Tectonic and Structural Framework of the Zagros Fold-Thrust Belt

The book "Tectonic and Structural Framework of the Zagros Fold–Thrust Belt" is a comprehensive resource that covers the latest research and developments in the unique tectonic and structural geology of the Zagros. It is a valuable reference for oil companies, structural geologists, and students interested in the region's potential hydrocarbon resources.

Format: Paperback / softback
Length: 310 pages
Publication date: 05 December 2018
Publisher: Elsevier Science Publishing Co Inc

The latest volume in the Developments in Structural Geology and Tectonics series from Elsevier, Tectonic and Structural Framework of the Zagros Fold–Thrust Belt, is a comprehensive collection of the most recent research and developments in the unique tectonic and structural geology of the Zagros. Renowned among geologists, the Zagros fold–thrust belt is one of the most extensively studied terrains globally. Due to its distinctive structures, the Zagros orogeny poses significant challenges for researchers and experts. This book serves as an indispensable reference, compiling the latest data and thoroughly exploring this facet. Furthermore, as the Zagros range holds potential for hydrocarbons, it holds immense interest for petroleum geologists and exploration companies worldwide. This book is a vital, cutting-edge resource for oil companies, structural geologists, and students at both undergraduate and postgraduate levels.

The Zagros fold–thrust belt, located in the western part of the Iranian Plateau, is a complex geological region characterized by intricate folding and thrusting of rocks. It is one of the most seismically active areas in the world, with frequent earthquakes and volcanic eruptions. The belt is home to a diverse range of geological features, including mountains, valleys, and plateaus, and is known for its rich mineral resources, including copper, gold, and oil.

The tectonic and structural framework of the Zagros fold–thrust belt is a subject of ongoing research and exploration. The region is believed to have undergone significant deformation and metamorphism during the Mesozoic and Cenozoic periods, resulting in the formation of complex geological structures. The study of the Zagros fold–thrust belt has important implications for understanding the tectonic evolution of the Iranian Plateau and the broader region.

One of the key challenges in studying the Zagros fold–thrust belt is the complex topography and geology of the region. The mountains and valleys of the belt are steep and rugged, making it difficult to access and study the underlying rocks. Additionally, the region is prone to natural disasters such as earthquakes, landslides, and volcanic eruptions, which can further complicate the research process.

Despite these challenges, there have been significant advancements in our understanding of the Zagros fold–thrust belt in recent years. Researchers have used a range of techniques, including satellite imagery, geophysical surveys, and drilling, to study the region's geology and tectonic structures. These techniques have helped to reveal the complex deformation patterns and the distribution of mineral resources in the belt.

One of the most important findings of recent research is the role of the Zagros Mountains in the formation of the Zagros fold–thrust belt. The mountains are believed to have formed as a result of the collision of the Arabian Plate with the Eurasian Plate, which caused the uplift and deformation of the Iranian Plateau. The collision also resulted in the formation of the Zagros orogeny, a series of mountain ranges that stretch across the entire length of the Iranian Plateau.

The Zagros orogeny is characterized by a complex series of folds and thrusts that have created a series of mountain ranges and plateaus. The highest peak in the belt, Mount Dena, is located in the Zagros Mountains and reaches an elevation of over 4,600 meters. The mountains are also home to a number of important geological structures, including the Qomolangma-Damavand Fault, which is one of the world's largest fault systems.

The Qomolangma-Damavand Fault is a major tectonic boundary that separates the Arabian Plate from the Eurasian Plate. It is responsible for the frequent earthquakes and volcanic eruptions that occur in the Zagros fold–thrust belt. The fault is also a potential source of hydrocarbons, as it has been shown to contain oil and gas reserves.

In addition to the Zagros Mountains, the Zagros fold–thrust belt is also home to a number of other important geological features, including the Qomolangma-Damavand Basin, which is one of the largest sedimentary basins in the world. The basin is believed to have formed as a result of the uplift and deformation of the Iranian Plateau and is home to a rich variety of fossil fuels, including oil and gas.

The study of the Zagros fold–thrust belt has important implications for understanding the tectonic evolution of the Iranian Plateau and the broader region. The region is believed to have played a critical role in the formation of the Arabian Plate and the Eurasian Plate, and its complex geological structures have helped to shape the landscape of the region. The study of the Zagros fold–thrust belt also has important implications for oil and gas exploration and development in the region.

In conclusion, the Zagros fold–thrust belt is a complex and fascinating geological region that is home to a rich variety of geological features and mineral resources. The tectonic and structural framework of the belt is a subject of ongoing research and exploration, and there have been significant advancements in our understanding of the region in recent years. The Zagros Mountains are believed to have formed as a result of the collision of the Arabian Plate with the Eurasian Plate, and the Qomolangma-Damavand Fault is a major tectonic boundary that separates the two plates. The Zagros fold–thrust belt is also home to the Qomolangma-Damavand Basin, one of the largest sedimentary basins in the world, which is believed to have formed as a result of the uplift and deformation of the Iranian Plateau. The study of the Zagros fold–thrust belt has important implications for understanding the tectonic evolution of the Iranian Plateau and the broader region, and it also has important implications for oil and gas exploration and development in the region.

Weight: 824g
Dimension: 216 x 276 x 21 (mm)
ISBN-13: 9780128150481