life in the oceans; invertebrate animals and their geological history. Geological history of fishes; evolution of plants. Terrestrial vertebrates, including dinosaurs and mammals. Mass extinctions; human evolution; impact of human activities on the global environment and the biosphere. A student may not receive credit for both 1024 and 1114.

82. Salt Tectonics - South Oman Salt Basin salt tectonics South Oman salt Basin. Badar H. Al-Barwani1, Ken McClay2, andChris Elders1. (1) geology Department, Royal Holloway University of London, http://aapg.confex.com/aapg/sl2003/techprogram/paper_78447.htm

Salt Tectonics - South Oman Salt Basin Badar H. Al-Barwani , Ken McClay , and Chris Elders . (1) Geology Department, Royal Holloway University of London, Royal Holloway College, Egham, Surrey, TW20 OEX, United Kingdom, phone: (44)1784 414 250, fax: (44) 1784 471 780, badar@gl.rhul.ac.uk, (2) Department of Geology, Royal Holloway University of London, Egham, Surrey, TW20 0EX, United Kingdom This paper presents an analysis of salt structures in the South Oman Salt Basin (SOSB), utilizing 2D and 3D seismic data to establish 3D geometries of the salt structures and the effects of variable 3D sedimentation on basin evolution. An understanding of the timing and 3D geometries of salt movement gives an insight into the evolution of carbonate stringers within the Ara salt, which is the main exploration target in the SOSB. AAPG: Global Salt Tectonics AAPG Annual Meeting 2003: Energy - Our Monumental Task Technical Program

83. Salt Tectonics Above Complex Basement Extensional Fault Systems: Results From An Royal Holloway University Of London, geology Department, Egham Hill, Egham, Physical models of salt tectonics related to thickskinned extension are http://aapg.confex.com/aapg/hu2002/techprogram/paper_25164.htm

Salt Tectonics above Complex Basement Extensional Fault Systems: Results from Analog Modeling Tim Dooley, Fault Dynamics Research Group, Royal Holloway University Of London, Geology Department, Egham Hill, Egham, TW20 0EX, United Kingdom, phone: 44-1784-443618, tim@gl.rhul.ac.uk, Ken McClay , Fault Dynamics Research Group, Department of Geology, Geology Department, Egham Hill, London, TW20 0EX, United Kingdom, and Mark Hempton, Shell UK Ltd, 1 Altens Farm Road, Nigg, Aberdeen, AB12 3FY, United Kingdom. Physical models of salt tectonics related to thick-skinned extension are largely confined to 2D structures. An experimental program, utilising silicone polymer and silica sand/ceramic beads as ductile and brittle analogs respectively, was designed to investigate the 3D relationships between salt diapirs and intersecting basement fault systems seen in the Central Graben, UK North Sea. During extension, intersection points in the basement fault system generate complex single, 2-way or 3-way, flap structures in the overburden, localizing cover deformation and footwall diapiric activity on the rift margins. Flap structures and associated diapirs are located adjacent to, but diagonally inboard of, the basement intersection points and consist of convex-to-the-hangingwall fault segments that are gradually breached with increasing extension. Major diapirs that attain passive status accommodate much of the continued basement extension through downbuilding. Intra-basin horst systems develop inwardly-dipping graben cored by a major salt wall during initial extension. Axial flow along this structure feeds growing diapirs. Grounding of the brittle overburden results in source cut-off and deflation of the salt wall due to continued expansion by extensional faulting.

