Jurassic Sedimentary Evolution and Nappe Emplacement in the Argolis Peninsula (Peloponnesus, Greece)
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Home > Sciences & Environment > Earth sciences > Geology, geomorphology and the lithosphere > Jurassic Sedimentary Evolution and Nappe Emplacement in the Argolis Peninsula (Peloponnesus, Greece)
Jurassic Sedimentary Evolution and Nappe Emplacement in the Argolis Peninsula (Peloponnesus, Greece)

Jurassic Sedimentary Evolution and Nappe Emplacement in the Argolis Peninsula (Peloponnesus, Greece)


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Die mesozoisch-tertiaren Serien der Argolis-Halbinsel sind In der externen Adhami-Basalsequenz wird die Radiolarit- in ein mehrphasiges Deckengebaude einbezogen, in dem sich Formation von Ophiolith fUhrenden lithischen Kalkareni- zwei tertiar-tektonische "Composite Units" und die Akros- ten und schliesslich von groben, mehrere 100 m machtigen Decke unterscheiden lassen. Beide "Composite Units" set- Hornstein-Kalk-Breccien iiberlagert (Kandhia Breccia). Die zen sich aus einer Basalsequenz und im Spat jura darauf Komponenten stammen hauptsachlich aus der tektonisch iiberschobenen Deckeneinheiten zusammen. Die Adhami- auflagernden Asklipion-Decke. Die Kandhia-Breccie er- "Composite Unit" als externe und die Dhidhimi-Trapezona brachte Radiolarienfaunen des Tithonian. "Composite Unit" als interne Einheit unterscheiden sich Die Asklipion-Decke umfasst eine Tiefwasserserie, begin- durch eine zeitlich und faziell verschiedene oberjurassische nend mit untertriadischen sauren Vulkaniten, gefolgt von klastische Faziesentwicklung in der Basalsequenz wie auch bis zu 1000 m machtigen Hornstein-Plattenkalken, die sich durch einen verschiedenen Gesteinsinhalt der iiberlagernden bis in den Lias fortsetzen. Diese Serie wird ebenfalls von, spat jurassischen Decken. Die Entwicklung von Plattform- hier mitteI- bis oberjurassischen Radiolariten (Koliaki zu peJagischer Sedimentation erfolgte in beiden Basal- Chert) und einer Ophiolith-Klasten fUhrenden, zunehmend sequenzen zunachst auf ahnliche Weise: Obertriadische bis grobkornigeren klastischen Serie iiberlagert. Die mittel-/ mittelliasische Flachwasserkalke (Pantokrator-Kalk) wer- obertriadischen Asklipion-Kalke treten als verkehrt liegende den im ganzen Gebiet von pelagischen Kalken iiberlagert.

