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  • 1
    Keywords: Earth sciences. ; Sedimentology. ; Physical geography. ; Geology. ; Geochemistry. ; Engineering geology.
    Description / Table of Contents: Cosmogenic surface exposure dating applications from Turkey: moraines, alluvial fans, fluvial terraces, lava flows and incision rates -- Tectonic Geomorphology and Paleoseismology of the Muğla-Yatağan Fault (Southwest Turkey) -- Slip rate estimation of the North Anatolian Fault using geomorphology and paleoclimate chronology: The Ganos Fault, Turkey -- Energy relief analysis of the northern Marche-Romagna region, northern Apennine, central Italy -- Evaluation of Electromagnetic Induction method to map soil salinity in semi-arid Tunisia -- Comparison of organic carbon stock of Regosols under two different climates in Tunisia -- Evolution of organic carbon stocks in a Vertisol after three years of no-tillage practice in northern Tunisia -- Spectral characteristics of soil types in northwestern Jordan: consideration of iron oxides effects and colors -- Wind-eroded sediment in southern Hungary, with special reference to the content of toxic elements -- Time-Scale Variations of organic carbon in Paddy Soils: Sanjiang Plain, China.
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource(XXIX, 395 p. 259 illus., 226 illus. in color.)
    Edition: 1st ed. 2022.
    ISBN: 9783030725471
    Series Statement: Advances in Science, Technology & Innovation, IEREK Interdisciplinary Series for Sustainable Development
    Language: English
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  • 2
    Keywords: Earth sciences-Congresses. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (373 pages)
    Edition: 1st ed.
    ISBN: 9783030725471
    Series Statement: Advances in Science, Technology and Innovation Series
    DDC: 551
    Language: English
    Note: Intro -- About the 2nd Springer Conference of the Arabian Journal of Geosciences (CAJG-2), Tunisia 2019 -- Proceedings Volume 1: New Prospects in Environmental Geosciences and Hydrogeosciences -- Proceedings Volume 2: Advances in Geophysics, Tectonics and Petroleum Geosciences -- Proceedings Volume 3: Recent Research on Geomorphology, Sedimentology, and Geochemistry -- Proceedings Volume 4: Research developments in Geotechnics, Geo-Informatics and Remote Sensing -- About the Conference Steering Committee -- Preface -- Contents -- About the Editors -- Geomorphology, Soil Science, Landslides, Coastal Processes, and Geoarchaeology (T9): Geomorphology: Fault Slip and Incision Rates -- 1 Cosmogenic Surface Exposure Dating Applications from Turkey -- Moraines, Alluvial Fans, Fluvial Terraces, Lava Flows and Incision Rates -- Abstract -- 1 Introduction -- 2 Methods -- 3 Results -- 3.1 Glacial Deposits and Surfaces -- 3.2 Alluvial Fans, Landslides and Faults -- 3.3 Fluvial Terraces -- 3.4 Lava Flows -- 3.5 Erosion Rates -- 4 Conclusions -- References -- 2 Tectonic Geomorphology and Paleoseismology of the Muğla-Yatağan Fault (SW Turkey) -- Abstract -- 1 Introduction -- 2 Materials and Methods -- 3 Results -- 4 Conclusions -- References -- 3 Slip Rate Estimation on the North Anatolian Fault Using Geomorphology and Paleoclimate Chronology: The Ganos Fault, Turkey -- Abstract -- 1 Introduction -- 2 Geomorphological Setting and Drainage Development -- 3 Results -- 4 Conclusions -- References -- 4 Energy Relief Analysis of the Northern Marche-Romagna Region, Northern Apennine, Central Italy -- Abstract -- 1 Introduction -- 2 Study Area -- 3 Data and Method -- 4 Results -- 5 Discussion and Conclusions -- References -- Geomorphology, Soil Science, Landslides, Coastal Processes, and Geoarchaeology (T9): Soil Science. , 5 Evaluation of Electromagnetic Induction