84. UB - Programes De Doctorat De La Universitat De Barcelona. Consulta D'assignatur Strikeslip, salt tectonics. Fault mechanics and deformation mechanisms Journal of Geophysical Research Journal of Structural geology tectonics http://www.ub.es/div3/3cicle/doctorate/Assignatures/conques/geoestruct.htm

University of Barcelona : Doctoral Programmes Taught Modules Programme Title : EXPLORATION, ANALYSIS AND MODELLING OF BASINS AND OROGENIC SYSTEMS Biennium : Module Title : STRUCTURAL GEOLOGY FOR OIL EXPLORATION: STRUCTURAL STYLES Department : GEODYNAMICS AND GEOPHYSICS Professor : KEN MCCLAY Number of credits : Module Syllabus : 2D extensional structures, 3D extensional structures, inversion, thrust systems Strike-slip, salt tectonics. Fault mechanics and deformation mechanisms Reading List : Marshak, S. and Mitra, G. 1988. Basic Methods of Structural Geology. Prentice Hall, New Jersey. 446 pp. McClay, K.R. 1988. Mapping of Geological Structures. John Wiley and Sons. McClay, K. R. , 2003. Advanced Structural Geology for Petroleum Exploration. Course Notes, 550 pp. Ragan, D.M. 1973. Structural Geology. Wiley 208 p. Ramsay, J.G. 1967. Folding and Fracturing of Rocks. McGraw Hill 568 pp. Ramsay, J.G. and Huber, M.H. 1983. Techniques of Modern Structural Geology. Volume I. Strain Analysis . Academic Press, London. 330 pp. Ramsay, J.G. and Huber, M.H. 1983. Techniques of Modern Structural Geology. Volume II. Folds and Faults. Academic Press, London. 700 pp.

85. The Leading Edge -- Sign In Page The salt tectonics of offshore Morocco may provide some very specific (Marineand Petroleum geology, 2000). Tectonic and depositional history of the http://tle.geoscienceworld.org/cgi/content/full/19/10/1074

Quick Search: advanced search GSW Home GeoRef Home My GSW Alerts ... SEARCH This item requires a subscription to GeoScienceWorld. Full Text Salt tectonics in the Atlantic margin of Morocco Tari et al. The Leading Edge. This Article Figures Only Full Text (PDF) Submit a response ... Alert me if a correction is posted Services Email this article to a friend Alert me to new issues of the journal Download to citation manager GeoRef GeoRef Citation To view this item, select one of the options below: Sign In User Name Sign in without cookies. Can't get past this page? Help with Cookies. Need to Activate? Password Forgot your user name or password? Athens users Sign in via Athens : Access is available using your Athens username and password. Contact your library if you do not have an Athens username and password. List of Athens registered sites , including contact details. Sign Up Subscribe to the Journal - Subscribe to the print and/or online journal. JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ... SEARCH

86. Houghton Mifflin College Structural geology, Reflection Seismology and Plate tectonics (multiple courses) tectonics and Mountain Building. Active tectonics salt tectonics http://college.hmco.com/geology/resources/geologylink/toc/topic09.html

GeologyLink The Earth Today In the News Virtual Classroom ... Glossary Student Resource Center GeologyLink Inside Geology Folds, Faults, and Mountains Lecture Links Related Links Lecture Links Links to Intro Geology Course Notes Physical Geology -University of Houston Introduction to Physical Geology -University of Colorado, Boulder Physical Geology and another version of Physical Geology -Georgia Perimeter College Listing of Online General Geology Courses -University of Connecticut (go to the individual courses for lecture notes) Exploring the Geological Sciences -University of Florida How the Earth Works - Bryn Mawr The Dynamic Earth - Miami University of Ohio Planet Earth - Penn State Introductory Geology - Duke University (images for each lecture rather than notes) Introduction to Geology - California State University, San Jose Introductory Geology - SUNY Oswego How the Earth works: Dynamic Planet - University of Michigan Physical Geology - University of New Brunswick Physical Geology - University of Toronto Links to Advanced Courses with Lecture Notes Structural Geology -Cornell University Geodynamics -University of Washington Structural Geology, Reflection Seismology and Plate Tectonics

87. Dr. Bruce Trudgill Basins Group at the TH Huxley School as a Lecturer in geology and Geophysics.His main research interests lie in the tectonics of sedimentary basins. http://www.huxley.ic.ac.uk/research/Basins/people.php?ID=19

