DOCSLIB.ORG

Download the Course Outline

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Download the Course Outline Competence Level: N144: Rift Systems, Faulting and 5 Days Skilled Fault-Controlled Sedimentary Architecture: Gulf of Corinth Field Course (Greece) Classroom Elements Instructor(s): Mary Ford and Ed Williams Low Physical Demand Summary This course evaluates rift stratigraphy and structure, the geometry and kinematics of a normal fault network and the facies of selected Gilbert-type fan deltas. Participants will examine fluvial successions, fan deltas and turbidites deposited in an active rift; the controlling factors in delta construction and distribution; geometry, connectivity and growth of a normal fault network; the interaction of surface processes and tectonics in active rifts. This course will primarily be of use in exploration but is also applicable to reservoirs and oil fields in extensional settings during appraisal, development and production. Learning Outcomes Participants will learn to: 1. Assess the tectonic setting and evolution of the Corinth Rift; evaluate the rapidity and scale of the rifting processes compared with other rift systems. 2. Evaluate the geometry, kinematics and evolution of a normal fault system. 3. Understand the evolution of rift stratigraphic architecture in time and space. 4. Assess geometry and sediment infill of an individual fault block. 5. Construct a cross-section through part of the rift. Calculate the heave and throw of faults, individually and cumulatively. 6. Compare and contrast fault block stratal and structural geometries, including syn-sedimentary block tilting and folding. 7. Evaluate the role of inherited palaeotopography in rift basins. 8. Examine a detailed case history of relay ramp evolution and assess its influence on sedimentary input and the location of deltas. 9. Describe and interpret the stratal architecture and key surfaces of a Gilbert-delta and evaluate operative tectonic versus eustatic controls. 10. Compare models for rifting and normal fault growth mechanisms, strain localisation and the effects on sediment distribution. 11. Analyse sediment routing systems in an evolving rift and their influence on the distribution of sediments (thickness and facies). Duration and Training Method This is a five-day course, consisting primarily of field work with some classroom tuition. The proportion of field and classroom time is approximately 80/20. Classwork will comprise presentations and practical exercises such as construction of cross sections. Outcrop investigations will be linked to subsurface examples with a particular emphasis on reservoir geology. Course Outline Competence Level: N144: Rift Systems, Faulting and 5 Days Skilled Fault-Controlled Sedimentary Architecture: Gulf of Corinth Field Course (Greece) Classroom Elements Instructor(s): Mary Ford and Ed Williams Low Physical Demand Physical Demand The physical demands for this class are LOW according to the Nautilus Training Alliance field course grading system. There will be multiple walks of up to 1 km (0.5 miles) most days. The longest walk is approximately 3 km (1.5 miles) with an ascent (and descent) of 200 m (80 feet). The field area is at an elevation approximately 300 m (1000 ft) and conditions are variable but likely to be hot. There may be rain from late autumn to early spring. Transport will be by minicoach on paved roads. Who Should Attend The course is relevant for all geoscientists who wish to broaden and deepen their knowledge of tectonics and sedimentation in rift systems. The course will provide a working knowledge of these systems for graduates and inexperienced staff, while providing deeper insights to more experienced participants for more detailed application to subsurface projects. Multidisciplinary teams working assets in extensional settings would benefit from collaborating in this field environment. Prerequisites and Linking Courses It is assumed that participants will have a