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|2 23
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|a Tectonic and structural framework of the Zagros fold-thrust belt /
|c edited by Ali Farzipour Saein
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| 264 |
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1 |
|a Amsterdam, Netherlands :
|b Elsevier,
|c 2019.
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| 300 |
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|a 1 online resource
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| 336 |
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|a text
|b txt
|2 rdacontent
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| 337 |
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|a computer
|b c
|2 rdamedia
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| 338 |
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|a online resource
|b cr
|2 rdacarrier
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| 490 |
1 |
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|a Developments in structural geology and tectonics ;
|v volume 3
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| 500 |
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|a Includes indexes.
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|a Online resource; title from PDF title page (ScienceDirect, viewed December 17, 2018).
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|a Front Cover; TECTONIC AND STRUCTURAL FRAMEWORK OF THE ZAGROS FOLD-THRUST BELT; About the Series; TECTONIC AND STRUCTURAL FRAMEWORK OF THE ZAGROS FOLD-THRUST BELT; Copyright; Dedication; Contents; Contributors; Preface; Acknowledgments; 1 -- Fracture Analysis of Hydrocarbon Reservoirs by Static and Dynamic Well Data, Case Study: The Aghajari Oil Field ... ; INTRODUCTION; GEOLOGIC FRAMEWORK; METHODOLOGY; Characterization; Modeling and Calibration; Upscaling; RESULTS AND DISCUSSION; CONCLUSIONS; Acknowledgments; References
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|a 2 -- Tectono-Sedimentary Evolution of the Iranian Zagros in a Global Context and Its Impact on Petroleum HabitatsINTRODUCTION; EVOLUTION OF THE IRANIAN ZAGROS; Observations of Zagros Main Events in Global Tectonic Evolution Framework; Discussions; CONCLUSIONS; Acknowledgments; References; 3 -- Zagros Foreland Fold Belt Timing Across Lurestan to Constrain Arabia-Iran Collision; INTRODUCTION; STRUCTURE AND STRATIGRAPHY OF THE LURESTAN PROVINCE: FORELAND SUCCESSIONS; AFRINEH AND CHAMAN GOLI GROWTH SYNCLINES; The Afrineh Growth Syncline; The Chaman Goli Growth Syncline; MAGNETOSTRATIGRAPHY
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|a Sampling StrategyPaleomagnetic Analysis; CORRELATION OF LOCAL MAGNETIC POLARITY STRATIGRAPHY WITH GLOBAL POLARITY TIME SCALES; Correlation of Afrineh Local Magnetic Polarity Stratigraphy With Geomagnetic Polarity Time Scale; Correlation of Chaman Goli Local Magnetic Polarity Stratigraphy With Geomagnetic Polarity Time Scale; DISCUSSION; Regional Time Transgressive Formation Boundaries of Zagros Foreland Basin Stratigraphy During the Neogene; Age of Growth Synclines and Sequence of Folding Propagation; Age of Folding to Constrain the Timing of the Zagros Continental Collision; CONCLUSIONS
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|a AcknowledgmentsReferences; 4 -- Structural Geology and Neotectonics of Iraq, Northwest Zagros; INTRODUCTION; SHALAIR TERRANE; OUTER ARABIAN PLATFORM; Zagros Fold-Thrust Belt; Zones of Zagros Fold-Thrust Belt; Suture or Thrust Zone; Imbricate Zone; High Folded Zone; Low Folded Zone; Basement Blocks of Zagros Fold-Thrust Belt of Iraq; MOSUL FAULT; Greater Zab Fault; General Description of Folds and Faults in the Zagros Fold-Thrust Belt; Crustal Structure of Zagros Fold-Thrust Belt; Stress Analyses of Zagros Fold-Thrust Belt; Seismicity of Zagros Fold-Thrust Belt; Mesopotamia Foredeep
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| 505 |
8 |
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|a Al-Jazira PlainThe East Northeast-West Southwest Fault System; Tel-Hajar Structures; Khleissia Graben; Tayarat North and South Grabens; Anah Graben; The Northwest-Southeast Fault System; Mesopotamia Plain; Folds, Faults, and Salt Structures of the Mesopotamia Plain; Folds; Faults; Neotectonics of Mesopotamia Plain; INNER ARABIAN PLATFORM; CONCLUSION; References; Further Reading; 5 -- High-Pressure/Low-Temperature Blueschists in the Zagros Mountains; INTRODUCTION; Windows in the Hajiabad Area of the Sanandaj-Sirjan Zone; HAJIABAD BLUESCHISTS; The Makran; NEO-TETHYIAN OPHIOLITES
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| 504 |
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|a Includes bibliographical references and index.
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| 650 |
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0 |
|a Geology, Structural
|z Zagros Mountains (Iran and Iraq)
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| 650 |
|
7 |
|a SCIENCE
|x Earth Sciences
|x Geography.
|2 bisacsh
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| 650 |
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7 |
|a SCIENCE
|x Earth Sciences
|x Geology.
|2 bisacsh
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| 650 |
|
7 |
|a Geology, Structural
|2 fast
|0 (OCoLC)fst00940775
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| 651 |
|
7 |
|a Middle East
|z Zagros Mountains
|2 fast
|0 (OCoLC)fst01731544
|
| 700 |
1 |
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|a Saein, Ali Farzipour,
|e editor.
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| 776 |
0 |
8 |
|i Print version :
|z 9780128150481
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| 830 |
|
0 |
|a Developments in structural geology and tectonics ;
|v v. 3.
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| 856 |
4 |
0 |
|u https://sciencedirect.uam.elogim.com/science/bookseries/25429000/3
|z Texto completo
|