88. Geodynamics / Petrology traps in fold/thrust belts and salt tectonic terrains (Swiss Alps, Gulf ofMexico); Karl Mueller Structural geology, tectonic geomorphology, http://www.colorado.edu/GeolSci/geophysics.html

Geodynamics / Petrology The study of dynamic processes within the Earth and on the surface of Earth and other planets is the subject of numerous research programs and academic courses in which the Department and the facilities of two affiliated institutes, CIRES and LASP , are closely interrelated. The interdepartmental Geophysics Ph.D. Program links expertise in geophysics across the campus. Research Programs In addition to field studies in Colorado and other areas of the western U.S., field programs are currently active in igneous petrology, economic geology, and geochemistry in Mexico, Chile, Peru, southern Africa, and Nepal. Through ties with other departments and LASP A research branch of the Water Resources Division of the U.S. Geological Survey is also housed on the University campus. Numerous cooperative research projects exist between personnel of the U.S. Geological Survey and University faculty in the water sciences. Members of the faculty also collaborate with scientists at the Los Alamos National Laboratory in neutron diffraction studies of mineral structures, and with scientists at the U.S. Geological Survey in Denver in a variety of disciplines including trace elements, stable and radiogenic isotopes, and mineral spectroscopy Research Facilities Diverse facilities are available at CU/Boulder.

89. CGG Brokerage Offices From the exploitation point of view, the thrust and salt tectonic styles caused the Lageson, DL, 1984 Structural geology of Stewart Peak Culmination, http://www.cgg.com/proserv/reservoir/papers/rivas.html

Structural Model of the Chiapas-Tabasco Area (Southeast Mexico) By J.Z. Rivas (CGG-ASI) The purpose of this study is to find a structural model that agrees with local geologic information and explains production behaviors. Surface and subsurface data are analyzed and interpreted to determine the Chiapas-Tabasco structural model. Basic concepts of extensional and compressional regimens to methods of balanced cross sections and relationships among faults are developed using 2D and 3D seismic data. This process is integrated with the global tectonic and the regional stratigraphy of Southern Mexico. The data analyzed point out that only wrench-compressional structures are present in the Chiapas-Tabasco area. Structural geometries as fault-bend foldings and ramps are interpreted. Décollement (footwall flats) of the thrust faults, located in the Jurassic salt, are not clearly identified due to the lack of seismic information beneath the Cretaceous and the Jurassic poor acoustic impedance contrast. The Chiapas-Tabasco area is classified as a "Duplex Thrust System" (Boyer and Elliott classification of systems of thrusts, 1982). The oil structural traps found in the Chiapas-Tabasco area are located in fault-bend foldings caused by thrust-tectonism. Potential oil traps are probably located beneath the actual known fault-bend folding oil traps.

90. Africareg Petroleum geology of Africa New Themes and Developing Technologies Examples ofsalt tectonics from West Africa a comparative approach http://users.powernet.co.uk/geopubs/africareg.htm

AFRICA REGIONAL MAPS Link to Geopubs Home Page updated: 21 October 2002 Africa - Geological Map 1:5,000,000. UNESCO/CGMW, 1986-91, 6 sheets. This high quality map represents the most detailed geological coverage available for some parts of Africa, as well as providing excellent reference material. AFRGLM001 - Complete set of six individual sheets - £125-00. Six sheets assembled into one large "Multimake" map - AFRGLM001M - £350-00. NEW in 2003. Petroleum Geology of Africa: New Themes and Developing Technologies Contents - A map compilation and synthesis of Africa's petroleum basins and systems - 2nd and 3rd Millennium Reserves Development in African Basins - Africa's Petroleum Systems: four tectonic aces in the past 600 million years - Tectonic Development of North African Basins - Examples of salt tectonics from West Africa: a comparative approach - Syn-rift regional subsidence across the West African continental margin: the role of lower plate ductile extension - Play fairways of the Gulf of Guinea transform margin - Prospectivity in ultra deep water: The case for petroleum generation and migration within the outer parts of the Niger Delta Apron - Frasnian organic-rich shales in North Africa: regional distribution and depositional model - Aptian source rocks in some South African cretaceous basins - Geochemical evaluation of East Sirte Basin (Libya) petroleum systems and oil provenance - Gravity Signatures of Sediment Systems - Predicting Reservoir Distribution in Angolan and Brazilian Basins