basic knowledge of structural geology and sedimentology and be familiar with associated terminology before attending the class. This course is complementary to other courses focusing on extensional tectonics and fault systems such as N041 (Extensional Tectonics and Normal Fault Patterns, Utah). Course Content The Gulf of Corinth is one of the fastest opening rifts in the world with a rate of NS extension of up to 1.6 cm/yr. On the south side of the Gulf, the rift’s tilted fault blocks and their synrift succession (Late Pliocene-Middle Pleistocene) are exceptionally well-exposed due to rapid uplift up to 1200 m and deep incision by rivers. The onshore clastic rift succession, up to 2.8 km thick, includes a series of spectacular giant Gilbert-type fan deltas (up to 800 m thick, radii up to 4 km) that are used as analogues for reservoirs. These are exposed on cliffs up to 800 m high, where their stratigraphic architecture and facies can be studied in detail. Theme 1 The behaviour of the normal fault network during evolution of the rift, in particular the distribution of displacement on the fault network in space and time and the apparent abandonment of large parts of the network as tectonic activity became focussed within a relatively narrow basin in the last one million years. The narrowness of the fault blocks (4 to 8 km wide) is also a topic of debate. Course Outline Competence Level: N144: Rift Systems, Faulting and 5 Days Skilled Fault-Controlled Sedimentary Architecture: Gulf of Corinth Field Course (Greece) Classroom Elements Instructor(s): Mary Ford and Ed Williams Low Physical Demand Theme 2 The stratigraphic architecture and facies distribution within the Plio-Pleistocene syn-rift stratigraphy. Particular attention has been focused on the giant Gilbert-type fan delta systems. Exercise topics and practical work that will be taught with this fieldtrip: Geometry and kinematics of extensional fault systems. Interpretation of rift geometries and successions. Lithostratigraphy of rifts. Typical facies and thickness distributions in space and time. Geodynamics of rifts (theoretical analysis of processes involved in rift evolution. syn-rift, post-rift phases, necking, the uniform stretching model and more recent models). Cross-section construction based on field observations, reconstruction of the Corinth rift history. Itinerary The course will undertake field excursions to the Vouraikos Valley, Kerinitis Valley, Krathis valley and Derveni area, all within 1 hour’s drive from the hotel. Participants will construct cross-sections and make stratigraphic correlations across a series of fault blocks, each with a different geometry and stratigraphic architecture. Day 0: Assemble at Athens airport, travel to the Gulf of Corinth with short visit to the Corinth canal. Check in to hotel at Elaionas, followed by Course Introduction, and Safety Brief. Day 1: General overview and introduction to the Corinth Rift. Geometry and stratigraphy of a single fault block (Trapeza, Ano Diakofto, Asomati Plateau, West Helike Fault) Day 2: Vouraikos section: Fault block geometry and stratigraphic architecture (Mikros church, Doumena east, Kato Zachlorou, Megha Speleo, Kalavryta road junction, Railway crossing) Day 3: Krathis section: relay ramp evolution, lateral variations in rift infill and fault geometries (Bridge to Kalamia and Bougsismos, Vallimi North, Tsivlos road exercise,Tsivlos Lake, Mavra Litharia, Krathis-Diakopto Road corals) Course Outline Competence Level: N144: Rift Systems, Faulting and 5 Days Skilled Fault-Controlled Sedimentary Architecture: Gulf of Corinth Field Course (Greece) Classroom Elements Instructor(s): Mary Ford and Ed Williams Low Physical Demand Day 4: The Keranitis Gilbert-type fan delta (Aghio Andreas area, Keranitis valley) Day 5: Eastern rift and its Gilbert deltas and prodelta turbidites (Evrostini delta panorama, Medourianika south, Evrostina road). Travel to Athens, final group dinner. Day 6: Depart Athens. Course Outline.