Method to Map Soil Salinity in Semiarid Tunisia -- Abstract -- 1 Introduction -- 2 Materials and Methods -- 3 Results -- 3.1 Soil Properties -- 3.2 Calibration of EM38 Readings -- 3.3 Spatial Variation of Soil Salinity -- 4 Discussion -- 5 Conclusions -- Acknowledgements -- References -- 6 Comparison of Organic Carbon Stock of Regosols Under Two Different Climates in Tunisia -- Abstract -- 1 Introduction -- 2 Materials and Methods -- 3 Results -- 3.1 Particle Size, Bulk Density, Organic Carbon, and pH of Both Soils -- 3.2 Soil Organic Carbon Stocks of Both Soils -- 4 Discussion -- 5 Conclusions -- References -- 7 Organic Carbon Stocks Evaluation After Three Years of No-Tillage Practice in a Vertisol, Northern Tunisia -- Abstract -- 1 Introduction -- 2 Materials and Methods -- 3 Results -- 4 Discussion -- 5 Conclusions -- References -- 8 Spectral Characteristics of Soil Types in Northwestern Jordan Considering Iron Oxides Effects and Colors -- Abstract -- 1 Introduction -- 2 Settings, Methods, and Materials -- 3 Results and Discussion -- 3.1 Soil Chemical and Color Properties -- 3.2 Spectral and Chemical Characteristic -- 3.3 Correlation of Soil Colors with Chemical and Spectral Parameters -- 4 Conclusion -- References -- 9 Examining Wind-Eroded Sediment Especially the Content of Toxic Elements, Southern Hungary -- Abstract -- 1 Introduction -- 2 Sample Area and Methods -- 3 Results and Discussion -- 4 Conclusions -- References -- 10 Time-Scale Variation of Organic Carbon in Paddy Soil in Sanjiang Plain, China -- Abstract -- 1 Introduction -- 2 Materials and Methods -- 2.1 Location of Sanjiang Plain -- 2.2 Test Soil and Sample Collection -- 2.3 Measurement Item and Method -- 3 Results and Discussion -- 3.1 Soil Carbon Variance Analysis -- 3.2 Soil Carbon-Level Regression Analysis. , 3.2.1 Relationship Between Organic Carbon of Different Soils and Rice-Cultivation Time -- 3.2.2 Effect of Rice-Cultivation Time on Carbon Content in Different Soil Components -- 4 Conclusions -- References -- Geomorphology, Soil Science, Landslides, Coastal Processes, and Geoarchaeology (T9): Landslides and Debris Flows -- 11 Stability Assessment of a Cliff and Hazard Characterization Methodology of the "Landslide": Application to Korbous Cliff (Cap-Bon, Tunisia) -- Abstract -- 1 Introduction -- 2 Materials and Methods -- 3 Results -- 3.1 Slope -- 3.2 Rainfall -- 4 Discussion -- 5 Conclusions -- References -- 12 Landslide Susceptibility Modeling Using GIS and MAUT Combined with Artificial Neural Network Models -- Case of Aghribs Watershed (Neogen Basin of Tizi-Ouzou, Algeria) -- Abstract -- 1 Introduction -- 2 Methodology -- 2.1 Location of the Study Area -- 2.2 Inventory Map -- 3 Results -- 3.1 Land Slide Risks Map Applying MAUT -- 3.2 ANN Results -- 3.3 Interpolation by Using Thiessen's Polygons -- 4 Discussion -- 5 Conclusion -- References -- 13 Landslide Distribution Analysis in the Foglia River Basin, Northern Apennines, Italy -- Abstract -- 1 Introduction -- 2 Materials and Methods -- 3 Results -- 3.1 Landslides and Lithology -- 3.2 Landslides and Land Use -- 3.3 Landslides and Slope -- 3.4 Landslides and Altitude -- 3.5 Landslides and Orientation of the Slope -- 4 Discussion and Concluding Remarks -- References -- 14 Spatial Distribution of Debris Flow-prone Catchments in Hengduan Mountainous Area in Southwestern China -- Abstract -- 1 Introduction -- 2 Study Area -- 3 Results -- 3.1 Spatial Distribution of Debris-Flow Catchments in Different Units -- 3.2 Distribution of Debris Flow Catchments with Annual Rainfall Results -- 4 Conclusions -- References. , Geomorphology, Soil Science, Landslides, Coastal Processes, and Geoarchaeology (T9): Coastal Processes -- 15 Evolution of Shoreline Kinematics at the Bejaia Bay (East