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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, ...
In geology and mineralogy, crystal systems are a classification system used to categorize and describe the geometric shapes, or crystal forms, that minerals can take based on the internal arrangement of their atoms or ions. These crystal systems help scientists ...
A Comparison of Two Related Fields Geology and geography are two interconnected fields of study that focus on the Earth and its various features. While geology is concerned with the composition, structure, and processes of the Earth, geography is more ...
Introduction: Non-metallic miner als, also known as non-metals, are a diverse group of elements that do not possess metallic properties. They are soft, brittle, and generally have low melting and boiling points. Non-metallic minerals play a vital role in the ...
✳️Cinnabar is a toxic mercury sulfide mineral with a chemical composition of HgS. 🔷It is the only important ore of mercury. It has a bright red color that has caused people to use it as a pigment, and carve it ...
Coal, a fossil fuel formed over millions of years, holds a pivotal role in powering civilizations and shaping energy landscapes. This article explores the intricate details of coal, from its formation to the various types that fuel industries worldwide. Formation ...
What the meaning of Bauxite ? Bauxite is the most important aluminum ore. This type of rock consists mainly of the minerals gypsite Al(OH)3, bohemite γ-AlO(OH), anddiaspore α-AlO(OH) in a mixture that usually includes iron oxide goethite,hematite,the clay mineral kaolin, ...
In engineering and geology, a fault is a fracture or discontinuity in the Earth’s crust where movement or displacement has occurred. Types of faults Causes of Fault The causes of faults are diverse and depend on the type of fault. ...
What is Strike? The strike is the compass direction of a line marking the intersection of an inclined plane with a horizontal plane such as the Earth’s surface. Measuring Strike In order to measure the strike, place the side or ...
All of the important processes of metamorphism that we are familiar with can be directly related to geological processes caused by plate tectonics. The relationships between plate tectonics and metamorphism are summarized in Figure. Most regional metamorphism takes place within continental ...
Geological Time Scale The geological time scale is a system of chronological measurement that relates geological events and geological time to a numerical scale. It is used to describe the timing and relationships between events that have occurred throughout Earth’s ...
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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