Load more

Recommended publications
  • KALAVRYTA: Occupation of 1941-1944 and the Holocaust of December 13, 1943 Memories from the Village of Aghios Nikolaos
    KALAVRYTA: Occupation of 1941-1944 and the Holocaust of December 13, 1943 Memories from the Village of Aghios Nikolaos The Grieving Mother of Kalavryta Peter N. Demopoulos LOS ANGELES, 2017 KALAVRYTA: Occupation of 1941-1944 and the Holocaust of December 13, 1943 Memories from the Village of Aghios Nikolaos Peter N. Demopoulos …and you shall know the truth and the truth shall set you free. (John 8.32) 2017 First published in 2013 by Peter N. Demopoulos and the Hellenic University Club of Southern California in Los Angeles, California, www.huc.org . © Copyright 2015, 2017, Peter N. Demopoulos and the Hellenic University Club of Southern California. All rights reserved. Work may not be reproduced without permission by Peter N. Demopoulos or the publisher. Quoting is permitted with a reference to the source and a notice to the publisher at [email protected]. Published by the Hellenic University Club of Southern California PO Box 45581 Los Angeles, CA 90045-0581 USA ISBN-13: 978-1-938385-00-1 949.507 DF849 Published in the United States of America Second Edition 2017 10 9 8 7 6 5 4 3 2 1 Also, can be found Online in GREEK and ENGLISH at the Hellenic University Club website www.huc.org Click on “Publications” and wait a few seconds for it to download. Contact: Peter N. Demopoulos 7485 McConnell Ave., Los Angeles, CA 90045 Phone/FAX: 310.215.3130 m: 310.923.1519 [email protected] TABLE OF CONTENTS Page Foreword……………………………………………………………………………………………………. 5 Acronyms…………………………………………………………………………………………………… 6 Greeks Defend Themselves Against the Invaders, 1940-1941…………………….. 6 The Italian Occupation ……………………………………………………………………………….
    [Show full text]
  • Developing a Biotic River Typology and Defining Reference Conditions in the Rivers of Greece: a Spatially- Based Approach
    Developing a biotic river typology and defining reference conditions in the rivers of Greece: a spatially- based approach A.N. Economou, S. Zogaris, S. Giakoumi, R. Barbieri & D. Petridis Abstract Developing a biotic river typology and reference conditions are vital components of ecological assessment using fish. In Greece, due to the absence of systematic monitoring data, fish sampling data from previous ichthyological surveys conducted primarily in the southern and western parts of the Hellenic Western Balkan ecoregion (Illies' ecoregion 6) were utilised. These surveys were undertaken for the purpose of fish conservation and were not designed with the prospect of ecological assessments. As a consequence, the sampling methodologies, the site selection criteria, the analytical procedures and the recorded parameters were not in line with the requirements of the WFD. A brief synopsis of the main environmental features of the Greek rivers which indicate a remarkable environmental heterogeneity is presented. Greece is a geographically fragmented mountainous country with a large number of medium and small sized rivers. Most rivers run through narrow mountain valleys that descend abruptly to the coast. Usually a mountain river becomes a lowland river very near its estuary. As a result many small and medium sized rivers have a flashy and erosive behavior and suffer from the lack of lowland riverine habitat. Lowland rivers are usually small; large floodplain rivers are very few, almost wholly restricted to northern Greece. Precipitation is irregularly distributed and hydrology varies remarkably among basins. Semi-arid regions and areas with seasonally arid conditions exist in parts of the south and southeast where localized karstic springs play an important role in enabling perennial water flows.
    [Show full text]
  • 19 March 2009
    THE GREEK AUSTRALIAN The oldest circulating Greek newspaper outside VEMA Greece MARCH 2009 Tel. (02) 9559 7022 Fax: (02) 9559 7033 E-mail: [email protected] OUR PRIMATE’S VIEW THE PARABLE OF THE PRODIGAL SON PAGES 4/22 - 5/23 STIMULUS St Andrew’s PAYMENTS Theological College SCRIPTUREenters 24th LESSONS year of teaching will support jobs PAGE 7/25 Stimulus package handouts will minimise unemployment one-off training and learning bonus and education entry as the economy slows, Treasurer Wayne Swan says. payment is paid to eligible students. Parents, carers and farmers started receiving bonus The one-off bonus of up to $900 for taxpayers earning payments of up to $950 from Wednesday 11 March, as part less than $100,000 will flow from April. of a $42 billion fiscal stimulus package. In December, pensioners and low-income families were “Now these bonuses are a key part of our efforts to on the receiving end of cash payments from the support jobs by strengthening demand in the economy so government’s initial $10.4 billion stimulus package. that companies can afford to keep on and employ workers The coalition opposes the government’s second stimulus because there is sufficient demand in the economy,” Mr package. Swan told parliament during question time. Mr Swan quoted a speech by former treasurer Peter Treasury forecasts released last month predicted the Costello, delivered in 2001 during the last global economic unemployment rate would climb to seven per cent by mid- slowdown, to undermine the opposition’s position. 2010 as 300,000 jobs were lost.