Algeria) from 1989 to 2017 -- Abstract -- 1 Introduction -- 2 Study Area -- 3 Materials and Methods -- 4 Results -- 5 Discussion -- 6 Conclusions -- References -- 16 Impact of Beach Surface Moisture on Aeolian Sand Transport Rate and Vertical Mass Flux Distribution, the Case of Atlantic Coast, Southern Morocco -- Abstract -- 1 Introduction -- 2 Settings and Methods -- 3 Results and Discussion -- 4 Conclusions -- References -- 17 Relative Sea-Level Changes on the Southwestern Arabian Gulf since the Last Glacial Maximum -- Abstract -- 1 Introduction -- 2 Method and Material -- 3 Results -- 4 Discussion -- 5 Conclusions -- References -- 18 Shoreline Change Analysis Using Digital Shoreline Analysis System along Southeast Romanian Coast -- Abstract -- 1 Introduction -- 2 Materials and Methods -- 3 Results and Discussion -- 4 Conclusions -- Acknowledgements -- References -- 19 Lithogolical and Geochemical Analysis of Mainland and Spit Sandy Beach Sediments: SE Baltic Sea (Lithuania) -- Abstract -- 1 Introduction -- 2 Study Area and Methodology -- 3 Results -- 4 Discussion -- 5 Conclusions -- References -- 20 Modeling of Lithodynamic Processes in the Area of Sea Port (Russia) -- Abstract -- 1 Introduction -- 2 Materials and Methods -- 3 Results -- 4 Discussion -- 5 Conclusions -- References -- Geomorphology, Soil Science, Landslides, Coastal Processes, and Geoarchaeology (T9): Geoarchaeology and Geoheritage -- 21 Geophysical Investigations of the Bronze Age Archaeological Site in the Trans-Urals, Russia -- Abstract -- 1 Introduction -- 2 Survey Methodology and Initial Analysis of Measurements -- 3 Results of Geophysical Investigation -- 3.1 Results of Magnetic Survey. , 3.2 Results of GPR Survey -- 4 Conclusion -- Acknowledgements -- References -- 22 Reconstruction of Roman Aqueduct Route that Supplied the Ancient City of Tomis -- Abstract -- 1 Introduction -- 2 Materials and Methods. -- 3 Results and Discussion -- 4 Conclusions -- References -- 23 The Usefulness of Geomorphology for Finding the Landscapes Drawn by Leonardo Da Vinci in the Montefeltro Region (Central Italy) -- Abstract -- 1 Introduction -- 2 Methodology -- 3 Results -- 4 Discussion -- 5 Conclusions -- References -- 24 Landscape as a Cultural Resource: Science, Poetry, and Ancient Music for the Enhancement of the Marche Region, Central Italy -- Abstract -- 1 Introduction -- 2 Methods -- 3 Results and Discussion -- 4 Conclusions -- Reference -- Sedimentology, Stratigraphy, Paleontology, and Marine Geosciences (T14): Sedimentology-Environmental, Tectonic and Diagenetic Processses -- 25 Sedimentology and High-Frequency Cycles of the Upper Pleistocene of the Bizerte Coast (N-E Tunisia) -- Abstract -- 1 Introduction -- 2 Results -- 3 Discussion -- 4 Conclusion -- References -- 26 On the Presence of Halokinetic Sequences, from Latest Aptian to Late Albian, NW Salt Province of Tunisia -- Abstract -- 1 Introduction -- 2 Materials and Methods -- 3 Results -- 4 Conclusions -- References -- 27 Geological Processes Enhancing the Reservoir Quality of Aptian "Tight" Proven Reservoirs in Northwestern Tunisia -- Abstract -- 1 Introduction -- 2 Materials and Methods -- 3 Results -- 4 Discussion -- 5 Conclusions -- References -- 28 Petrophysics and Reservoir Properties of the Turonian-Coniacian Bireno and Douleb Carbonate Members in Northern-Central Tunisia -- Abstract -- 1 Introduction -- 2 Materials and Methods -- 3 Results and Discussion -- 3.1 The Turonian-Coniacian Sedimentological Characteristics -- 3.2 Petrophysical Properties. , 3.3 Diagenesis Influence on the Porosity.
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  • 3
    Keywords: Paleontology-Congresses. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (325 pages)
    Edition: 1st ed.
