CLASSIFICATION LINDGREN


Lindgren (1907, 1913 and 1922) popularized the Genetic Classification or deposit of product classification mechanics or chemical concentration and classification of hydrothermal veins (hydrothermal vein). In group Lindgren including pirometa-somatic (igneous metamorpik) and hydrothermal deposits.

Classification Lindgren (Modification)
1. The precipitate that formed through a process of chemical concentrations (Temperature and Pressure Varies)



a. In a magma, by the process of differentiation
· magmatic deposits (segresi magma, magmatic liquid), T 700-15000C; P is very high.
· deposition Pegmatit; T medium-very high, very high P

b. In the body of rock
· concentrations because there is the addition of external (epigenetic)
· origin depends on the eruption of igneous rocks
Ø By blowing directly clot (magma)
ü From the effusive; sublimat; fumaroles, T 100-6000C; P atmosphere-medium
ü From the intrusive, Igneous metamorphic deposits; T 500-8000C, very high P
Ø By the addition of hot water filled with magma material
ü hipothermal deposition; T 300-5000C, very high P
ü mesothermal deposits; T 200-3000C, very high P
ü epithermal deposits; T 50-2000C, very high P
ü telethermal deposition; low T, low P
ü xenothermal deposition; T high-medium, medium-atmospheric P

· concentration of material in the rock body itself:
Ø Concentration by dynamic and regional metamorphism, T s / d 4000C; P high.
Ø The concentration of water in the soil; T 0-1000C; P is
Ø Concentration by lapukan rocks and weathering residue near the surface, T 0-1000C, P is-atmosphere

c. In the surface water
· The solution interaction; T 0-700C; P is
Inorganic Reaction Ø
Ø Organic Reactions
· by solvent evaporation

2. Deposits generated through mechanical concentration; T & P is.

Ket.
P = Pressure
T = Temperature