    [Show full text]
  • Back Matter (PDF)
    Index Page numbers in italics refer to Figures. Page numbers in bold refer to Tables. Acidere Formation 205 Catalina-Rincon Mountains Permo-Triassic evolution 36 Acigo¨l Fault 199 (Arizona, USA) 4 magmatism 39–44 acoustic fluidization 17 Central Anatolide Crystalline Complex metamorphism 36–39 Aegean extensional province 198 sedimentary basins and tectonic map 198 Central Finland Granitoid Complex 229 volcanics 44–47 tectonic setting 197–198, 200 crust detail 242, 245, 246 map 35 Aegean Sea structure interpretation 237, 238 numerical analysis of geological geodynamics 181–183 Central Volcanic Region (New Zealand) evolution geological map 140 74, 79, 81–83 model set-up 47–49 tectonic map 170, 181 chlorite, and fault strength 15 thermomechanics 50–52 Agridi Fault 126, 127, 129, 130, 131 clays, reactions and fault strength 15 numerical and natural data compared Akrata Fault 129 Coastal Fault System 141, 144, 145 52–53 Alasehir detachment 199, 205 collisional modelling 225–226 magmatism 58–64 Alasehir graben 215, 217 continental back-arc systems 73 metamorphism 53–58 Alasehir granitoid 199, 202 conceptual model 74 sedimentary basins and Alpine orogeny 34–36 studies in New Zealand, extension in volcanics 64 Amonton’s Law 11–12, 17 relation to local variables Evciler granitoid 199 Amorgos detachment crustal structure 78–81 Evia 140, 141 geological setting 171–173 extension and arc migration 78 exhumation, factors affecting 179 map 170 extension–rotation relations 78 extension timing of detachment geodetic strain estimates 76–77 and isostasy
    [Show full text]
  • Structural Cross Sections Through the Corinth-Patras Detachment Fault-System in Northern Peloponnesus (Aegean Arc, Greece) N
    Δελτίο της Ελληνικής Γεωλογικής Εταιρίας, Τομ. XXXIV/1, 235-241, 2001 Bulletin of the Geological Society of Greece, Vol. XXXIV/1, 235-241, 2001 Πρακτικά 9ου Διεθνούς Συνεδρίου, Αθήνα, Σεπτέμβριος 2001 Proceedings of the 9th International Congress, Athens, September 2001 STRUCTURAL CROSS SECTIONS THROUGH THE CORINTH-PATRAS DETACHMENT FAULT-SYSTEM IN NORTHERN PELOPONNESUS (AEGEAN ARC, GREECE) N. FLOTTÉ1 & D. SOREL1 ABSTRACT Structural mapping in northern Peloponnesus reveals the emergence of an E-W striking, more than 70km long, low angle detachment fault dipping to the north beneath the Gulf of Corinth. This paper describes four north-south structural cross-sections in northern Peloponnesus. Structural and sedimentological field observa­ tions show that in the studied area the normal faults of northern Peloponnesus branch at depth on this major low angle north-dipping brittle detachment. The southern part of the detachment and the related normal faults are now inactive. To the north, the active Helike and Aigion normal faults are connected at depth with the seismically active northern part of the detachment beneath the Gulf of Corinth. KEY WORDS: rifting, Corinth Gulf, Peloponnesus, detachment normal fault, Pleistocene INTRODUCTION : GEODYNAMIC SETTING AND STRUCTURAL FRAME Some 130 km long and 5 to 20 km wide, the Corinth-Patras rift is the major active transverse structure of the Aegean Arc (Fig. 1). Fault kinematics (Sibrier, 1977), earthquakes focal mechanisms (e.g. Hatzfeld et al, 1996), and satellite geodesy (Clarke et al, 1998) indicate a N0° to 20°E direction of extension. The extension rate increases toward the west (Le Pichon et al., 1994; Clarke et al., 1998): from 0.5cm/yr near Corinth, it reaches 1.5cm/yr near Aigion.
