The document discusses three main types of ore forming processes: magmatic, sedimentary, and metamorphic. It focuses on magmatic processes, describing early and late magmatic processes like dissemination, segregation, injection, and residual liquid segregation and injection. Immiscible liquid segregation and injection are also discussed. Pegmatite deposits and contact metasomatic deposits near invading magmas are summarized. A variety of ore deposits can form from these magmatic processes depending on temperature and pressure conditions during crystallization and cooling of magma.

1. Ore Forming
Process
By
Abdul Bari Qanit
M.Sc. Geology

2. The processes of formation of mineral deposits
are grouped into three main types:
a. Magmatic Process
b. Sedimentary Process
c. Metamorphic Process.

3. Mineral deposits formed due to the various
processes associated with magmatic activities are
called 'Primary-Mineral Deposits'.
Mineral deposits arising out of the processes
of weathering, and activities of several geological
agents are called 'Secondary Mineral Deposits'.
These are closely associated with the sedimentary
processes of formation.
Metamorphic mineral deposits are the out-
come of metamorphic processes acting upon an
earlier formed mineral deposits or rocks.

5. • Charnockite • Gneiss
• Sandstone beds

6. Magmatic Ore Forming
Process

7. As we know, magma consists of a multitude of
constituents, which are in mutual solution. As the magma
approaches the earth's surface its temperature and the
external pressure drop, with the result of crystallization
and differentiation of minerals in a definite sequence. The
formation temperature of different magmatic deposits
varies from 1500'C to 300C°.

10. Magmatic Process
Early Magmatic Late Magmatic
Dissemination Residual Liquid Segregation
Segregation Residual Liquid Injection
Injection Immiscible Liquid Segregation
Immiscible Liquid Injection

11. Early Magmatic Process
The early magmatic deposits are believed to
have been formed simultaneously with the
host-rock. (or)
Where the Ore Deposits formed in the Early
stage of Magmatic periods.

12. Late Magmatic Process
The late magmatic deposits are
formed towards the close of the
magmatic deposits.
For example Titaniferous magnetite,

13. Magmatic Dissemination
Magmatic Dissemination (Simple
crystallization without concentration). It
involves simple crystallization whereby
early formed crystals are found

14. Diamond formation in Kimberlite Pipes

15. Magmatic Segregation
This type of magmatic concentration is
often due to the gravitative
crystallization of early formed heavy
minerals for, e.g., Bushveld chromite
deposits (South Africa), chromite
deposits of Keonjhar (Orissa).

16. Chromite Crystals Segregation

17. Magmatic Injection
In this case, the metallic concentrates
instead of remaining -at the place of
their original accumulation, get injected
into the adjacent solid rock-masses It
occurs at the residual magmatic stage,
e.g., Magnetite deposits of Kiruna
(Sweden).

18. Magmatic Injection

19. Immiscible Liquid Segregation
Sometimes magma of an ore-and-
silicate composition breaks down
during cooling into two immiscible
fractions which accumulate to form
liquid segregation deposits e.g.
Sulphide minerals Deposits.

20. Immiscible Liquid Segregation

21. Immiscible Liquid Injection
The immiscible liquid accumulations
before consolidation when subjected to
disturbances, get injected into the
surrounding rocks, forming immiscible
liquid-injection. A nickeliferous
Sulphide deposit of Sudbury (U.S.A.) is

22. Immiscible Liquid Injection

23. Residual Liquid Segregation
Basic magmas undergoing differentiation may
sometimes become enriched in iron and
titanium. This heavy residual liquid may
segregate and crystallize within the parent
igneous mass. Such ore bodies commonly
occur in form of parallel bands. The host rocks
are usually anorthosite, norite, gabbro
etc, e.g.. Titaniferous magnetite bands of

24. Residual Liquid Segregation

25. Residual Liquid Injection
In such cases, residual liquid be squeezed
out towards places of less pressure into
the neighboring rock mass forming late
magmatic injections, e.g., Titaniferous
magnetite deposits Adirondack region of
New York.

26. Residual Liquid Injection

27. Pegmatite

28. These are formed towards the very end of
consolidation of the magma, in which the
residual fraction is highly enriched with
volatile constituents. Pegmatitic liquids
may be squeezed out to fill in the cracks
and fissures in the parent igneous body or
the adjoining country rocks, and form
pegmatite veins or dykes. These are
usually formed between 500°C to 800"C.

29. Deposits of mica, feldspar, beryl,
lithium minerals, Gemstones and tin
mineral like cassiterite are included in
the pegmatite deposits.

30. multicolor tourmaline crystal in the
Himalaya pegmatite

31. Mica-rich pegmatite

32. Contact metasomatic
deposits

33. In the neighborhood of invading magmas,
alteration and replacement of the country
rocks due to invasion of magmatic
emanations may sometimes lead to the
development of mineral deposits of
economic importance.

34. In this case, the enclosing country rock is
altered by the heat and other chemical
constituents of the invading intrusive
magma forming new minerals under
conditions of high temperature and
pressure. The deposits are usually
resulted in calcareous rocks. The
temperature of formation ranges from
400°C to 1000°C.

35. Contact metasomatic deposits