91. Page Not Found Assistant Professor of geology Ph.D. Stanford University, 1999 tectonics andclimate impact basin formation and evolution and I am interested in these http://geoscience.unlv.edu/Faculty_Staff/hanson.html

Quick Find About UNLV Academic Advising Academic Calendar Administrative Units Catalogs, Schedules Community Links Distance Education Educational Outreach Events Calendar Facilities Management Human Resources Performing Arts Ctr Police Department Public Affairs Student Life Tickets Transcripts WebCT Web Services We're sorry! The page you were trying to view does not exist or has moved. If you found the link on UNLV's site, please report the error to the webmaster listed on the referring page. A contact e-mail address should appear somewhere on that page. To aid you in your search, the following tools are available for UNLV's website. Search the UNLV Web Site Search Tips A-Z Index Use this listing to search alphabetically by topic. Directories Check this page to search for employees and their e-mail addresses. Also available is our Experts Directory, Speakers Bureau, and departmental directory. Also check out: About UNLV Maps / directions

92. Polish Geological Institute Key words glacioisostatic movements, salt tectonics, neotectonics, Quaternarygeology, Pleistocene, northwestern Poland. http://www.pgi.gov.pl/pgi_en/index.php?option=articles&task=viewarticle&artid=49

93. Safaricz IfG UP Marine and Petroleum geology 17 (5), 601–618. PDF 2.5 MB In salt TectonicsProject Phase III, Final Report (Davison, I., Evans, N., Alsop, http://www.geo.uni-potsdam.de/mitarbeiter/Safaricz/Safaricz_Publications/Safaric

Publications Reviewed Journal Articles Professional Industry Reports Conference Abstracts Theses Reviewed Journal Articles Safaricz, M. [PDF 4 MB] Safaricz, M. [PDF 2.5 MB] Safaricz, M. Safaricz, M. Professional Industry Reports Safaricz, M. 1999. Which parameters control the geometries of deformation structures? A review on experimental modelling of geological deformation with focus on overburden deformation around salt diapirs. Consultancy report for Japan Petroleum Exploration Co. (JAPEX), 21 p. Safaricz, M. Safaricz, M. Safaricz, M. Safaricz, M. Safaricz, M. Safaricz, M. Safaricz, M. Safaricz, M. Safaricz, M. Safaricz, M. Safaricz, M. Safaricz, M. Safaricz, M. Safaricz, M. Safaricz, M. Safaricz, M. Conference Abstracts Safaricz, M. Davison, I., Evans, N., Safaricz, M. Safaricz, M. 1998. Central Graben Salt Diapir Fields, N. Sea: Geometry and Structural Evolution. European Geophysical Society: 23rd General Assembly, Nice (France), April Safaricz, M. Safaricz, M. Safaricz, M. Safaricz, M. April Safaricz, M. Safaricz, M. Safaricz, M. Theses Safaricz, M.

94. Dictionary Page CO.UK - Geology UK geology Don’t know the meaning of some words? Tired of listing through allthe encyclopedias? Your friends make jokes on you because of your ignorance? http://geology.b.dictonarypage.co.uk/

Geology -oid a a axis Geology -oid a a axis ... zones of regional metamorphism

95. Page Has Moved Bureau of Economic geology s. site has moved. This page has moved tohttp//www.beg.utexas.edu/indassoc/agl/saltani.htm http://www.utexas.edu/research/beg/giovanni/

Bureau of Economic Geology's site has moved. This page has moved to http://www.beg.utexas.edu/indassoc/agl/saltani.htm You should be taken there automatically in a few seconds... Please update your bookmarks!

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