    [Show full text]
  • Drama, O Agora, 27.04.2009 Platanenaue, 272 M Dra 132, KF 75.87.00, 41°08'04''N, 24°21'22''E
    A Willing Contribution to Flora Hellenica Field records 2010 von Eckhard & Rita Willing Dessau January 2011 Published by BGBM Press Botanic Garden and Botanical Museum Berlin-Dahlem Freie Universität Berlin Berlin, 2012 ISBN 978-3-921800-77-5 http://dx.doi.org/10.3372/wfr2010 © Eckhard & Rita Willing, 2011 The Botanic Garden and Botanical Museum Berlin-Dahlem as publisher reserves the right not to be responsible for the topicality, correctness, completeness or quality of the information provided. The information provided is based on material identified and named by the authors. The entire collections are preserved in the Herbarium of the Botanic Garden and Botanical Museum Berlin- Dahlem, where the determinations can be reassessed. This publication should be cited as: Willing E. & Willing R. 2011: A Willing contribution to Flora Hellenica. Field records 2010. – Berlin: Botanic Garden and Botanical Museum Berlin-Dahlem, published at http://dx.doi.org/10.3372/wfr2010 Address of the authors: Eckhard & Rita Willing Augustenhof 14 D-06842 Dessau-Roßlau Germany [email protected] 2 1. Einführung Wie in den vergangenen Jahren möchten wir hiermit über die Ergebnisse unserer letzten Sammelreise für die Flora Hellenica berichten. Die im Jahr 2010 gesammelten Pflanzen sind jetzt alle montiert, bestimmt (einige nur bis zur Gattungsebene), etikettiert, in die Accessdatenbank eingegeben, als solche auch verfügbar und sämtlichst ab sofort im Botanischen Museum Berlin- Dahlem einzusehen. Als Sammelgebiete für 2010 hatten wir ursprünglich das Bergland der Zentral-Peloponnes gewählt. Auf Wunsch von Bearbeitern der Flora Hellenica haben wir dies relativ spät geändert und die böotische Ebene mit ihren angrenzenden Hügelketten und die Insel Euböa angesteuert.
    [Show full text]
  • Rifting and Shallow-Dipping Detachments, Clues from the Corinth
    Rifting and shallow-dipping detachments, clues from the Corinth Rift and the Aegean Laurent Jolivet, Loic Labrousse, Philippe Agard, Olivier Lacombe, Vivien Bailly, Emmanuel Lecomte, Frédéric Mouthereau, Caroline Mehl To cite this version: Laurent Jolivet, Loic Labrousse, Philippe Agard, Olivier Lacombe, Vivien Bailly, et al.. Rifting and shallow-dipping detachments, clues from the Corinth Rift and the Aegean. Tectonophysics, Elsevier, 2010, 483 (3-4), pp.287-304. 10.1016/j.tecto.2009.11.001. insu-00448474 HAL Id: insu-00448474 https://hal-insu.archives-ouvertes.fr/insu-00448474 Submitted on 19 Jan 2010 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. 1 Rifting and shallow-dipping detachments, clues from the Corinth Rift and the Aegean Laurent Jolivet 1,2, Loïc Labrousse 1, Philippe Agard 1, Olivier Lacombe 1, Vivien Bailly 1, Emmanuel Lecomte 1, Frédéric Mouthereau 1, Caroline Mehl 3 1 ISTEP, UPMC-Paris6, UMR 7193, T 46-00 E1, 4 Place Jussieu, 75252 Paris cedex 05 2 Now at: ISTO, UMR 6113, Université d'Orléans 1A, Rue de la Férollerie, 45071 Orléans Cedex 2, France 3 Ecole des Mines de Paris, Centre de Géosciences, 35 rue Saint Honoré, 77300 Fontainebleau France Keywords: Aegean, Corinth, rifting, post-orogenic extension, detachment, Phyllite-Quartzite Abstract : The Corinth Rift is superimposed on the Hellenic nappe stack that formed at the expense of the Apulian continental crust above the subducting African slab.
