Table of Contents
- 1 How is a hydrothermal form?
- 2 Where does hydrothermal come from?
- 3 How do hydrothermal fluids form gold deposits?
- 4 How ore mineral deposit are created?
- 5 What is metasomatism explain?
- 6 What is the difference between metasomatism and hydrothermal alteration?
- 7 How are hydrothermal deposits important?
- 8 What are hydrothermal gold deposits?
How is a hydrothermal form?
Hydrothermal fluid forms as seawater are modified through interactions with heat and the earth’s crust. These fluids emanate back into ocean water at hydrothermal vents on the seafloor. Chemical reactions that occur at vents are also considered, including organic synthesis and the formation of metal sulfides.
Where does hydrothermal come from?
It may be released by a crystallizing magma; it can be expelled from a mass of rock undergoing metamorphism; or it may originate at Earth’s surface as rainwater or seawater and then trickle down to great depths through fractures and porous rocks, where it will be heated, react with adjacent rocks, and become a …
How do hydrothermal fluids form gold deposits?
Mineral assemblages formed during hydrothermal alteration reflect the geochemical composition of ore-forming fluids. Gold is mainly transported in solution as Au–Cl and Au–S complexes. Gold tends to be concentrated in the vapor phase of fluids at high temperatures and pressures.
What happens during metasomatism?
Metasomatism refers to the process whereby a preexisting igneous, sedimentary, or metamorphic rock undergoes compositional and mineralogical transformations associated with chemical reactions triggered by the reaction of fluids (so-called metasomatic agents), which invade the protolith.
What fluid is generally responsible for metasomatism?
Most metamorphic fluids must be rich in silica and alkalis, which may result in the appearance of aggressive silica-alkali fluids responsible for regional metasomatism and granitization. In general, the solubility of Fe-, Mg-, Mn-, and Ca-bearing minerals in alkaline solutions is low compared with acidic solutions.
How ore mineral deposit are created?
In contact metamorphism mineral deposits form irregular ore bodies on the margins of metamorphosed rocks. In sedimentary rocks epigenetic processes, ore deposits are formed due to weathering and deposition of detrital sedimentary rocks in basins where placer deposits are emplaced.
What is metasomatism explain?
Metasomatism (from the Greek μετά metá “change” and σῶμα sôma “body”) is the chemical alteration of a rock by hydrothermal and other fluids. It is the replacement of one rock by another of different mineralogical and chemical composition. Synonyms to the word metasomatism are metasomatose and metasomatic process.
What is the difference between metasomatism and hydrothermal alteration?
Metamorphism in which much of the change is derived from fluids passing through the rock is known as metasomatism . When hot water contributes to changes in rocks, including mineral alteration and formation of veins, it is known as hydrothermal alteration .
How do ore deposits form?
Ore deposits formed by lateral secretion are formed by metamorphic reactions during shearing, which liberate mineral constituents such as quartz, sulfides, gold, carbonates, and oxides from deforming rocks, and focus these constituents into zones of reduced pressure or dilation such as faults.
How do mineral deposits form?
Mineral deposits may be formed by the heating action of solar radiations which evaporate sea water in shallow basins. The dissolved material is left behind.
How are hydrothermal deposits important?
Hydrothermal deposits of economically valuable and recoverable minerals are generally considered scarce, meaning such deposits are very small relative to the total area of earth’s surface. Hydrothermal mineral deposits play a key role in nearly all modern industrial activities. Ore minerals are precipitated directly from a magma.
What are hydrothermal gold deposits?
Types of Hydrothermal Deposits Rising Fluid Deposits. Epithermal gold and other metal deposits 50-300C, shallow depths. Circulated Fluid in the Magma. Deep-seated magma has a slow circulation of fluids, which are rich in copper, gold, silver, lead, and zinc. Sub-Sea Massive Sulfides. Gold Deposits.