    ISBN: 9783030014520
    Series Statement: Advances in Science, Technology and Innovation Series
    Language: English
    Note: Intro -- Preface -- About the 1st Springer Conference of the Arabian Journal of Geosciences (CAJG-1), Tunisia 2018 -- About the Conference Steering Committee -- Contents -- About the Editors -- Keynote -- 1 Phanerozoic Global Sea-Level Changes: Evidences from Tunisia Illustrating how Eduard Suess' Concepts (Gondwana, Tethys, Eustasy) are Still Relevant -- Abstract -- 1 Why Tunisia Can Be Considered as Good Example Supporting Eduard Suess's Concepts? -- 2 Henceforth Tunisia Is a Key Part of the Northern Gondwana Supercontinent as Inferred from Paleontological New Finds -- 3 Tunisia Is Part of the Vanished Tethyan Ocean Which Presence Was Hypothesized by Eduard Suess in 1893 -- 4 Sea Level Changes as Recorded in the Ghadames Basin, the Saharan Platform and Atlas Tunisia  (Third Suess' Concept) -- 2 Facies Architecture in Carbonate Ramps: Learned Lessons from Jurassic Cases Studies in the Iberian Basin -- Abstract -- 1 Introduction -- 2 Case Studies -- 2.1 Upper Sinemurian Ramp -- 2.2 Bajocian Ramp -- 2.3 Upper Kimmeridgian Homoclinal Ramp -- 3 Learned Lessons -- References -- 3 An Early Anthropocene Analog: The Geomorphology and Hydrology of the Rio Bravo Watershed in the Belize Tropics -- Abstract -- 1 Introduction -- 2 Settings, Materials and Methods -- 3 Results -- 4 Discussion -- 5 Conclusion -- References -- Palaeontology-Systematics -- 4 Similarity Analysis of Ostracoda Faunas in West-Tethyan During the Upper Pliensbachian-Lower Toarcian -- Abstract -- 1 Introduction -- 2 Materials and Methods -- 3 Results and Discussion -- 4 Conclusions -- References -- 5 Cladistic approach for phylogenetic reconstruction testing the subfamily Reineckiinae (Saida, western Algeria) -- Abstract -- 1 Introduction -- 2 Materials and Methods -- 3 Results -- 4 Discussion -- 5 Conclusion -- References -- 6 Rudists in the Revised Bivalvia 'Treatise Online'. , Abstract -- 1 Introduction -- 2 Progress with Publication to Date -- 3 Future Publication Tasks -- References -- 7 Morphological variability of Polyconites hadriani (Hippuritida, Bivalvia) in the Aptian carbonate platforms of the western Maestrat Basin, eastern Iberia -- Abstract -- 1 Introduction -- 2 Materials and Methods -- 3 Results -- 4 Discussion -- References -- 8 Description of a New Genus of Radiolitidae (Bivalvia, Hippuritida) with Canals in the Calcitic Shell Layer -- Abstract -- 1 Introduction -- 2 Materials and Methods -- 3 Results -- 4 Discussion -- 5 Conclusion -- References -- 9 Similarities and Differences of Orbitoides & -- Omphalocyclus Microspheric Forms with Selected Examples from Northern Iraq and Turkey and Their New Morphometric Data -- Abstract -- 1 Introduction -- 2 Materials and Methods -- 3 Results -- 3.1 Comparison of Microspheric Forms of Orbitoides and Omphalocyclus -- 3.2 Morphometric Data on the Orbitoides Genus -- 4 Discussion -- 5 Conclusion -- References -- 10 Cretaceous Paleodictyon Trace Fossils: Evolutionary Mimicry Tactic Versus Burrowing: Examples from the Kurdistan Region, Northeastern Iraq -- Abstract -- 1 Introduction -- 2 Methodology and Materials -- 3 Results -- 3.1 Paleodictyons and Coral in the Same Basin -- 3.2 Corals in the Neo-Tethys (Present Western Zagros) -- 4 Discussion -- 5 Conclusion -- References -- 11 First Titanosauriform Teeth from the Early Cretaceous of Tunisia -- Abstract -- 1 Introduction -- 2 Geographical and Geological Settings -- 3 Materials and Institutional Abbreviations -- 4 Systematic Palaeontology -- 5 Discussion -- 6 Conclusion -- References -- 12 Mesopelagic Fish Size Reduction in Response to the Messinian Salinity Crisis -- Abstract -- 1 Introduction -- 2 Materials and Methods -- 3 Results -- 4 Discussion -- 5 Conclusion -- Acknowledgements -- References. , 13 Middle Miocene Giraffokeryx (Giraffidae) with Marks of Enamel Hypoplasia from Dhok Bun Amir Khatoon, Punjab, Pakistan -- Abstract -- 1 Introduction -- 2 Materials and Methods -- 3 Systematic Palaeontology -- 3.1 Description -- 3.2 Comparison -- 4 Discussion -- 5 Conclusion -- References -- 14 Dental Morphology and Palaeoecological Implications of Brachypotherium (Rhinocerotidae) of the Middle Miocene Siwaliks (Pakistan) -- Abstract -- 1 Introduction -- 2 Materials and Methods -- 3 Results -- 4 Discussion -- 4.1 Comparison with Reported