    [Show full text]
  • The Structures, Stratigraphy and Evolution of the Gulf of Corinth Rift, Greece Brian Taylor, Jonathan R
    The structures, stratigraphy and evolution of the Gulf of Corinth rift, Greece Brian Taylor, Jonathan R. Weiss, Andrew M. Goodliffe, Maria Sachpazi, Mireille Laigle, Alfred Hirn To cite this version: Brian Taylor, Jonathan R. Weiss, Andrew M. Goodliffe, Maria Sachpazi, Mireille Laigle, et al.. The structures, stratigraphy and evolution of the Gulf of Corinth rift, Greece. Geophysical Jour- nal International, Oxford University Press (OUP), 2011, 185 (3), pp.1189 - 1219. 10.1111/j.1365- 246X.2011.05014.x. hal-01399970 HAL Id: hal-01399970 https://hal.archives-ouvertes.fr/hal-01399970 Submitted on 21 Nov 2016 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. Geophysical Journal International Geophys. J. Int. (2011) 185, 1189–1219 doi: 10.1111/j.1365-246X.2011.05014.x The structures, stratigraphy and evolution of the Gulf of Corinth rift, Greece Brian Taylor,1 Jonathan R. Weiss,1 Andrew M. Goodliffe,2 Maria Sachpazi,3 Mireille Laigle4 and Alfred Hirn4 1Department of Geology and Geophysics, School of Ocean and Earth Science and Technology, University of Hawaii at Manoa, Honolulu, HI, USA. E-mail: [email protected] 2Department of Geological Sciences, The University of Alabama, Tuscaloosa, AL, USA 3Geodynamic Institute, National Observatory of Athens, Athens, Greece 4Laboratoire de Sismologie Experimentale,´ Departement´ de Sismologie, Institut de Physique du Globe de Paris, Paris, France Accepted 2011 March 8.
    [Show full text]
  • Full Table of Projects
    CATEGORY 2: URBAN PLANNING and URBAN DESIGN PROJECTS TABLE 2.1 URBAN DESIGN PROJECTS COMMISSION CONSTRUC PARTICIPA a/n PROJECT STUDY A K K ASSOCIATES CLIENT TION TION (%) EUROPAN - 3, Competition. Hellenic Ministry for the Environment, "At home in the city. 2.1.1 Physical Planning & 1994 50% Μ.Katsaros 50% Urbanising Residential Public Works, Areas", Pyrgos - Hellas EUROPAN First Prize ΕUROPAN- 4, Competition . "Constructing the town Hellenic Ministry for upon the town / The the Environment, Μ.Katsaros 20% 2.1.2 periphery of Gorlitz - Physical Planning & 1996 60% S.Boutis 20% Zgorzelec", Public Works, Bundesrepublik EUROPAN Deutschland -Polska Participation Development Project Riken Conceptual Design Organising Yammamoto,Design Competition for the Committee of the 1999 2.1.3 7,5% Company ltd, Arata Olympic Village of Athens Athens 2004 2000 Isozaki and Olympics TM Associates & Field Shop, S.Boutis 2.5% Participation Architectural and Urban Design project for the The Municipal Reconstruction of 14 Development 2000 2.1.4 S.Boutis 25% building plots in the Enterprise of Ano 2001 Municipality of Ano Liosia Liosia Final Study Final Study for the The Municipal Reconstruction of the Development 2.1.5 2002 75% S.Boutis 25% Yannoulas Stream Enterprise of Ano Liosia Final Study Advanced Preliminary Study for the Municipality of Development of Platanos Akrata Municipal 2.1.6 2003 60% S.Boutis 40% Settlement, Municipality of Enterprise of Akrata, Ahaia Prefecture Tsivlos Preliminary Study Unification and Rejuvenation of Ioannina Municipality of 2.1.7 Town Centre Public 2004 65% S.Boutis 35% Ioannina Spaces Participation Development of Platanos Settlement, Municipality of Akrata, within the framework of the Pilot Mouzakitis Van Allen 2.1.8 Implementations action AHAIA SA 2004 30% Zervou 50% S.