Table of Contents:
Abstract.- Résumé.- Zusammenfassung.- A. Introduction.- 1 Geological Frame, Definition of Units and Main Results.- 1.1 Adhami Composite Unit.- 1.2 Dhidhimi — Trapezona Composite Unit.- 1.3 Akros Unit and Emplacement of Eocene Units.- 2 History of Research.- 3 Objectives of Study and Methods of Investigation.- Methods of Investigation.- B. Sedimentary Stratigraphy and Paleogeographic Evolution.- 1 Basal Sequences.- 1.1 From Shallow Water to Pelagic Sedimentation — Evolution of a Passive Continental Margin.- 1.1.1 Pantokrator Limestone — Late Triassic and Early Jurassic Shallow Water Limestones and Dolomites.- Name and Occurrence.- Lithology and Age.- Conclusive Remarks on the Facies Evolution of the Pantokrator Limestone.- 1.1.2 Pelagic Limestones and Rosso Ammonitico.- Sequence 1.- Sequence 2.- Sequence 3.- Sequence 4.- Paleogeographic Evolution.- 1.1.3 Ayios Nikolaos Chert.- 1.1.4 Angelokastron Chert.- 1.2 Classic Deposition and Formation of Olistostromes — Evolution of an Active Continental Margin.- 1.2.1 Kandhia Breccia.- Short Definition.- Type Section.- Composition and Lateral Variation.- Sedimentology.- Environment of Deposition.- Origin of Clasts.- 1.2.2 Dhimaina Formation.- Short Definition.- Previous Work.- Type Sections.- Dhimaina Formation Lower Member.- Sedimentology and Depositional Setting of the Lower Member.- Dhimaina Formation Upper Member.- Sedimentology and Depositional Setting of the Upper Member.- Lateral Variation.- 1.2.3 Potami Formation.- Short Definition.- Previous Work.- General Occurrence and Distinction from Other Formations.- Type Area.- Lithologies.- Age of the Potami Formation.- Origin of Clasts.- Mode of Debris Emplacement and Accumulation.- Contact with the Overlying Migdhalitsa Ophiolite Unit.- 2. Overlying Late Jurassic Nappes.- 2.1 Asklipion Unit.- 2.1.1 Theokafta Subunit.- Occurrence.- 2.1.1.1 Adhami Limestone.- 2.1.1.2 Koliali Chert.- Occurrence.- Lithology.- Age.- 2.1.1.3 Olistoliths of Anisian to Norian.- Asklipion Limestone.- Occurrence.- Bio- and Lithostratigraphy.- 2.1.1.4 Sedimentologic and Paleogeographic.- Conclusions on the Theokafta Subunit.- 2.1.2 Main Asklipion Unit.- Occurrence.- 2.1.2.1 Early to Middle Triassic Acidic.- Volcanics and Tuffs..- Occurrence.- Age…..- 2.1.2.2 Ayios Andreas Beds.- Occurrence.- Age.- Sedimentology.- 2.1.2.3 Adhami Limestone.- Occurrence.- Age.- Sedimentology.- 2.1.2.4 Transition to the Koliaki Chert.- Generalized Stratigraphy, Ages and Sedimentology.- Sedimentologic and Paleogeographic Interpretation.- 2.1.2.5 Koliaki Chert.- Occurrence.- Facies Development.- Age.- 2.1.2.6 Clastic Formations.- Facies Development.- Age.- 2.2 Ophiolites.- 2.2.1 Introduction.- 2.2.2 Occurrence of Ophiolite Lithogies in Several Structural Positions.- 2.2.3 Migdhalitsa Ophiolite Unit.- C. Petrography and Geochemistry of Ophiolites, Ophiolite Clasts and Triassic Volcanics.- 1. Petrographic Remarks on the Ophiolites.- 1.1 Mafic and Ultamafic Cumulates.- 1.1.1 Serpentinized Dunites and Harzburgites….- 1.1.2 Pyroxenites.- 1.1.3 Gabbros.- 1.1.4 Conclusive Remarks on the Cumulates.- 1.2 Mafic Volcanic Rocks.- 1.2.1 Dolerites.- 1.2.2 Basaltic (Pillow-) Lavas.- 2. Geochemistry of Ophiolites and Triassic Acidic Volcanics.- 2.1 Introduction.- 2.2 Methods of Analysis and Presentation of Data.- 2.3 Graphic Representation of Data and Discussion of Results.- 2.3.1 AFM and Ka-K-Ca Ternary Diagrams.- 2.3.2 Discriminant Analysis after Pearce (1976).- 2.3.3 Trace Elements: Ti-Cr and Ti-Zr Diagrams.- 3. Conclusions.- D. Chrome Spinel and Clay Mineralogy.- 1 Chrome Spinel Mineralogy.- 1.1 Introduction.- 1.2 Optical Indentification and Extraction from Clastic Rocks.- 1.3 X-Ray Energy-Dispersive Analysis.- Main Results.- Compositional Trends.- 1.4 Conclusions and Geological Significance.- 2 Clay Mineralogy.- 2.1 Introduction.- 2.2 Results.- 2.3 Conclusions and Geological Significance.- E. Conclusions.- 1 General Evolution, Palinspastic Position and Late Jurassic Emplacement of Units.- 1.1 Basal Sequences.- 1.2 Asklipion Unit.- 1.3 Migdhalitsa Ophiolite Unit.- F. Acknowledgments.- G. References.


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Product Details
  • ISBN-13: 9783764317195
  • Publisher: Birkhauser Verlag AG
  • Publisher Imprint: Birkhauser Verlag AG
  • Language: English
  • Returnable: Y
  • ISBN-10: 3764317191
  • Publisher Date: 01 Jan 1985
  • Binding: Hardback
  • No of Pages: 111
  • Weight: 890 gr


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