Literature -- 4.2 Palaeoecological Implication -- 5 Conclusion -- References -- 15 Systematic Study of the New Remains of Propotamochoerus Hysundricus (Suidae, Mammalia) from the Late Miocene-Early Pliocene Middle Siwaliks (Pakistan) -- Abstract -- 1 Introduction -- 2 Materials and Methods -- 3 Results -- 3.1 Upper Dentition -- 3.2 Lower Dentition -- 4 Discussion -- 5 Conclusion -- References -- 16 Systematics and Palaeo-Environmental Implications of Hexaprotodon Sivalensis (Hippopotamidae, Mammalia) from the Plio-Pleistocene Upper Siwaliks (Pakistan) -- Abstract -- 1 Introduction -- 2 Materials and Methods -- 3 Results -- 4 Discussion -- 4.1 Comparison with the Reported Literature -- 4.2 Palaeo-Environmental Implications -- 5 Conclusion -- References -- Biostratigraphy -- 17 Bajocian Ostracods from the Krachoua Formation (Beni Kheddache, Southern Tunisia): Implications for Biostratigraphy and Paleoecology -- Abstract -- 1 Introduction -- 2 Materials and Methods -- 3 Results -- 3.1 Stratigraphical Implication -- 3.2 Paleoecologic Implication -- 4 Discussion -- 5 Conclusion -- References -- 18 Paleobathymetric Influence on the Distribution of Ammonite and Foraminifer Settlements in the Callovian of the Saïda Region (Western Algeria) -- Abstract -- 1 Introduction -- 2 Materials and Methods -- 3 Results -- 4 Discussion. , 5 Conclusion -- References -- 19 First Calpionellid Biozonation of the Berriasian Reference Section of Jebel Ben Younes (Gafsa Basin, South Central Tunisia): Updated Age Attribution and Geodynamic Consequences -- Abstract -- 1 Introduction -- 2 Settings -- 3 Materials and Methods -- 4 Results: Calpionellid Biozonation and Age of the Study Sections -- 5 Discussion -- 6 Conclusion -- References -- 20 Berriasian Ammonite and Calpionellid Associations from the North-South Range of Central Tunisia: Updated Biozonation, Regional Geodynamic Context and Paleobiogeography -- Abstract -- 1 Introduction -- 2 Methods and Materials -- 3 Results and Discussion -- 3.1 Biozonations -- 3.2 Regional Correlations and Geodynamic Context -- 3.3 Paleobiogeography -- 3.4 Discussion -- 4 Conclusion -- References -- 21 Barremian-Albian (Lower Cretaceous) Rudist Chronostratigraphy, Caribbean Province North America -- Abstract -- 1 Introduction -- 2 Methods -- 3 Results -- 4 Conclusion -- References -- 22 Mid-Cretaceous Rudist Assemblage from the Lhasa Block, Tibet (China) -- Abstract -- 1 Introduction -- 2 Geological Setting -- 3 Results -- 4 Discussion -- 5 Conclusion -- References -- 23 Tethyan Non-rudist Associations from the Cretaceous Rudist Formations in Northern Egypt -- Abstract -- 1 Introduction -- 2 Materials and Methods -- 3 Results -- 4 Discussion -- 5 Conclusion -- References -- 24 New Biostratigraphic Scheme from the Cenomanian-Turonian of South Algeria -- Abstract -- 1 Introduction -- 2 Biostratigraphic Scheme -- 2.1 Zone C1-Neolobites vibrayeanus Total-Range Zone -- 2.2 Zone C2-Nigericeras gadeni Interval Zone -- 2.3 Zone C3-Vascoceras cauvini Interval Zone -- 2.4 Zone T1-Pseudotissotia nigeriensis-Choffaticeras sinaiticum Interval Zone -- 3 Cenomanian-Turonian Boundary -- References. , 25 Ostracods of the Cenomanian-Turonian Transition (Whiteinella archaeocretacea Zone) in the Ksour and Amour Mountains (Saharan Atlas, Algeria): Paleobiogeographic Implication -- Abstract -- 1 Introduction -- 2 Materials and Methods -- 3 Results and Discussion -- 3.1 Ostracod Distribution in the Study Basins -- 3.2 Qualitative Comparison of the Taxonomic Composition Between Basins -- 4 Conclusion -- References -- 26 Cenomanian Foraminiferal Biostratigraphy of the Aures Basin (Northeastern Algeria) -- Abstract -- 1 Introduction -- 2 Geographical and Geological Settings -- 3 Methodology -- 4 Results and Discussion -- 5 Conclusion -- References -- 27 An Integrated Biostratigraphy of the Cenomanian-Turonian Transition at Kasserine Area in Central Tunisia: Implication from Khanguet Esslougui Section -- Abstract -- 1 Introduction -- 2 Materials and Methods -- 3 Results -- 4 Discussion -- 5 Conclusion -- References -- 28 Micropaleontological Study of the Contact Between Kometan and Shiranish Formations from Dokan Area, Northern Iraq -- Abstract -- 1 Introduction -- 2 Materials and Methods -- 3 Results -- 4 Conclusion -- References -- 29 Planktonic Foraminiferal Evidence of Upper Cretaceous in the Well "A" (Gulf of Hammamet Area, Northeastern Offshore Tunisia) -- Abstract -- 1 Introduction -- 2 Materials and Methods -- 3 Results -- 4 Discussion -- 5 Conclusion -- References -- 30 Paleocene Benthic Foraminifera and Neoeponides duwi Event from Dineigil Area, South-Western Desert, Egypt -- Abstract -- 1 Introduction -- 2 Geological Setting, Lithology, Studied Section, and Methods -- 3 Results -- 4 Discussion -- 4.1 Southern Tethyan Neoeponides duwi Bio-Event -- 4.2 Paleoenvironmnets -- 5 Conclusion -- Acknowledgements -- References -- 31 Upper Eocene (Priabonian) Larger Foraminifera from the Deh-Rashti Section, Rafsanjan City, Southeastern Iran -- Abstract. , 1 Introduction.
