Sign up to join our community!
Lost your password? Please enter your email address. You will receive a link and will create a new password via email.
You must login to ask a question.
Porphyry copper deposits are among the most significant sources of copper globally, accounting for over 60% of the world’s copper production . 1. Geological Overview a) Geological Background Porphyry copper deposits are typically associated with magmatic arcs related to subduction zones, where an oceanic plate subducts beneath a continental or another oceanic plate. This tectonic […]Table of Contents Toggle 1. Geological Overviewa) Geological Background
Introduction Ore-bearing hydrothermal fluids are one of the most important agents in the formation of mineral deposits. These fluids, which originate from various geological processes, have the ability to dissolve, transport, and deposit metals in economic concentrations. The study of hydrothermal fluids is crucial for understanding ore genesis and guiding mineral exploration. This article provides […]Table of Contents Toggle Introduction1. Sources of Hydrothermal Fluids
Gold has been one of the most sought-after minerals for centuries due to its value and rarity. Prospectors, geologists, and even hobbyists often search for gold-bearing rocks in the field. But how do you identify rocks that contain gold? This guide will provide an in-depth look at the geological features, rock types, and mineral indicators […]Table of Contents Toggle 1. Understanding the Geological Settings of Gold
Introduction Alteration in geology refers to mineralogical, textural, and chemical changes in rocks due to interactions with fluids, temperature variations, and pressure changes. This process occurs in diverse geological settings, including hydrothermal systems, weathering environments, and metamorphic terrains. Understanding alteration is essential in mineral exploration, petrology, geotechnical engineering, and environmental studies. This article explores the […]Table of Contents Toggle IntroductionTypes and Processes of Alteration
Introduction The Induced Polarization (IP) method is one of the most effective geophysical techniques used in the exploration of sulfide ore deposits. This method is particularly useful for identifying disseminated sulfide minerals, which are commonly associated with copper (Cu), gold (Au), silver (Ag), zinc (Zn), and lead (Pb) deposits. This article provides a detailed overview […]Table of Contents Toggle Introduction1. Understanding the Induced Polarization ...
Introduction Gold exploration is a complex process that requires a combination of geological knowledge, geochemistry, and geophysical techniques. One of the most effective methods for locating gold deposits is the identification of pathfinder elements and minerals. Pathfinder elements and minerals are geochemical indicators that suggest the presence of gold nearby, even if the gold itself […]Table of Contents Toggle IntroductionWhat Are Pathfinders for Gold Deposits?
Introduction Structural control is one of the most significant factors influencing the formation and distribution of hydrothermal gold deposits. Structural geology determines the pathways for mineralizing fluids, the locations of ore deposition, and the overall geometry of gold-bearing zones. Understanding these structural controls is essential for exploration geologists seeking new gold deposits and for mining […]Table of Contents Toggle IntroductionStructural Controls in Hydrothermal Gold Deposits
Introduction to Geology Geology, derived from the Greek words geo (Earth) and logos (study), is the scientific discipline dedicated to understanding the Earth’s composition, structure, processes, and history. It seeks to answer fundamental questions: How did mountains form? Why do volcanoes erupt? What clues do rocks hold about ancient life? From the atomic structure of […]Table of Contents Toggle Introduction to Geology
Engineering geological tests are critical for assessing the physical, mechanical, and chemical properties of rocks and soils to ensure safe and cost-effective design of infrastructure (e.g., dams, tunnels, foundations). These tests help determine material strength, stability, permeability, and susceptibility to hazards like landslides or subsidence. Below are key tests categorized by their application: 1. Field […]Table of Contents Toggle 1. Field Tests (In-Situ)2. Laboratory Tests
Sand Dune Landform: Formation, Types, and Significance Sand dunes are dynamic landforms created by the interaction of wind, sand, and vegetation. These striking natural features are common in deserts, coastal regions, and even in some semi-arid and arid zones. This article explores every aspect of sand dunes, including their formation, types, ecological significance, and role […]Table of Contents Toggle Sand Dune Landform: Formation, Types, and Significance
⚒️🔥 Volcanic materials 🔥⚒️ When volcanoes erupt, solid rock debris, molten materials (magma) and gases come out. ♦️️ rock debris: As a result of volcanic eruptions, solid rock debris of various types and sizes usually emerges in the initial period of a volcanic eruption. The rock debris is derived fRead more
⚒️🔥 Volcanic materials 🔥⚒️
When volcanoes erupt, solid rock debris, molten materials (magma) and gases come out.
♦️️ rock debris:
As a result of volcanic eruptions, solid rock debris of various types and sizes usually emerges in the initial period of a volcanic eruption. The rock debris is derived from the hardened crust that is extracted from the walls of the neck as a result of the strong and violent push of lava and gaseous materials emanating from magma. Rock debris is composed of materials of different sizes, including rock blocks, shells and embers, sand and volcanic dust.
♦️️ Gases:
Water vapor gases emerge from volcanoes during their activity, and it emanates in great quantities, forming huge clouds in which dust and other gases mix with it. These vapors condense, causing heavy rains to fall in the vicinity of the volcano. The explosions and rain are accompanied by the occurrence of electric lights that arise from the friction of volcanic ash granules with each other and as a result of air disturbances, except for the extremely hot water fumes, the volcano emits multiple gases, the most important of which are hydrogen, chlorine, sulfur compounds, nitrogen compounds, carbon compounds and oxygen.
♦️️ Lava:
They are liquid masses ejected by volcanoes, with a temperature between 800°C and 1200°C. The lava emanates from the crater of the volcano, as well as through the cracks and fractures in the sides of the volcanic cone, those fractures that are created by the explosions and the pressure of the magma masses.
Light lava:
This is characterized by the bone of its viscosity, and therefore it is slow flowing, like the lava that emanated from the Pelly volcano (in the Martinique Islands in the Caribbean) in 1902. It was so thick and sticky that it was unable to move, and it began to accumulate and rise, forming a tower above the crater, with a height of about 300 meters. Then, soon after that, it was broken and shattered as a result of the explosions caused by the exit of gases.
⚒ Dark heavy lava:
It is basaltic lava, and it is characterized by being highly liquid and mobile, and it flows in the form of streams on the slopes of the volcano, and when this lava emerges through large fractures, it spreads over huge areas forming spacious plateaus, such as the Abyssinian Plateau and the Deccan Plateau in India and the Columbia Plateau in North America.
🔥️ Volcanic materials
🔹️Volcanic Solids:
The parts that make up volcanic rocks are:
⚒Volcanic ejecta:
It is a frozen magma and lava ejected to the surface.
⚒ Pumice rock:
It is a silicate foam that is evaporated by gases.
⚒Volcanic ash:
It results from the fragmentation and scattering of the frozen magma summit in the neck of the volcano under the influence of pressure and steam, and it hardens quickly.
🔹️Liquid volcanic materials magma and lava (lava):
It consists of liquid materials from the lava that flows burning from the crater to great distances sometimes, and the extent of lava liquidity is subject to several factors. Such as the slope of the earth, the nature of magma and lava (viscous or fluid) and the viscosity ratio depends on the percentage of silica, and on the strength of the volcano
Gaseous volcanic materials:
See lessAmong the most important gases emitted from volcanoes are:
⚒ water vapor
⚒ Hydrocarbon compounds
⚒ sulfur dioxide