    [Show full text]
  • Back Matter (PDF)
    Index Page numbers in italics refer to Figures. Page numbers in bold refer to Tables. accommodation zones 220 Basin and Range, rift displacement–strain rate 242 Aegean Sea 133 basin-bounding fault reactivation in Porcupine Basin rift displacement–strain rate 242 511, 512 Aegean tectonic domain 133 Beatrice Field see Inner Moray Firth Basin, fault study Aeges Formation 141 Benin Formation 170 Aegion Fault 134, 143, 148 Bergen Arcs Shear Zone 467, 469 Agbadi Formation 170 bimodal faults 20, 20 Aiges Formation 141, 142 Biscay, Bay of, Parentis Basin, extension and inversion Akata Formation 170 501–505 Alkyonides Gulf 133, 135 blind faults 189 Almannagja Fault Zone 51 Border Fault System 112, 113, 115 alternative (coherent) model 3 Bornholm, Robbedale Formation fault study 252–253, Amfithea Formation 141 254, 255, 265 analogue modelling boundary conditions, influence of 5 clay modelling, fault-segment boundary types boundary faults, Thailand 418–419 methods branch lines choice of materials 82–83 conservative fault junction 19 model analysis 83–85 defined 11 model design 83 geometry 11 results Gulf of Mexico, 3D mapping 13–14 structure and scaling 85–91 Gullfaks field 14–16 summary 92, 93, 94, 95, 96 mapping 11–13 temporal and spatial evolution 97–100 orientation 19–20, 20 results discussed relation to slip direction 20, 20 breached-segment boundary types 102–103 Troll Field 16–17 overlap and spacing 101–102 branch points 11 segment boundary evolution 100–101 Brazil see Santos Basin summary of results 103 breached segment boundary 80, 97, 102
    [Show full text]
  • Euscorpius — 2010, No
    172 Euscorpius — 2010, No. 95 Figure 242: Embryo of Iurus dufoureius, Kalivia Sohas, Mystras, Greece. Metasoma, ventral view, showing setae. Large view (top, 50x) and close-up of three setae (bottom, 200x). Kovařík, Fet, Soleglad & Yağmur: Iurus Revision 173 Figure 243: Embryo of Iurus dufoureius, Kalivia Sohas, Mystras, Greece. Telson, full lateral view on left (75x); aculeus view on top (150x); and close-up of setation on the vesicle (350x). 174 Euscorpius — 2010, No. 95 Figure 244: Embryo of Iurus dufoureius, Kalivia Sohas, Mystras, Greece. Bottom. Left chelal fixed finger showing socketed setae (100x). Top. Close-up of distal aspect of fixed finger showing socketed setae and three constellation array sensilla (350x). Kovařík, Fet, Soleglad & Yağmur: Iurus Revision 175 Figure 245: Embryo of Iurus dufoureius, Kalivia Sohas, Mystras, Greece. Top. Close-up of left chelal fixed finger showing socketed setae and constellation array (500x). Bottom. Close-up of right fixed finger showing five constellation array sensilla (750x). 176 Euscorpius — 2010, No. 95 Figure 246: Embryo of Iurus dufoureius, Kalivia Sohas, Mystras, Greece. Top. Right leg II showing socketed setae (200x). Bottom. Close-up of right leg II distal tip (350x). Kovařík, Fet, Soleglad & Yağmur: Iurus Revision 177 tolerate a large range of temperatures. In Anatolia, Iurus (1981) followed Vachon (1953) and Kinzelbach (1975) is “a strictly hygrophilic scorpion that lives in dense fir in attributing the distribution pattern of the genus Iurus and maple, forests and oak groves, where it is fairly to a vicariant process resulting from the recent tectonic common” (Crucitti, 1999a). One of the authors (EAY) events that occurred between the Turkish Plate and the observed and collected three Anatolian species of Iurus Anatolian Fault during the Quaternary period (1.8 Mya).
    [Show full text]