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  • 4
    Keywords: Paleontology  ; Paleoecology ; Geology ; Geology ; Paleontology  ; Paleoecology ; Geomorphology. ; Physical geography. ; Konferenzschrift Conference of the Arabian Journal of Geosciences (1. : 2018: Hammamet) 12.11.-15.11.2018 ; Arabische Staaten ; Iberische Halbinsel ; Paläontologie ; Paläontologie ; Fossil ; Kongress ; Mittelmeerraum ; Nordafrika ; Tethysmeer ; Historische Geologie ; Sedimentologie ; Tektonik ; Fossil ; Biodiversität
    Description / Table of Contents: This edited volume contains the best papers accepted for presentation during the 1st Springer Conference of the Arabian Journal of Geosciences (CAJG-1), Tunisia 2018. The volume shares the latest results from paleontological, biostratigraphic and sedimentological studies by experienced researchers mainly from research institutes in the Mediterranean and Middle East. Main topics include: paleontology, biostratigraphy, sedimentology, paleoclimatology and geomorphology. Some new insights are given on paleobiodiversity and major biological tools for biostratigraphy, patterns, mechanisms and processes of meso-cenozoic sedimentation in the Mediterranean and Middle East. In particular, case studies are included to highlight the major controlling factors of Tethyan biosphere-geosphere interactions as inferred from the Mediterranean and Middle East regions. The book is of interest to all researchers in the fields of different disciplines involved in the sedimentary geology
    Type of Medium: Online Resource
    Pages: Online-Ressource (XXXI, 358 p. 165 illus., 137 illus. in color, online resource)
    Edition: Springer eBook Collection. Earth and Environmental Science
    ISBN: 9783030014520 , 9783030014520
    Series Statement: Advances in Science, Technology & Innovation, IEREK Interdisciplinary Series for Sustainable Development
    Language: English
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  • 5
    Electronic Resource
    Electronic Resource
    Springer
    International journal of earth sciences 76 (1987), S. 677-697 
    ISSN: 1437-3262
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Description / Table of Contents: Abstract The sedimentary evolution of the North Peruvian margin during upper Cretaceous can be summarized as follows: The upper Aptian transgression involved the whole margin, and was accompanied by minor, local, synsedimentary tectonic features. It could be coeval with the individualization of the Western ensialic marginal basin. The transgression reached its maximum during middle Albian, and is associated with anoxic deposits, and with the main activity of the marginal basin. A regression followed during the upper Albian. It was materialized during lower Cenomanian by intertidal deposits, by a westward deltaic progradation, and by synsedimentary tectonic features. This regressive maximum is correlatable with the tectonic closure and folding of the western marginal basin. Then, the great upper Cretaceous transgression affected the eastern parts of the margin. Major deepening stages occured during late Middle Cenomanian and at the base of the Turonian. During Turonian, a widespread, calm carbonate shelf developed. A new major transgressive pulse occured at the Turonian-Coniacian boundary. As a result of a general uplift, the whole margin emerged diachronically between Santonian and Campanian, leading to the deposition of continental Red Beds. The latter recorded a new tectonic phase of uppermost Senonian age. During upper Cretaceous times, the sedimentary evolution of the North Peruvian margin appears to be controlled both by the eustatic sea-level changes, and by the uppermost Albian to early Cenomanian, and the upper Senonian tectonic events.
