Nature of Ore-Bearing Fluids Flashcards

1
Q

Ore-bearing fluids

A

Magma/Magmatic Fluids

Hydrothermal Fluids

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2
Q

is a high temperature rock melt of liquid and crystals

A

Magma

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3
Q

oxide or sulfide dominated magma that solidify directly as ore

A

Ore magma

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4
Q

a process where a partly crystallized magma is subjected to stress, the fluid fraction is squeezed off from the residual crystalline mush

A

Filter pressing

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5
Q

coexistence between two liquids and their separation from each other

A

liquid immiscibility

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6
Q

high temperature

A

100C - 800C

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7
Q

Hydrothermal Flow Mechanisms

A

Fluids released due to magma cooling

Density differences induced by intrusion

compaction of sediments

osmotic pumping

salinity differences

hydraulic pressure difference

metamorphic recrystallization of hydrous phases

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8
Q

fractionated fluids and volatiles that travel upward from the magma

A

magmatic/juvenile waters

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9
Q

Chalcophile elements

A

Cu, Pb, Zn, Ag, Au, As, S

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10
Q

Large Ion Lithophile

A

Li, be, B, Rb, Cs

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11
Q

Alkalies, AEE, Volatiles

A

Na, K, Cl, Ca, CO2, H2O

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12
Q

Deacrase viscosity of magmas, lower freezing points of minerals, make possible devolpment of minerals/complexes that would not form in a dry melt

A

Fluxes

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13
Q

Elements that do not fit in feldspars and mafic silicate

A

LILEs

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14
Q

any water that passed through and equilibrated with the atmosphere

A

Meteoric Water

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15
Q

a medium of dispersion of dissolved ions, molecules, and suspended particles

A

Seawater

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16
Q

Effects of Hydrothermal Fluid Density

A

Solubility of volatiles and non-volatiles solutes in supercritical water varies inversely with density

chloride complexes dissociate as hydrothermal fluid density decrease

17
Q

water trapped in sediments at the time they were deposited

rich in Na and Cl

A

Connate Water

18
Q

connate and meteoric water subjected to heat and pressure from magmatic intrusion

A

Metamorphic Waters

19
Q

can be derived from the breakdown of hydrous minerals

A

Metamorphic Waters

20
Q

products of hydrothermal fluid flow

A

Veins

Breccia

Hydrothermal Alteration

21
Q

tabular veins of minerals that precipitated from hydrothermal fluids

22
Q

mineral growth in fluid-filled space

A

Distant Veins

23
Q

planar body of hydrothermally altered rock adjacent to a fracture or a channelway

A

Replacement Veins

24
Q

fluid is flowing through a rock

A

Open System

25
result of rock fragmentation in a pressure gradient
Brecciation
26
Causes of Fragmentation
Tectonic Gravity collapse in open of fluid-filled space explosive release of pressurized fluid
27
veins form due to local redistribution of fluids and solutes in a rock
Closed System
28
a chemical replacement of minerals where a fluid delivers the chemical reactants and removes the aqueous reaction products
hydrothermal Alteration
29
Commong Alteration Rxn | 8
``` Hydrolysis Hydration Alkali or Alkali-Earth Metasomatism Decarbonation Silication Silicification Redox Sulfidation ```
30
Alteration Type qtz, ms, tpz with common accessories of tur, fl, rt, cst, wolframite
Greisen
31
Alteration Type bt, kfelds plus one ore more of the ff: ser, chl, qtz
Potassic
32
Alteration Type ab, chl, ep, zeo, sme at low temp
Propylitic
33
Alteration Type qtz, ser, py, chl
Sericitic
34
Alteration Type qtz plus one or more of the ff; kln, dck, prl commonly ser, py, alu, tur, zunyite, tpz, dsp
Advanced Argilic
35
Alteration Type sme, kln, crs
Argilic
36
Alteration Type qtz, crs, trd, rt or ant
Silicic & Residual Silica
37
Alteration Type cal, dol, ank, sd
Carbonate
38
Alteration Type Ca and Mg silicates
Skarn