1. ORE DEPOSITSFORMED BY WEATHERING ANDFORMATION
OF PLACERDEPOSITS
Topic :
Submitted By:Nazir Hussain Submitted To Dr.Riyaz M.K Khan
Class : M.Sc Semester : 2nd
2. introduction
ORE DEPOSITS:-
An ore deposits, in its simplest terms, is a portion of the Earth’s
crust from which some industrial raw material can be extracted at a
profit.
As such, its characteristics are as much economic as geochemical.
ORE DEPOSITS FORMED BY WEATHERING
Many types of mineral deposit form by weathering .
Weathering is the breakdown and alteration of rocks by physical
and chemical processes,both of which may be added by organic
activity.
3. The fractionation of the rock occurs in response to change in
environmental condition since the rock was formed.
E.g : The mineral of ignous rocks formed, at high temperature in the
absence of abundant water are unstable in the cooler.
The mineral of these rocks are altered to low-temperature, water
bearing faces or dissolved and removed.
Physical weathering disintegrates the rock creating large surface
areas and greater access by fluids.
These mineral deposits are among the most important ores formed
by weathering and supergene enrichment is one of the best
underestood aspects of weathering.
4. Placer deposits are formed by the mechanical concentration of
resistate minerals, which are released by weathering from
source rocks in which their distribution is normally
subeconomic.
The main commodities derived from placer deposits are tin,
gold, platinum, niobium, tantalum, titanium, zircon and
diamonds.
Some metals, such as gold, occur within the entire spectrum
of placer deposits, but it is more common for a mineral to be
concentrated in a specific placer environment, which is
ultimately controlled by tectonic setting.
FORMATION OF PLACER DEPOSITS
5. The main environment of placer formation are reviewed with
particular emphasis appropiate exploration techniques.
CLASSIFICATION OF PLACER DEPOSITS
Various classification systems have been proposed for placer
deposits ( wells, 1969, Smirnov, 1976 ).
We prefer to use a simplified version of a classification proposed by
Macdonald ( 1983 ) which is based primarily on geological
environment.
Schematic cross-section which shows the distribution of the
sub-environment of placers.