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What is VMS? Assemblages of mostly sulfide minerals that develop on the seafloor at locations of concentrated hydrothermal discharge, relates to a kind of ore deposit that’s mined from existing oceanic crust formed underwater are Volcanogenic Massive Sulfides (VMS) Deposit. ...
Geology 101 is the study of the Earth and its materials, structures, processes, and history. It is a broad field that encompasses many different disciplines, including mineralogy, petrology, paleontology, and geophysics. Geologists study the Earth’s physical features, including its rocks, ...
Metamorphic rocks are classified based on their texture, mineralogy, and composition. The facies classification of metamorphic rocks is based on the conditions of temperature and pressure under which the rock formed. The following are the facies classification of metamorphic rocks: ...
Skarn Deposits: Unraveling the Geological Marvel Skarn deposits, also known as skarns, represent a fascinating geological phenomenon formed through the interaction of hot fluids from intrusive igneous bodies with carbonate-rich sedimentary rocks. In this comprehensive guide, we’ll explore the various ...
Marine and petroleum geology is a field of study that focuses on the exploration and understanding of Earth’s subsurface, particularly in relation to the formation, accumulation, and extraction of petroleum resources in marine environments. This interdisciplinary field combines aspects of ...
Unveiling the Rich Tapestry of Iron Ore Hematite, a mineral of profound geological significance, stands as one of the most abundant and economically vital iron ores on Earth. Let’s delve into its intricacies, exploring both its physical and chemical properties. ...
An ophiolite is a section of oceanic crust and upper mantle that has been uplifted and exposed above sea level due to tectonic processes. Ophiolites are important geological features because they provide a window into the Earth’s interior and allow ...
BSc Geology, a captivating journey into the depths of our planet, opens a realm of exploration for those intrigued by Earth’s mysteries. This comprehensive program delves into diverse aspects of geosciences, offering a profound understanding of geological processes, mineralogy, and ...
Porosity Definition Porosity refers to the amount of empty space or voids within a material or substance. It is often expressed as a percentage of the total volume of the material, with the remaining percentage being occupied by the solid ...
What are Rare Earths? The Japanese call them “the seeds of technology.” The US Department of Energy calls them “technology metals.” They make possible the high tech world we live in today – everything from the miniaturization of electronics, to the enabling of ...
Unveiling the Mysteries of Igneous Rocks Introduction: Igneous rocks, born from the fiery depths of the Earth, hold a unique place in the geological tapestry. Formed through the solidification of molten magma or lava, these rocks play a pivotal role ...
Geology is the scientific study of the all constituents of planets, their internal and external forms and processes. More precisely, it is the study of nature, structure and history of the planet. Earth is the home to all life, well ...
The statement that oceanic crust cannot be older than 200 million years is based on the process of plate tectonics and the concept of seafloor spreading. Oceanic crust is continuously being created at mid-ocean ridges through volcanic activity, where magma rises to the surface, cools, and solidifiesRead more
The statement that oceanic crust cannot be older than 200 million years is based on the process of plate tectonics and the concept of seafloor spreading. Oceanic crust is continuously being created at mid-ocean ridges through volcanic activity, where magma rises to the surface, cools, and solidifies, forming new crust. As this process occurs, older crust is pushed away from the ridge and eventually subducted beneath continental plates or other oceanic crust in subduction zones.
Since the theory of plate tectonics suggests that the oldest oceanic crust is typically no more than around 200 million years old, this implies that older oceanic crust has been recycled back into the Earth’s mantle through subduction. This process effectively renews the oceanic crust, preventing it from accumulating to ages much older than 200 million years.
However, it’s important to note that there are exceptions to this general rule. Some fragments of ancient oceanic crust, known as ophiolites, can be found in certain geological settings, such as mountain belts, where they have been preserved and uplifted through tectonic processes. These ophiolites provide valuable insights into the history and evolution of oceanic crust, but they are relatively rare compared to the ongoing formation and recycling of younger oceanic crust at mid-ocean ridges and subduction zones.
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