    Abstract: Résumé L'évolution sédimentaire de la marge nord-péruvienne au Crétacé supérieur peut être résumée ainsi: La transgression de l'Aptien supérieur affecte toute la marge, et s'accompagne d'une légère instabilité tectonique localisée. Celle-ci peut être contemporaine de l'individualisation du bassin marginal occidental. La transgression atteint son maximum à l'Albien moyen. Elle est contemporaine de dépôts anoxiques et de l'activité du bassin marginal. Une régression survient au cours de l'Albien supérieur. Elle se matérialise au Cénomanien inférieur par l'installation d'une plate-forme carbonatée, puis par la progradation du delta oriental et par des mouvements tectoniques synsédimentaires. Cette régression est en relation avec la fermeture du bassin marginal occidental. La grande transgression du Crétacé supérieur affecte ensuite les zones orientales de la marge, les étapes majeures d'approfondissement se situant à la fin du Cénomanien moyen et à la base du Turonien. Au Turonien, une vaste plate-forme carbonatée s'installe, et un nouvel approfondissement survient à la limite Turonien-Coniacien. A la suite d'une surrection générale, la marge émerge de façon diachrone entre le Santonien et le Campanien, donnant lieu au dépôt des Couches Rouges continentales qui enregistrent au Sénonien terminal un nouvel événement tectonique. Au Crétacé supérieur, l'evolution sédimentaire de la marge nord-péruvienne semble donc contrôlée à la fois par les variations eustatiques, et par les événements tectoniques de l'Albien terminal-Cénomanien inférieur, et du Sénonien.
    Notes: Zusammenfassung Die sedimentäre Entwicklung des nordperuanischen Kontinentalrandes zeigt während der Ober-Kreide folgende Etappen: die Transgression des Oberaptes erstreckt sich über den gesamten Kontinentalrand und geht mit leichten synsedimentären tektonischen Diskonformitäten einher, die gleichzeitig mit der Entstehung des westlichen Randbeckens zu sehen sind. Die Transgression erreicht ihren Höhepunkt im mittleren Alb, sie ist verbunden mit anoxischen Ablagerungen und mit den Hauptbewegungen im randlichen Becken. Im Oberalb folgt eine Regression. Sie zeigt sich im unteren Cenoman durch intertidale Ablagerungen, durch nach Westen progradierende Deltas und durch synsedimentäre Tektonik. Der Höhepunkt der Regression ist verbunden mit der tektonischen Isolation und Faltung des westlichen Randbeckens. Die große Transgression während der Oberkreide beeinflußt vor allen Dingen die östlichen Teile des Randes. Wesentliche Eintiefungsphasen erscheinen im oberen Mittelcenoman und an der Basis des Turons. Während des Turons entwickelt sich ein weiter Karbonatschelf. Ein größerer Transgressionsvorstoß erscheint an der Grenze von Turon zu Coniac. Als Ergebnis einer generellen Heraushebung wird der gesamte Kontinentrand diachron zwischen Santon und Campan herausgehoben und es entstehen kontinentale Rotablagerungen. Diese Sedimente dokumentieren eine neue tektonische Phase im obersten Senon. Während der Oberkreide wird die sedimentäre Weiterentwicklung des nordperuanischen Kontinentalrandes durch globale Meeresspiegelschwankungen zusammen mit tektonischen Ereignissen (Oberapt, Oberalb-unteres Cenoman, Senon und oberstes Senon) kontrolliert.
    Type of Medium: Electronic Resource
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